From df034010c3355aefb0ef9d47a5242ec7c3b0a586 Mon Sep 17 00:00:00 2001 From: Dylan Beaudette Date: Mon, 21 Jun 2021 13:17:46 -0700 Subject: [PATCH 1/3] parking refactored parseOSD code here, low-level fille access is no part of soilDB --- misc/parseOSD-migration/diagnostics.R | 32 + misc/parseOSD-migration/local_functions.R | 703 ++++++++++++++++++ misc/parseOSD-migration/main.R | 42 ++ .../predict-missing-colors-OLS.R | 386 ++++++++++ misc/parseOSD-migration/use-OSDRegistry.R | 113 +++ 5 files changed, 1276 insertions(+) create mode 100644 misc/parseOSD-migration/diagnostics.R create mode 100644 misc/parseOSD-migration/local_functions.R create mode 100644 misc/parseOSD-migration/main.R create mode 100644 misc/parseOSD-migration/predict-missing-colors-OLS.R create mode 100644 misc/parseOSD-migration/use-OSDRegistry.R diff --git a/misc/parseOSD-migration/diagnostics.R b/misc/parseOSD-migration/diagnostics.R new file mode 100644 index 0000000000..87713a93c8 --- /dev/null +++ b/misc/parseOSD-migration/diagnostics.R @@ -0,0 +1,32 @@ +library(Hmisc) + +## note: must explicitly use print() when source()-ing code that includes sink() + +## parsed from OSDs, no cleaning / estimation of missing colors +d <- read.csv('parsed-data.csv.gz', stringsAsFactors=FALSE) + +## dump basic summary, skipping horizon narratives +options(width=160) +sink(file='QC/parsed-hz-data-summary.txt') +print(Hmisc::describe(d[, grep('narrative', names(d), invert = TRUE)])) +sink() + + +## parsed from OSDs, no cleaning / estimation of missing colors +s <- read.csv('parsed-site-data.csv.gz', stringsAsFactors=FALSE) + +## dump basic summary, skipping last column containing horizon narratives +options(width=160) +sink(file='QC/parsed-site-data-summary.txt') +print(Hmisc::describe(s)) +sink() + + +## parsed from OSDs, after cleaning +d <- read.csv('parsed-data-est-colors.csv.gz', stringsAsFactors=FALSE) + +## dump basic summary, skipping horizon narratives +options(width=160) +sink(file='QC/cleaned-hz-data-summary.txt') +print(Hmisc::describe(d[, grep('narrative', names(d), invert = TRUE)])) +sink() diff --git a/misc/parseOSD-migration/local_functions.R b/misc/parseOSD-migration/local_functions.R new file mode 100644 index 0000000000..a6355dec52 --- /dev/null +++ b/misc/parseOSD-migration/local_functions.R @@ -0,0 +1,703 @@ +### moved all OSD HTML|TXT file getting / prep to soilDB + + +####### fulltext search support ################### + +# re-make entire fulltext table, containing an OSD per record +makeFullTextTable <- function(fullTextList, outputFile='fulltext-data.sql') { + # reset fulltext SQL file + cat('DROP TABLE osd.osd_fulltext;\n', file=outputFile) + cat('CREATE TABLE osd.osd_fulltext (series citext, fulltext text);\n', file=outputFile, append = TRUE) + cat("set client_encoding to 'latin1' ;\n", file=outputFile, append = TRUE) + + # remove NULL elements + idx <- which(! sapply(fullTextList, is.null)) + fullTextList <- fullTextList[idx] + + # iterate over list elements and write to file + # source text is gzip compressed + n <- lapply(fullTextList, function(i) { + # decompress text on the fly + txt <- memDecompress(i, type = 'gzip', asChar = TRUE) + cat(txt, file = outputFile, append = TRUE) + }) +} + + +# re-make sectioned fulltext table, containing an OSD per record +makeFullTextSectionsTable <- function(fullTextList, outputFile='fulltext-section-data.sql') { + + # reset fulltext SQL file + # need to adjust fields manually as we edit + cat('DROP TABLE osd.osd_fulltext2;\n', file='fulltext-section-data.sql') + cat('CREATE TABLE osd.osd_fulltext2 ( +series citext, +brief_narrative text, +taxonomic_class text, +typical_pedon text, +type_location text, +ric text, +competing_series text, +geog_location text, +geog_assoc_soils text, +drainage text, +use_and_veg text, +distribution text, +remarks text, +established text, +additional_data text + );\n', file='fulltext-section-data.sql', append = TRUE) + cat("set client_encoding to 'latin1' ;\n", file='fulltext-section-data.sql', append = TRUE) + + # remove NULL elements + idx <- which(! sapply(fullTextList, is.null)) + fullTextList <- fullTextList[idx] + + # iterate over list elements and write to file + # source text is gzip compressed + n <- lapply(fullTextList, function(i) { + # decompress text on the fly + txt <- memDecompress(i, type = 'gzip', asChar = TRUE) + cat(txt, file = outputFile, append = TRUE) + }) +} + + + + +# convert HTML text to fulltext DB table record +ConvertToFullTextRecord <- function(s, s.lines, tablename='osd.osd_fulltext') { + # collapse to single chunk + s.text <- paste(s.lines, collapse = '\n') + # convert into INSERT statement + # note: single quotes escaped with $$: + # http://stackoverflow.com/questions/12316953/insert-varchar-with-single-quotes-in-postgresql + res <- paste0('INSERT INTO ', tablename, " VALUES ($$", s, "$$,$$", s.text, "$$);\n") + return(res) +} + + +# convert HTML text to an insert statement with data split by section +ConvertToFullTextRecord2 <- function(s, s.lines, tablename='osd.osd_fulltext2') { + # split sections to list, section titles hard-coded + sections <- extractSections(s.lines) + + # get names of all sections + st <- names(.sectionData) + + # combine sections with $$ quoting + blob <- sapply(st, function(i) {paste0('$$', sections[[i]], '$$')}) + res <- paste0('INSERT INTO ', tablename, ' VALUES ( $$', s, '$$, ', paste(blob, collapse = ', '), ');\n') + return(res) +} + + +####### fulltext search support ################### + + + + + +downloadParseSave <- function(i) { + + # get OSD from WWW pages / HTML parsing + # result is a list + # i.lines <- try(soilDB:::.getLiveOSD(i), silent = TRUE) + + # get from local OSDRegistry repository + # result is a list + i.lines <- try( + soilDB:::.getLocalOSD(i, path = 'E:/working_copies/OSDRegistry/OSD'), + silent = TRUE + ) + + # no OSD... + if(class(i.lines) == 'try-error') + return(FALSE) + + # output as list + res <- list() + + # register section REGEX + # this sets / updates a global variable + setSectionREGEX(i) + + # get rendered HTML->text and save to file + # store gzip-compressd OSD for bulk INSERT + res[['fulltext']] <- memCompress(ConvertToFullTextRecord(i, i.lines), type='gzip') + + ## previously: + # cat(i.fulltext, file = 'fulltext-data.sql', append = TRUE) + + # split data into sections for fulltext search, catch errors related to parsing sections + i.sections <- try(ConvertToFullTextRecord2(i, i.lines)) + if(class(i.sections) != 'try-error') { + + # store gzip-compressed sections for bulk INSERT + res[['sections']] <- memCompress(i.sections, type='gzip') + + ## previously: + # cat(i.sections, file = 'fulltext-section-data.sql', append = TRUE) + } + + + # append hz data to our list, catch errors related to parsing sections + hz.data <- try(extractHzData(i.lines), silent = TRUE) + + # append site data to our list, catch errors related to parsing sections + section.data <- try(extractSections(i.lines), silent = TRUE) + site.data <- try(extractSiteData(section.data), silent = TRUE) + + # append if result was a data.frame + if(class(hz.data) == 'data.frame') { + # add seriesname to final column + hz.data$seriesname <- i + res[['hz']] <- hz.data + } + + # append if result was a data.frame + if(class(site.data) == 'data.frame') { + # add seriesname to final column + site.data$seriesname <- i + res[['site']] <- site.data + } + + return(res) +} + +# use this approach to make the wrapper "safe" +downloadParseSave.safe <- purrr::safely(downloadParseSave) + + + +testIt <- function(x) { + # get data + res <- soilDB:::.getLiveOSD(x) + + # init section REGEX: critical for locating brief narrative + setSectionREGEX(x) + + # extract sections + l <- list() + l[['sections']] <- extractSections(res) + l[['section-indices']] <- findSectionIndices(res) + l[['site-data']] <- extractSiteData(l[['sections']]) + l[['hz-data']] <- extractHzData(res) + + return(l) +} + +testItLocal <- function(x, path = 'E:/working_copies/OSDRegistry/OSD') { + # get data + res <- soilDB:::.getLocalOSD(x, path) + + # init section REGEX: critical for locating brief narrative + setSectionREGEX(x) + + # extract sections + l <- list() + l[['sections']] <- extractSections(res) + l[['section-indices']] <- findSectionIndices(res) + l[['site-data']] <- extractSiteData(l[['sections']]) + l[['hz-data']] <- extractHzData(res) + + return(l) +} + + +## safely (efficiently?) find specific classes within a vector of narratives +# needle: class labels +# haystack: narrative by horizon +findClass <- function(needle, haystack) { + # iterate over vector of horizon narratives, searching for exact matches + test.by.hz <- lapply(haystack, stri_detect_fixed, pattern = needle, opts_fixed = list(case_insensitive=TRUE)) + + # iterate over search results by horizon, keeping names of matching classes + matches <- lapply(test.by.hz, function(i) { + needle[i] + }) + + # compute number of characters: longer matches are the most specific / correct + res <- map_chr(matches, function(i) { + + # find the longest matching string + idx <- which.max(nchar(i)) + + # extract it + m <- i[idx] + + # convert _nothing_ into NA + if(length(m) > 0) { + return(m) + } else { + return(NA) + } + + }) + + return(res) +} + + +# vectorized parsing of texture class from OSD +parse_texture <- function(text) { + # mineral texture classes, sorted from coarse -> fine + textures <- c('coarse sand', 'sand', 'fine sand', 'very fine sand', 'loamy coarse sand', 'loamy sand', 'loamy fine sand', 'loamy very fine sand', 'coarse sandy loam', 'sandy loam', 'fine sandy loam', 'very fine sandy loam', 'loam', 'silt loam', 'silt', 'sandy clay loam', 'clay loam', 'silty clay loam', 'sandy clay', 'silty clay', 'clay') + + ## TODO: this is too greedy as 'fine sand' will be found _within_ 'fine sandy loam' + # https://github.com/dylanbeaudette/parse-osd/issues/10 + + # combine into capturing REGEX + # texture.regex <- paste0('(', paste(textures, collapse='|'), ')') + # + # # get matches + # m <- stri_match(text, regex = texture.regex, mode='first', opts_regex=list(case_insensitive=TRUE)) + # + # # fail gracefully in the case of no section data or no matches + # if(nrow(m) < 1) + # return(NA) + # + # # keep only matches and convert to lower case + # m <- tolower(m[, 2]) + + ## 2019-05-29: generalized for all non-greedy, exact matching + m <- findClass(needle=textures, haystack=text) + m <- tolower(m) + + # convert to ordered factor + m <- factor(m, levels=textures, ordered = TRUE) + + return(m) +} + +# vectorized parsing of horizon boundary +parse_hz_boundary <- function(text) { + + distinctness <- c('very abrupt', 'abrupt', 'clear', 'gradual', 'diffuse') + topography <- c('smooth', 'wavy', 'irregular', 'broken') + bdy <- apply(expand.grid(distinctness, topography), 1, paste, collapse=' ') + + + ## TODO: this is too greedy ? + # https://github.com/dylanbeaudette/parse-osd/issues/10 + + # combine into capturing REGEX + bdy.regex <- paste0('(', paste(bdy, collapse='|'), ') boundary') + + # get matches + m <- stri_match(text, regex = bdy.regex, mode='first', opts_regex=list(case_insensitive=TRUE)) + + # fail gracefully in the case of no section data or no matches + if(nrow(m) < 1) + return(NA) + + # keep only matches and convert to lower case + m <- tolower(m[, 2]) + + # split into pieces + res <- data.frame( + distinctness = findClass(needle=distinctness, haystack=m), + topography = findClass(needle=topography, haystack=m), + stringsAsFactors = FALSE + ) + + return(res) +} + +# vectorized parsing of coarse fraction qty+class from OSD +parse_CF <- function(text) { + cf.type <- c('gravelly', 'cobbly', 'stony', 'bouldery', 'channery', 'flaggy') + cf.qty <- c('', 'very ', 'extremely ') + cf <- apply(expand.grid(cf.qty, cf.type), 1, paste, collapse='') + + + ## TODO: this is too greedy as 'fine sand' will be found _within_ 'fine sandy loam' + # https://github.com/dylanbeaudette/parse-osd/issues/10 + + # combine into capturing REGEX + cf.regex <- paste0('(', paste(cf, collapse='|'), ')') + + # get matches + m <- stri_match(text, regex = cf.regex, mode='first', opts_regex=list(case_insensitive=TRUE)) + + # fail gracefully in the case of no section data or no matches + if(nrow(m) < 1) + return(NA) + + # keep only matches and convert to lower case + m <- tolower(m[, 2]) + + return(m) +} + +# vectorized parsing of pH +parse_pH <- function(text) { + + # combine into capturing REGEX + ph.regex <- '\\(ph\\s?([0-9]\\.[0-9])\\)' + + # get matches + m <- stri_match(text, regex = ph.regex, mode='first', opts_regex=list(case_insensitive=TRUE)) + + # fail gracefully in the case of no section data or no matches + if(nrow(m) < 1) + return(NA) + + # keep only matches + m <- as.numeric(m[, 2]) + + return(m) +} + + +# vectorized parsing of pH class +parse_pH_class <- function(text) { + + # mineral texture classes + pH_classes <- c('ultra acid', 'extremely acid', 'very strongly acid', 'strongly acid', 'moderately acid', 'slightly acid', 'neutral', 'slightly alkaline', 'mildly alkaline', 'moderately alkaline', 'strongly alkaline', 'very strongly alkaline') + + ## 2019-05-29: generalized for all non-greedy, exact matching + m <- findClass(needle=pH_classes, haystack=text) + m <- tolower(m) + + # return as an ordered factor acidic -> basic + m <- factor(m, levels=pH_classes, ordered = TRUE) + + return(m) +} + + +# vectorized parsing of drainage class +parse_drainage_class <- function(text) { + + # drainage classes, in order, lower case + classes <- c("excessively", "somewhat excessively", "well", "moderately well", + "somewhat poorly", "poorly", "very poorly", "subaqueous") + + ## TODO: this is too greedy as 'fine sand' will be found _within_ 'fine sandy loam' + # https://github.com/dylanbeaudette/parse-osd/issues/10 + + + # combine into capturing REGEX + classes.regex <- paste0('(', paste(classes, collapse='|'), ')') + + # get matches + m <- stri_match(text, regex = classes.regex, mode='first', opts_regex=list(case_insensitive=TRUE)) + + # fail gracefully in the case of no section data or no matches + if(nrow(m) < 1) + return(NA) + + # keep only matches and convert to lower case + m <- tolower(m[, 2]) + + # return as an ordered factor acidic -> basic + m <- factor(m, levels=classes, ordered = TRUE) + + return(m) +} + + + +### TODO: test / move into aqp ### + + +## this has to be done before any extraction is possible +# init the section names and REGEX search paterns +# the current series name is required for the top-most section +setSectionREGEX <- function(s) { + ## temporary hack: storing as a global variable + # values are REGEX that try to accommodate typos + # names are the proper section names + + ## TODO: + # consider anchoring all to left-side + optional white-space + # "TYPICAL PEDON" REGEX is too greedy + # "BRIEF DESCRIPTION" has date in front of "XXX SERIES" due to HTML formatting + # date is absent in OSDRegistry (local text file) interface + .sectionData <<- c('BRIEF DESCRIPTION' = paste0('^([0-9/]+)?', toupper(s), ' SERIES\\s?$'), + 'TAXONOMIC CLASS' = '^\\s*TAXONOMIC CLASS[:]? ', + 'TYPICAL PEDON'='^\\s*TYP.*\\sPEDON[:|-|;]?\\s?', + 'TYPE LOCATION'='^\\s*TYPE\\sLOCATION[:]?\\s?', + 'RANGE IN CHARACTERISTICS'='^\\s*RANGE IN CHARACTERISTICS[:]? ', + 'COMPETING SERIES'='^\\s*COMPETING SERIES[:]? ', + 'GEOGRAPHIC SETTING'='^\\s*GEOGRAPHIC SETTING[:]? ', + 'GEOGRAPHICALLY ASSOCIATED SOILS'='^\\s*GEOGRAPHICALLY ASSOCIATED SOILS[:]? ', + 'DRAINAGE AND PERMEABILITY'='^\\s*DRAINAGE AND (PERMEABILITY)|(HYDRAULIC CONDUCTIVITY)[:]? ', + 'USE AND VEGETATION'='^\\s*USE AND VEGETATION[:]? ', + 'DISTRIBUTION AND EXTENT'='^\\s*DISTRIBUTION AND EXTENT[:]? ', + 'REMARKS'='^\\s?REMARKS[:]? ', + 'SERIES ESTABLISHED'='^\\s*SERIES ESTABLISHED[:]? ', + 'ADDITIONAL DATA'='^\\s*ADDITIONAL DATA[:]? ' + ) + +} + + + + + +# locate section line numbers +findSectionIndices <- function(chunk.lines) { + # result is a list, sometimes a section REGEX will match multiple lines + s <- lapply(.sectionData, function(st) grep(st, chunk.lines, ignore.case = TRUE)) + + # filter out sections with no matches + match.idx <- which(sapply(s, function(i) length(i) > 0)) + s <- s[match.idx] + + # keep the first match + indices <- sapply(s, function(i) i[1]) + + # get set of section names with parsed data + section.names <- names(indices) + + return(indices) +} + +# extract sections from lines of OSD +extractSections <- function(chunk.lines, collapseLines=TRUE) { + # storage + l <- list() + + # locate section lines + # note: this will give values inclusive of the next section + section.locations <- findSectionIndices(chunk.lines) + section.names <- names(section.locations) + + # combine chunks into a list + for(i in 1:(length(section.locations) - 1)) { + + # current name and landmarks + this.name <- section.names[i] + start.line <- section.locations[i] + + # this stop line overlaps with the start of the next, decrease index by 1 + stop.line <- section.locations[i+1] - 1 + + # extract current chunk + chunk <- chunk.lines[start.line : stop.line] + + # special case #1: the brief narrative is split over two lines; first line is junk + if(this.name == 'BRIEF DESCRIPTION' & length(chunk) > 1) { + # attempt to remove when possible + chunk <- chunk[-1] + } + + # optionally combine lines + if(collapseLines) + chunk <- paste(chunk, collapse='') + + # attempt to remove section name + chunk <- gsub(this.name, '', chunk) + + # store + l[[this.name]] <- chunk + } + + return(l) +} + + + + + + +# parse important pieces from sections +# x: list of section chunks +extractSiteData <- function(x) { + + ## drainage class + + # this work for standard OSD format + drainage.class <- parse_drainage_class(x[['DRAINAGE AND PERMEABILITY']]) + + # alternative for SSR1 updated OSD format + # https://casoilresource.lawr.ucdavis.edu/sde/?series=bordengulch + if(is.na(drainage.class)) { + drainage.class <- parse_drainage_class(x[['BRIEF DESCRIPTION']]) + } + + + ## other things? + + + # composite into a list for later + r <- data.frame(drainage=drainage.class) + return(r) +} + + +# s.lines: result of getOSD() +extractHzData <- function(s.lines) { + options(stringsAsFactors=FALSE) + + ## TODO: this is kind of wasteful + # this will not work in the presence of typos + # new code for splitting blocks by section, lines from each section are not joined + sections <- extractSections(s.lines, collapseLines = FALSE) + tp <- sections[['TYPICAL PEDON']] + + ## REGEX rules + # http://regexr.com/ + ## TODO: combine top+bottom with top only rules + # TODO: allow for OCR errors: + # "O" = "0" + # "l" = "1" + ## ideas: http://stackoverflow.com/questions/15474741/python-regex-optional-capture-group + # detect horizons with both top and bottom depths + # hz.rule <- "^\\s*?([\\^\\'\\/a-zA-Z0-9]+)\\s?-+?\\s?([O0-9.]+)\\s+?to\\s+?([O0-9.]+)\\s+?(in|inches|cm|centimeters)" + hz.rule <- "([\\^\\'\\/a-zA-Z0-9]+)\\s*-+\\s*([O0-9.]+)\\s*?to\\s+?([O0-9.]+)\\s+?(in|inches|cm|centimeters)" + + # detect horizons with no bottom depth + hz.rule.no.bottom <- "([\\^\\'\\/a-zA-Z0-9]+)\\s*-+?\\s*([0-9.]+)\\s+?(in|inches|cm|centimeters)" + + + ## TODO: this doesn't work when only moist colors are specified (http://casoilresource.lawr.ucdavis.edu/sde/?series=canarsie) + ## TODO: these rules will not match neutral colors: N 2.5/ + ## TODO: toggle dry/moist assumption: + ## + ## Colors are for dry soil unless otherwise stated | Colors are for moist soil unless otherwise stated + ## + ## E1--7 to 12 inches; very dark gray (10YR 3/1) silt loam, 50 percent gray (10YR 5/1) and 50 percent gray (10YR 6/1) dry; moderate thin platy structure parting to weak thin platy; friable, soft; common fine and medium roots throughout; common fine tubular pores; few fine distinct dark yellowish brown (10YR 4/6) friable masses of iron accumulations with sharp boundaries on faces of peds; strongly acid; clear wavy boundary. + + ## A--0 to 6 inches; light gray (10YR 7/2) loam, dark grayish brown (10YR 4/2) moist; moderate coarse subangular blocky structure; slightly hard, friable, slightly sticky and slightly plastic; many very fine roots; many very fine and few fine tubular and many very fine interstitial pores; 10 percent pebbles; strongly acid (pH 5.1); clear wavy boundary. (1 to 8 inches thick) + ## + + ## TODO: test this + # establist default encoding of colors + dry.is.default <- length(grep('for dry (soil|conditions)', tp, ignore.case = TRUE)) > 0 + moist.is.default <- length(grep('for moist (soil|conditions)', tp, ignore.case = TRUE)) > 0 + + if(dry.is.default) + default.moisture.state <- 'dry' + if(moist.is.default) + default.moisture.state <- 'moist' + + # if neither are specified assume moist conditions + if((!dry.is.default & !moist.is.default)) + default.moisture.state <- 'moist' + + # if both are specified (?) + if(dry.is.default & moist.is.default) + default.moisture.state <- 'unknown' + + ## TODO: test this + # get all colors matching our rule, moist and dry and unknown, 5th column is moisture state + # interpretation is tough when multiple colors / hz are given + # single rule, with dry/moist state + # note that dry/moist may not always be present + color.rule <- "\\(([0-9]?[\\.]?[0-9]?[B|G|Y|R|N]+)([ ]+?[0-9\\.]+)/([0-9])\\)\\s?(dry|moist|)" + + # detect moist and dry colors + dry.color.rule <- "\\(([0-9]?[\\.]?[0-9]?[B|G|Y|R|N]+)([ ]+?[0-9\\.]+)/([0-9])\\)(?! moist)" + moist.color.rule <- "\\(([0-9]?[\\.]?[0-9]?[B|G|Y|R|N]+)([ ]+?[0-9\\.]+)/([0-9])\\) moist" + + # ID actual lines of horizon information + hz.idx <- unique(c(grep(hz.rule, tp), grep(hz.rule.no.bottom, tp))) + + # init empty lists to store hz data and colors + hz.data <- list() + dry.colors <- list() + moist.colors <- list() + narrative.data <- list() + + # iterate over identified horizons, extracting hz parts + for(i in seq_along(hz.idx)) { + this.chunk <- tp[hz.idx[i]] + + # parse hz designations and depths, keep first match + ## hack + # first try to find horizons with top AND bottom depths + h <- stri_match(this.chunk, regex=hz.rule) + # if none, then try searching for only top depths + if(all(is.na(h))) { + # this won't have the correct number of elements, adjust manually + h <- stri_match(this.chunk, regex=hz.rule.no.bottom) + h <- c(h, h[4]) # move units to 5th element + h[4] <- NA # add fake missing bottom depth + } + + # save hz data to list + hz.data[[i]] <- h + + # save narrative to list + narrative.data[[i]] <- this.chunk + + ## TODO: test this! + # parse ALL colors, result is a multi-row matrix, 5th column is moisture state + colors <- stri_match_all(this.chunk, regex=color.rule)[[1]] + # replace missing moisture state with (parsed) default value + colors[, 5][which(colors[, 5] == '')] <- default.moisture.state + + # exctract dry|moist colors, note that there may be >1 color per state + dc <- colors[which(colors[, 5] == 'dry'), 1:4, drop=FALSE] + mc <- colors[which(colors[, 5] == 'moist'), 1:4, drop=FALSE] + + # there there was at least 1 match, keep the first 1 + if(nrow(dc) > 0) + dry.colors[[i]] <- dc[1, ] + else + dry.colors[[i]] <- matrix(rep(NA, times=4), nrow = 1) + + if(nrow(mc) > 0) + moist.colors[[i]] <- mc[1, ] + else + moist.colors[[i]] <- matrix(rep(NA, times=4), nrow = 1) + } + + # test for no parsed data, must be some funky formatting... + if(length(hz.data) == 0) + return(NULL) + + # convert to DF + hz.data <- ldply(hz.data)[2:5] + dry.colors <- ldply(dry.colors)[2:4] + moist.colors <- ldply(moist.colors)[2:4] + narrative.data <- ldply(narrative.data) + + names(hz.data) <- c('name', 'top', 'bottom', 'units') + names(dry.colors) <- c('dry_hue', 'dry_value', 'dry_chroma') + names(moist.colors) <- c('moist_hue', 'moist_value', 'moist_chroma') + names(narrative.data) <- c('narrative') + + # cast to proper data types + hz.data$top <- as.numeric(hz.data$top) + hz.data$bottom <- as.numeric(hz.data$bottom) + + dry.colors$dry_value <- as.numeric(dry.colors$dry_value) + dry.colors$dry_chroma <- as.numeric(dry.colors$dry_chroma) + + moist.colors$moist_value <- as.numeric(moist.colors$moist_value) + moist.colors$moist_chroma <- as.numeric(moist.colors$moist_chroma) + + ## TODO sanity check / unit reporting: this will fail when formatting is inconsistent (PROPER series) + # convert in -> cm using the first horizon + if(hz.data$units[1] %in% c('inches', 'in')) { + hz.data$top <- round(hz.data$top * 2.54) + hz.data$bottom <- round(hz.data$bottom * 2.54) + } + + # remove units column + hz.data$units <- NULL + + # combine into single DF + res <- cbind(hz.data, dry.colors, moist.colors) + + # parse out other elements from the narrative + res$texture_class <- parse_texture(narrative.data$narrative) + res$cf_class <- parse_CF(narrative.data$narrative) + res$pH <- parse_pH(narrative.data$narrative) + res$pH_class <- parse_pH_class(narrative.data$narrative) + + bdy <- parse_hz_boundary(narrative.data$narrative) + res$distinctness <- bdy$distinctness + res$topography <- bdy$topography + + # add narrative + res <- cbind(res, narrative.data) + + return(res) +} + + diff --git a/misc/parseOSD-migration/main.R b/misc/parseOSD-migration/main.R new file mode 100644 index 0000000000..d9c8d9cea1 --- /dev/null +++ b/misc/parseOSD-migration/main.R @@ -0,0 +1,42 @@ +## Extract as much detail from text OSDs as possible, process colors, push to SoilWeb +## D.E. Beaudette +## 2019-11-19 + + +#### old method ### +## 1. get / parse data +# ~ 4-5 hours with single thread +# source('parse-all-series-via-sc-db.R') +# ~ 42 minutes parallel +# source('parallelParseOSD.R') + +########################### + +#### new method + +## 1. get / parse data +# ~ 3 minutes with local OSDRegistry files +# ~ fulltext source data is slow due to WD / scanning +source('use-OSDRegistry.R') + + +## 2. fill-in missing colors using OLS estimation of value and chroma +# ~ 2 minutes +source('predict-missing-colors-OLS.R') + +## TODO: finish evaluation / interpretation of color models + +## 3. diagnostics +source('diagnostics.R') + +## 4. send to SoilWeb + + + +## 5. re-load data: see sql/ dir in this repo + + + +# stats +x <- read.csv('logfile-2018-01-05.csv', stringsAsFactors = FALSE) +table(x$sections) diff --git a/misc/parseOSD-migration/predict-missing-colors-OLS.R b/misc/parseOSD-migration/predict-missing-colors-OLS.R new file mode 100644 index 0000000000..58ae2b8a48 --- /dev/null +++ b/misc/parseOSD-migration/predict-missing-colors-OLS.R @@ -0,0 +1,386 @@ +library(hexbin) +library(viridis) +library(aqp) +library(sharpshootR) +library(rms) +library(farver) +library(visreg) + +## dE00 observed vs. predicted +## +# ## static hue, dry value / chroma model +# 0% 5% 25% 50% 75% 95% 100% +# 0.000000 0.000000 0.000000 5.422945 9.359900 11.346863 61.787944 +# +# ## dry LAB model, before Munsell transform +# 0% 5% 25% 50% 75% 95% 100% +# 0.4382391 2.0232773 3.1119406 4.6279521 6.9709616 12.7304094 56.9446613 +# +# ## dry LAB model, after Munsell transform +# 0% 5% 25% 50% 75% 95% 100% +# 0.000000 0.000000 0.000000 3.931853 9.359900 11.318566 61.923273 +# + + +# from OSDs +d <- read.csv('parsed-data.csv.gz', stringsAsFactors=FALSE) + +# check initial conditions +str(d) + + +## estimation via value / chroma only +x <- na.omit(d[, c('dry_hue', 'dry_value', 'dry_chroma', 'moist_hue', 'moist_value', 'moist_chroma')]) + +# check assumption: moist/dry hues are the same +round(prop.table(table(x$dry_hue == x$moist_hue)), 3) + +# model +dd <- datadist(x) +options(datadist="dd") + +# dry from moist +(m.value.dry <- ols(dry_value ~ rcs(moist_value) + moist_chroma, data = x)) +(m.chroma.dry <- ols(dry_chroma ~ rcs(moist_chroma) + moist_value, data = x)) + +plot(Predict(m.value.dry), xlab='', ylab='dry value', asp=1) +plot(Predict(m.chroma.dry)) + +anova(m.value.dry) +anova(m.chroma.dry) + +# moist from dry +(m.value.moist <- ols(moist_value ~ rcs(dry_value) + dry_chroma, data=x)) +(m.chroma.moist <- ols(moist_chroma ~ rcs(dry_chroma) + dry_value, data=x)) + +plot(Predict(m.value.moist)) +plot(Predict(m.chroma.moist)) + +anova(m.value.moist) +anova(m.chroma.moist) + +## finish this +# plot(summary(m.value.moist, dry_value=c(3,4), dry_chroma=c(3,4))) +# plot(summary(m.value.dry, moist_value=c(3,4))) + +# +## partial effects via visreg: not all that interesting + +# visreg(m.value.dry) +# visreg(m.value.moist) +# +# visreg(m.chroma.dry) +# visreg(m.chroma.moist) + + + +## save a record of model accuracy +sink(file = 'QC/ols-model-accuracy.txt') +# moist colors +print(m.value.moist) +print(m.chroma.moist) +# dry colors +print(m.value.dry) +print(m.chroma.dry) +sink() + +# save model objects +save(m.value.dry, m.value.moist, m.chroma.dry, m.chroma.moist, file='models/missing-color-models.rda') + + +## predictions from full set + +# dry +pp.value.dry <- predict(m.value.dry) +pp.chroma.dry <- predict(m.chroma.dry) + +# moist +pp.value.moist <- predict(m.value.moist) +pp.chroma.moist <- predict(m.chroma.moist) + +# combine +pp.dry <- data.frame(pp.value.dry, pp.chroma.dry) +pp.moist <- data.frame(pp.value.moist, pp.chroma.moist) +z <- cbind(x, pp.dry, pp.moist) + +# check: OK +# head(z) + + +## note: must print() lattice graphics when code is source()-ed + +## graphical eval: seems reasonable +png(filename = 'figures/dv-model.png', width=800, height=800, res=90) + +print( + hexbinplot(pp.value.dry ~ dry_value, data=x, trans = log, inv=exp, colramp=viridis, asp=1, xbins=10, xlab='Observed Dry Value', ylab='Predicted Dry Value', colorkey=FALSE) +) + +dev.off() + + +png(filename = 'figures/dc-model.png', width=800, height=800, res=90) + +print( + hexbinplot(pp.chroma.dry ~ dry_chroma, data=x, trans = log, inv=exp, colramp=viridis, asp=1, xbins=10, xlab='Observed Dry Chroma', ylab='Predicted Dry Chroma', colorkey=FALSE) +) + +dev.off() + + +png(filename = 'figures/mv-model.png', width=800, height=800, res=90) + +print( + hexbinplot(pp.value.moist ~ moist_value, data=x, trans = log, inv=exp, colramp=viridis, asp=1, xbins=10, xlab='Observed Moist Value', ylab='Predicted Moist Value', colorkey=FALSE) +) + +dev.off() + + +png(filename = 'figures/mc-model.png', width=800, height=800, res=90) + +print( + hexbinplot(pp.chroma.moist ~ moist_chroma, data=x, trans = log, inv=exp, colramp=viridis, asp=1, xbins=10, xlab='Observed Moist Chroma', ylab='Predicted Moist Chroma', colorkey=FALSE) +) + +dev.off() + + + + + +## make a copy of some of the data, +x.original <- subset(d, subset = seriesname %in% c('AMADOR', 'DRUMMER', 'CECIL', 'REDDING', 'AVA', 'MIAMI', 'FRISCO')) + +# promote to SPC and convert colors +depths(x.original) <- seriesname ~ top + bottom +x.original$dry_soil_color <- munsell2rgb(x.original$dry_hue, x.original$dry_value, x.original$dry_chroma) +x.original$moist_soil_color <- munsell2rgb(x.original$moist_hue, x.original$moist_value, x.original$moist_chroma) + +# label +x.original$group <- rep('Original', times=length(x.original)) + + +## add a flags for estimated colors +d$dry_color_estimated <- FALSE +d$moist_color_estimated <- FALSE + +## fill missing color components via models + +# flag based on missing hue +d$dry_color_estimated[which(is.na(d$dry_hue))] <- TRUE +d$moist_color_estimated[which(is.na(d$moist_hue))] <- TRUE + +# copy vs. prediction of hue, use moist / dry hue +d$moist_hue[which(is.na(d$moist_hue))] <- d$dry_hue[which(is.na(d$moist_hue))] +d$dry_hue[which(is.na(d$dry_hue))] <- d$moist_hue[which(is.na(d$dry_hue))] + +# moist value +idx <- which(is.na(d$moist_value)) +d$moist_value[idx] <- round(predict(m.value.moist, d[idx, ])) + +# dry value +idx <- which(is.na(d$dry_value)) +d$dry_value[idx] <- round(predict(m.value.dry, d[idx, ])) + +# moist chroma +idx <- which(is.na(d$moist_chroma)) +d$moist_chroma[idx] <- round(predict(m.chroma.moist, d[idx, ])) + +# dry chroma +idx <- which(is.na(d$dry_chroma)) +d$dry_chroma[idx] <- round(predict(m.chroma.dry, d[idx, ])) + + +# estimated proportions +prop.table(table(d$dry_color_estimated)) +prop.table(table(d$moist_color_estimated)) + + +## filling missing O horizon colors requires fixing 0->O OCR errors +idx <- grep('^0', d$name) +sort(table(d$name[idx]), decreasing = TRUE) + +# replace 0 with O +d$name[idx] <- gsub('0', 'O', d$name[idx]) + + +## O horizon colors: moist and dry colors missing + +# find some to eval +x.o <- d[grep('^O', d$name), ] +nrow(x.o) +head(x.o) +sort(table(x.o$name), decreasing = TRUE) + +# generalize into a 3 classes + everything else +x.o$genhz <- generalize.hz(x.o$name, new=c('Oi', 'Oe', 'Oa'), pat = c('Oi', 'Oe', 'Oa')) + +# convert colors +x.o$dry_color <- munsell2rgb(x.o$dry_hue, x.o$dry_value, x.o$dry_chroma) +x.o$moist_color <- munsell2rgb(x.o$moist_hue, x.o$moist_value, x.o$moist_chroma) + +# split and upgrade to SPC +x.o.d <- subset(x.o, subset=! is.na(dry_color) & !is.na(top) & !is.na(bottom)) +x.o.m <- subset(x.o, subset=! is.na(moist_color) & !is.na(top) & !is.na(bottom)) + +depths(x.o.d) <- seriesname ~ top + bottom +depths(x.o.m) <- seriesname ~ top + bottom + +# aggregate colors +a.d <- aggregateColor(x.o.d, groups='genhz', col='dry_color', k=10) +a.m <- aggregateColor(x.o.d, groups='genhz', col='moist_color', k=10) + + +png(file='figures/O-hz-colors-dry.png', width = 900, height=550, res=90) +aggregateColorPlot(a.d, main='Dry Colors') +dev.off() + + +png(file='figures/O-hz-colors-moist.png', width = 900, height=550, res=90) +aggregateColorPlot(a.m, main='Moist Colors') +dev.off() + +knitr::kable(a.d$aggregate.data, row.names = FALSE) +knitr::kable(a.m$aggregate.data, row.names = FALSE) + + +## find O horizons that are missing colors, and use these ones + +# Oi / dry +idx <- which(grepl('Oi', d$name) & is.na(d$dry_hue)) +d$dry_hue[idx] <- '7.5YR' +d$dry_value[idx] <- 4 +d$dry_chroma[idx] <- 2 + +# Oi / moist +idx <- which(grepl('Oi', d$name) & is.na(d$moist_hue)) +d$moist_hue[idx] <- '7.5YR' +d$moist_value[idx] <- 2 +d$moist_chroma[idx] <- 2 + +# Oe / dry +idx <- which(grepl('Oe', d$name) & is.na(d$dry_hue)) +d$dry_hue[idx] <- '7.5YR' +d$dry_value[idx] <- 4 +d$dry_chroma[idx] <- 2 + +# Oe / moist +idx <- which(grepl('Oe', d$name) & is.na(d$moist_hue)) +d$moist_hue[idx] <- '7.5YR' +d$moist_value[idx] <- 2 +d$moist_chroma[idx] <- 2 + +# Oa / dry +idx <- which(grepl('Oa', d$name) & is.na(d$dry_hue)) +d$dry_hue[idx] <- '5YR' +d$dry_value[idx] <- 4 +d$dry_chroma[idx] <- 1 + +# Oa / moist +idx <- which(grepl('Oa', d$name) & is.na(d$moist_hue)) +d$moist_hue[idx] <- '7.5YR' +d$moist_value[idx] <- 2 +d$moist_chroma[idx] <- 1 + +# everything else, dry +idx <- which(grepl('O', d$name) & is.na(d$dry_hue)) +d$dry_hue[idx] <- '10YR' +d$dry_value[idx] <- 4 +d$dry_chroma[idx] <- 1 + +# everything else, moist +idx <- which(grepl('O', d$name) & is.na(d$moist_hue)) +d$moist_hue[idx] <- '10YR' +d$moist_value[idx] <- 2 +d$moist_chroma[idx] <- 1 + + +## +## extract same series and compare original vs. filled colors +## +x <- subset(d, subset = seriesname %in% c('AMADOR', 'DRUMMER', 'CECIL', 'REDDING', 'AVA', 'MIAMI', 'FRISCO')) +x$seriesname <- paste0(x$seriesname, '-filled') +depths(x) <- seriesname ~ top + bottom +x$dry_soil_color <- munsell2rgb(x$dry_hue, x$dry_value, x$dry_chroma) +x$moist_soil_color <- munsell2rgb(x$moist_hue, x$moist_value, x$moist_chroma) + +# label +x$group <- rep('Filled', times=length(x)) + +# stack +g <- combine(x.original, x) + +# convert to factor for groupedProfilePlot +g$group <- factor(g$group) + +# new group with original series name +g$original.name <- site(g)[[idname(g)]] +# trim 'filled' +g$original.name <- gsub('-filled', '', g$original.name) + +## graphical comparison... still needs some work + +png(file='figures/dry-original-vs-filled-example.png', width = 900, height=800, res=90) + +par(mar=c(1,1,3,1), mfrow=c(2,1)) +groupedProfilePlot(g, name='', groups='original.name', color='dry_soil_color', id.style='side', label='group') ; title('Dry Colors') +groupedProfilePlot(g, name='', groups='original.name', color='moist_soil_color', id.style='side', label='group') ; title('Moist Colors') + +dev.off() + + + + + + +png(file='figures/original-dry-vs-moist.png', width = 900, height=800, res=90) + +par(mar=c(2,1,3,1), mfrow=c(2,1)) +plot(x.original, color='dry_soil_color', max.depth=165, name='') +title('Original Dry Colors') +plot(x.original, color='moist_soil_color', max.depth=165, name='') +title('Original Moist Colors') + +dev.off() + + +png(file='figures/filled-dry-vs-moist.png', width = 900, height=800, res=90) + +par(mar=c(2,1,3,1), mfrow=c(2,1)) +plot(x, color='dry_soil_color', max.depth=165, name='') +title('Filled Dry Colors') +plot(x, color='moist_soil_color', max.depth=165, name='') +title('Filled Moist Colors') + +dev.off() + + + +## alternative display with colorspace::swatchplot() + +png(file='figures/original-vs-filled-swatch.png', width=700, height=400, res=90) + +colorspace::swatchplot( + 'dry missing'=x.original$dry_soil_color, + 'moist missing'=x.original$moist_soil_color, + 'dry filled'=x$dry_soil_color, + 'moist filled'=x$moist_soil_color +) + +dev.off() + +# convert logical -> character for portability +d$dry_color_estimated <- as.character(d$dry_color_estimated) +d$moist_color_estimated <- as.character(d$moist_color_estimated) + +## save results +write.csv(d, file=gzfile('parsed-data-est-colors.csv.gz'), row.names=FALSE) + + + + + + + + diff --git a/misc/parseOSD-migration/use-OSDRegistry.R b/misc/parseOSD-migration/use-OSDRegistry.R new file mode 100644 index 0000000000..8ca9566448 --- /dev/null +++ b/misc/parseOSD-migration/use-OSDRegistry.R @@ -0,0 +1,113 @@ +library(stringi) +library(httr) +library(rvest) +library(purrr) +library(furrr) +library(R.utils) + + +## TODO: remove dependency +# used by extractHzData() +library(plyr) + +# moved low-level file access here +library(soilDB) + +## TODO: convert to JSON section + + +# functions used here, some of which will go to soilDB +source('local_functions.R') + +## TODO: get latest SC from local NASIS if available + +# load latest SC-database +tf <- tempfile() +download.file(url = 'https://github.com/ncss-tech/SoilTaxonomy/raw/master/inst/extdata/SC-database.csv.gz', destfile = tf) +x <- read.csv(tf, stringsAsFactors = FALSE) + +# keep only those records that are established or tentative +x <- subset(x, subset= soilseriesstatus != 'inactive') + +# keep just the series names +x <- x$soilseriesname +names(x) <- x + + +# init parallel processing, works on macos and windows +plan(multisession) + +# using local copy of OSDs via OSDRegistry working copy +# ~ 3 minutes +system.time(res <- future_map(x, downloadParseSave.safe, .progress = TRUE)) + +# stop back-ends +plan(sequential) + + +######################################## + + +## TODO: update cached copy, for those series that have been updated since the last run +# cache results just in case +saveRDS(res, file='cached-copy.rds') + + +## process horizon data +z <- map(res, pluck, 'result', 'hz') +# remove NULL +idx <- which(! sapply(z, is.null)) +z <- z[idx] +# convert to data.frame (~ 15 seconds) +d <- do.call('rbind', z) +# save +write.csv(d, file=gzfile('parsed-data.csv.gz'), row.names=FALSE) + +## process site data +z <- map(res, pluck, 'result', 'site') +# remove NULL +idx <- which(! sapply(z, is.null)) +z <- z[idx] +# convert to data.frame (~ 1 seconds) +d <- do.call('rbind', z) +# save +write.csv(d, file=gzfile('parsed-site-data.csv.gz'), row.names=FALSE) + + + +## process fulltext +z <- map(res, pluck, 'result', 'fulltext') +# iterate over list elements and write to file (~ 5 minutes, slow due to scanning) +makeFullTextTable(z) + +# process sections +z <- map(res, pluck, 'result', 'sections') +makeFullTextSectionsTable(z) + + +## compress fulltext +f <- list.files(path='.', pattern = '\\.sql$', full.names = TRUE) + +for(i in f) { + print(i) + gzip(i, remove=TRUE, skip=FALSE) +} + + + + +## TODO: finish error checking and "problem OSDs" + +# # save dated log file +# write.csv(logdata, file=paste0('logfile-', Sys.Date(), '.csv'), row.names=FALSE) +# +# # ID those series that were not parsed +# parse.errors <- logdata$.id[which(! logdata$`hz-data` & logdata$sections)] +# cat(parse.errors, file=paste0('problem-OSDs-', Sys.Date(), '.txt'), sep = '\n') + + + + + +## done, now fill missing colors via supervised classification + From 129e692f3dcd85c3ec7f99eacaf597beeb53667f Mon Sep 17 00:00:00 2001 From: SoilKnowledgeBot Date: Mon, 21 Jun 2021 20:35:25 +0000 Subject: [PATCH 2/3] Update inst/extdata/ JSON files --- inst/extdata/OSD/B/BEETLEROCK.json | 6 +++--- inst/extdata/OSD/B/BELLECANYON.json | 26 +++++++++++++------------- inst/extdata/OSD/C/CABINCOVE.json | 8 ++++---- inst/extdata/OSD/C/CAHOON.json | 8 ++++---- inst/extdata/OSD/C/CANYONVIEW.json | 6 +++--- inst/extdata/OSD/C/COLONYMILL.json | 10 +++++----- inst/extdata/OSD/D/DORST.json | 6 +++--- inst/extdata/OSD/E/EDENCREEK.json | 10 +++++----- inst/extdata/OSD/F/FORGOTTEN.json | 10 +++++----- inst/extdata/OSD/G/GENERALGRANT.json | 8 ++++---- inst/extdata/OSD/G/GRATWELL.json | 8 ++++---- inst/extdata/OSD/H/HALSTEAD.json | 18 +++++++++--------- inst/extdata/OSD/H/HOCKETT.json | 8 ++++---- inst/extdata/OSD/I/ISOSCELES.json | 14 +++++++------- inst/extdata/OSD/K/KAWEAH.json | 12 ++++++------ inst/extdata/OSD/L/LACKEY.json | 18 +++++++++--------- inst/extdata/OSD/L/LADDERLAKE.json | 8 ++++---- inst/extdata/OSD/L/LITTLEPETE.json | 10 +++++----- inst/extdata/OSD/M/MARMOT.json | 16 ++++++++-------- inst/extdata/OSD/M/MCDERMAND.json | 16 ++++++++-------- inst/extdata/OSD/M/MINERALKING.json | 12 ++++++------ inst/extdata/OSD/P/PIGCHUTE.json | 14 +++++++------- inst/extdata/OSD/P/PINERIDGE.json | 8 ++++---- inst/extdata/OSD/R/RHODE_RIVER.json | 2 +- inst/extdata/OSD/T/THARPSLOG.json | 8 ++++---- inst/extdata/OSD/T/TIGERLILY.json | 16 ++++++++-------- inst/extdata/OSD/T/TUOHY.json | 12 ++++++------ inst/extdata/OSD/W/WAGER.json | 10 +++++----- inst/extdata/OSD/W/WHISKEYLOG.json | 16 ++++++++-------- inst/extdata/OSD/W/WINDOWPEAK.json | 6 +++--- inst/extdata/OSD/Y/YUCCACREEK.json | 10 +++++----- 31 files changed, 170 insertions(+), 170 deletions(-) diff --git a/inst/extdata/OSD/B/BEETLEROCK.json b/inst/extdata/OSD/B/BEETLEROCK.json index 7c44dbafff..687ea5859c 100644 --- a/inst/extdata/OSD/B/BEETLEROCK.json +++ b/inst/extdata/OSD/B/BEETLEROCK.json @@ -1,8 +1,8 @@ { "SERIES": "BEETLEROCK", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Beetlerock series consists of very deep, well drained soils formed in colluvium over residuum weathered from granite and granodiorite rocks. The Beetlerock soils are on mountain slopes of the Sierra Nevada mountains. Slopes range from 15 to 60 percent. The mean annual precipitation is about 980 mm and the mean annual air temperature is about 6 degrees C.", "TAXONOMIC CLASS": { @@ -31,7 +31,7 @@ }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", - "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Hockett and Kanawyer soils. The Hockett soils are formed in till on linear structural benches, and are 50 to 100 cm deep to bedrock. Kanawyer soils formed in till and on linear to convex mountain slopes have greater than 35 percent fragments in the particle size control section." + "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Doncecil, Hockett, and Kanawyer soils. The Doncecil soils formed in colluvium on linear to concave mountain slopes, and have greater than 35 percent fragments in the particle size control section. The Hockett soils are formed in till on linear structural benches, and are 50 to 100 cm deep to bedrock. Kanawyer soils formed in till on linear to convex mountain slopes, and have greater than 35 percent fragments in the particle size control section." }, "DRAINAGE AND PERMEABILITY": { "section": "DRAINAGE AND PERMEABILITY", diff --git a/inst/extdata/OSD/B/BELLECANYON.json b/inst/extdata/OSD/B/BELLECANYON.json index 51497c393d..a3a3821278 100644 --- a/inst/extdata/OSD/B/BELLECANYON.json +++ b/inst/extdata/OSD/B/BELLECANYON.json @@ -1,37 +1,37 @@ { "SERIES": "BELLECANYON", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB/JTW", - "REVDATE": "04/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Beetlerock series consists of very deep, well drained soils formed in colluvium over residuum weathered from granite and granodiorite rocks. The Beetlerock soils are on mountain slopes of the Sierra Nevada mountains. Slopes range from 15 to 60 percent. The mean annual precipitation is about 980 mm and the mean annual air temperature is about 6 degrees C.", + "OVERVIEW": "The Bellecanyon series consists of very deep, well drained soils formed in outwash over till derived from granitic rocks. The Bellecanyon soils are on moraines of the Sierra Nevada Mountains. Slopes range from 2 to 15 percent. The mean annual precipitation is about 860 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Sandy, isotic, frigid Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Bellecanyon loamy coarse sand on a south-east-facing (153 degree), 9 percent slope under a canopy of Jeffrey and lodgepole pine at an elevation of 2366 meters. (Colors are for dry soils unless otherwise noted. When described on September 12, 2014 the soil was dry throughout.)\nOi--0 to 5 cm; slightly decomposed plant material, dark brown (7.5YR 3/2) moist; about 100 percent fiber, 90 percent rubbed; few very fine roots throughout; very strongly acid (pH 5.0); abrupt smooth boundary. (0 to 5 cm thick) Lab sample #15N02494\nA--5 to 18 cm; brown (10YR 4/3) loamy coarse sand, dark brown (7.5YR 3/2) moist; 80 percent sand; 17 percent silt; 3 percent clay; weak coarse subangular blocky structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, fine, and medium roots throughout; common very fine and fine irregular pores; 10 percent subangular very strongly cemented granite gravel; NaF pH 10.3; strongly acid (pH 5.4); clear smooth boundary. (3 to 20 cm thick) Lab sample #15N02495\nBw1--18 to 43 cm; dark yellowish brown (10YR 4/4) gravelly loamy coarse sand, dark brown (10YR 3/3) moist; 80 percent sand; 17 percent silt; 4 percent clay; weak coarse subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, coarse, and very coarse roots throughout; common very fine, fine, and medium irregular pores; 15 percent subrounded very strongly cemented granite gravel; NaF pH 10.8; strongly acid (pH 5.4); clear smooth boundary. (15 to 40 cm thick) Lab sample #15N02496\nBw2--43 to 89 cm; yellowish brown (10YR 5/4) gravelly loamy coarse sand, dark brown (10YR 3/3) moist; 82 percent sand; 15 percent silt; 4 percent clay; weak medium subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, few fine, and common medium, coarse, and very coarse roots throughout; common very fine, fine, and medium irregular pores; 20 percent subrounded very strongly cemented granite gravel, 3 percent subrounded very strongly cemented granite cobbles; NaF pH 10.8; strongly acid (pH 5.4); clear smooth boundary. (25 to 50 cm thick) Lab sample #15N02497\n2C--89 to 160 cm; yellowish brown (10YR 5/4) very cobbly loamy coarse sand, very dark brown (7.5YR 2.5/3) moist; 83 percent sand; 14 percent silt; 4 percent clay; structureless single grain; loose, loose, nonsticky, nonplastic; common medium and coarse roots throughout; common very fine, fine, and medium irregular pores; 35 percent subrounded strongly cemented granite gravel, 22 percent subrounded strongly cemented granite cobbles, 2 percent subrounded strongly cemented granite stones; NaF pH 10.7; strongly acid (pH 5.4). Lab sample #15N02498" + "content": "TYPICAL PEDON: Bellecanyon loamy coarse sand on a south-east-facing (153 degree), 9 percent slope under a canopy of Jeffrey and lodgepole pine at an elevation of 2366 meters. (Colors are for dry soils unless otherwise noted. When described on September 12, 2014 the soil was dry throughout.)\nOi--0 to 5 cm; slightly decomposed plant material, dark brown (7.5YR 3/2) moist; about 100 percent fiber, 90 percent rubbed; few very fine roots throughout; very strongly acid (pH 5.0); abrupt smooth boundary. (0 to 5 cm thick) Lab sample # 15N02494\nA--5 to 18 cm; brown (10YR 4/3) loamy coarse sand, dark brown (7.5YR 3/2) moist; 80 percent sand; 17 percent silt; 3 percent clay; weak coarse subangular blocky structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, fine, and medium roots throughout; common very fine and fine irregular pores; 10 percent subangular very strongly cemented granite gravel; NaF pH 10.3; strongly acid (pH 5.4); clear smooth boundary. (3 to 20 cm thick) Lab sample # 15N02495\nBw1--18 to 43 cm; dark yellowish brown (10YR 4/4) gravelly loamy coarse sand, dark brown (10YR 3/3) moist; 80 percent sand; 17 percent silt; 4 percent clay; weak coarse subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, coarse, and very coarse roots throughout; common very fine, fine, and medium irregular pores; 15 percent subrounded very strongly cemented granite gravel; NaF pH 10.8; strongly acid (pH 5.4); clear smooth boundary. (15 to 40 cm thick) Lab sample # 15N02496\nBw2--43 to 89 cm; yellowish brown (10YR 5/4) gravelly loamy coarse sand, dark brown (10YR 3/3) moist; 82 percent sand; 15 percent silt; 4 percent clay; weak medium subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, few fine, and common medium, coarse, and very coarse roots throughout; common very fine, fine, and medium irregular pores; 20 percent subrounded very strongly cemented granite gravel, 3 percent subrounded very strongly cemented granite cobbles; NaF pH 10.8; strongly acid (pH 5.4); clear smooth boundary. (25 to 50 cm thick) Lab sample # 15N02497\n2C--89 to 160 cm; yellowish brown (10YR 5/4) very cobbly loamy coarse sand, very dark brown (7.5YR 2.5/3) moist; 83 percent sand; 14 percent silt; 4 percent clay; structureless single grain; loose, loose, nonsticky, nonplastic; common medium and coarse roots throughout; common very fine, fine, and medium irregular pores; 35 percent subrounded strongly cemented granite gravel, 22 percent subrounded strongly cemented granite cobbles, 2 percent subrounded strongly cemented granite stones; NaF pH 10.7; strongly acid (pH 5.4). Lab sample # 15N02498" }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, approximately 300 m west of Halstead Meadow; USGS 7.5 minute topographic quadrangle: Giant Forest, CA; WGS84 36.616922 latitude and -118.788800 longitude; UTM zone 11 4053867 meters N 340038 meters E NAD83." + "content": "TYPE LOCATION: Tulare County, California, approximately 2.7 km south west of Sugarloaf Peak, Kings Canyon National Park; USGS 7.5 minute topographic quadrangle: Mount Silliman, California; WGS84 36.712840 latitude and -118.680644 longitude; UTM zone 11 4064333 meters N 349897 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 9 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 40 to 110 cm\nReaction: slightly to strongly acid\nBase saturation: less than 50 percent in some or all parts of the epipedon (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 150 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 0 to 30 percent, with 0 to 30 percent gravel, 0 to 5 percent cobbles, and 0 to 5 percent stones\nClay content: 1 to 8 percent\nNaF pH: 8.5 to 11.0\nA horizon\nHue: 10YR or 2.5YR dry, 7.5YR or 10YR moist\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 or 2 moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 1 to 7 percent\nRock fragments: 0 to 30 percent\n0 to 30 percent gravel\n0 to 5 percent cobbles\n0 to 5 percent stones\nAB horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sand, loamy sand, loamy fine sand\nClay content: 1 to 7 percent\nRock fragments: 0 to 30 percent\n0 to 30 percent gravel\n0 to 5 percent cobbles\n0 to 5 percent stones\nBw horizon\nHue: 7.5YR, 10YR\nValue: 4 to 6 dry, 3 or 4 moist\nChroma: 2 to 4 dry, 2 or 3 moist\nTexture: sand, loamy sand, loamy fine sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 30 percent\n0 to 30 percent gravel\n0 to 5 percent cobbles\n0 to 5 percent stones\nC horizon\nHue: 10YR, 2.5Y\nValue: 6 to 8 dry, 4 or 5 moist\nChroma: 2 to 4, dry or moist\nTexture: coarse sand, sand, loamy coarse sand, loamy sand\nClay content: 1 to 7 percent\nRock fragments: 0 to 40 percent\n0 to 40 percent gravel\n0 to 30 percent paragravel\n0 to 5 percent cobbles\n0 to 5 percent paracobbles\n0 to 5 percent stones" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 5 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 100 cm\nReaction: slightly to strongly acid\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 2.0 percent (by weight) to a depth of 150 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 0 to 20 percent, with 0 to 20 percent gravel, 0 to 5 percent cobbles, and 0 to 5 percent stones\nClay content: 3 to 7 percent\nNaF pH: 8.5 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 4 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 or 2 moist\nTexture: loamy sand, loamy coarse sand\nClay content: 3 to 6 percent\nRock fragments: 0 to 20 percent gravel\nBw1 horizon\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 3 or 4, dry or moist\nTexture: loamy sand, loamy coarse sand\nClay content: 3 to 7 percent\nRock fragments: 0 to 20 percent gravel\nBw2 horizon\nHue: 10YR\nValue: 5 to 7 dry, 3 to 5 moist\nChroma: 2 to 4 dry, 3 to 6 moist\nTexture: loamy sand, loamy coarse sand\nClay content: 3 to 7 percent\nRock fragments: 0 to 25 percent\n0 to 20 percent gravel\n0 to 5 percent cobbles\n2C horizon\nHue: 10YR, 2.5Y\nValue: 6 or 7 dry, 4 or 5 moist\nChroma: 2 to 4 dry, 3 to 6 moist\nTexture: loamy sand, loamy coarse sand, sand\nClay content: 2 to 6 percent\nRock fragments: 30 to 60 percent\n30 to 60 percent gravel\n0 to 30 percent cobbles\n0 to 5 percent stones" }, "COMPETING SERIES": { "section": "COMPETING SERIES", - "content": "COMPETING SERIES: These are the Bellecanyon (T), Hockett (T), and Packerjohn soils. Bellecanyon soils are formed in outwash over till, have subrounded fragments, and do not contain fragments larger than cobbles in the upper part of the profile. Hockett (T) soils are 50 to 100 cm deep to a lithic contact. Packerjohn soils have pH values that range up to neutral and textures with ashy modifiers in the particle-size control section." + "content": "COMPETING SERIES: These are the Beetlerock, Hockett, and Packerjohn soils. Beetlerock soils are formed in colluvium and residuum, have subangular fragments, and contain fragments larger than cobbles throughout the profile. Packerjohn soils have pH values that range up to neutral and textures with ashy modifiers in the particle size control section. Hockett soils are 50 to 100 cm deep to a lithic contact." }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Beetlerock soils are on linear to convex backslopes of mountain slopes. Slopes range from 15 to 60 percent. These soils formed in colluvium over residuum weathered from granite and granodiorite. Elevation is 1980 to 2815 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 475 to 1375 mm and the mean annual air temperature is 4 to 9 degrees C. The frost free season is 85 to 160 days." + "content": "GEOGRAPHIC SETTING: The Bellecanyon soils are on linear footslopes of ground moraines. Slopes range from 2 to 15 percent. These soils formed in glacial outwash over glacial till derived from granite and granodiorite. Elevation is 2000 to 2900 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 775 to 1350 mm and the mean annual air temperature is 4 to 7 degrees C. The frost free season is 80 to 115 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", - "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Hockett and Kanawyer soils. The Hockett soils are formed in till on linear structural benches, and are 50 to 100 cm deep to bedrock. Kanawyer soils formed in till and on linear to convex mountain slopes have greater than 35 percent fragments in the particle size control section." + "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Kanawyer soils. Kanawyer soils are on linear backslopes of moraines and are sandy-skeletal." }, "DRAINAGE AND PERMEABILITY": { "section": "DRAINAGE AND PERMEABILITY", @@ -39,11 +39,11 @@ }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is white fir, Jeffrey pine, Sierra lodgepole pine, greenleaf manzanita, chinquapin, and whitethorn ceanothus." + "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is Jeffrey pine, Sierra lodgepole pine, white fir, greenleaf manzanita, whitethorn ceanothus, and chinquapin." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", - "content": "DISTRIBUTION AND EXTENT: Sierra Nevada Mountains of California; MLRA 22A. These soils are of moderate extent." + "content": "DISTRIBUTION AND EXTENT: Sierra Nevada Mountains of California; MLRA 22A. These soils are not extensive." }, "REGIONAL OFFICE": { "section": "SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE", @@ -51,10 +51,10 @@ }, "ORIGIN": { "section": "SERIES PROPOSED", - "content": "SERIES PROPOSED: Tulare County, California in Sequoia and Kings Canyon National Parks. Source of name from a landscape feature in Sequoia National Park." + "content": "SERIES PROPOSED: Tulare County, California in Sequoia and Kings Canyon National Parks. Source of name from a landscape feature in Kings Canyon National Park." }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 30 to 105 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 5 to 86 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2015CA7921029\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 30 to 105 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 5 to 89 cm\nAndic Soil Properties 18 to 43 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nLab Source ID: KSSL\nLab Pedon #: 15N0491\nNASIS User Pedon ID: S2014CA107003\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/C/CABINCOVE.json b/inst/extdata/OSD/C/CABINCOVE.json index 7ebce9f3b9..e453e6eace 100644 --- a/inst/extdata/OSD/C/CABINCOVE.json +++ b/inst/extdata/OSD/C/CABINCOVE.json @@ -1,8 +1,8 @@ { "SERIES": "CABINCOVE", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Cabincove series consists of moderately deep, well drained soils formed in residuum weathered from granitic rocks. The Cabincove soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 10 to 60 percent. The mean annual precipitation is about 1025 mm and the mean annual air temperature is about 9 degrees C.", "TAXONOMIC CLASS": { @@ -11,7 +11,7 @@ }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Cabincove sandy loam on a southeast-facing (152 degree), 43 percent slope under mixed conifer and hardwood forest at an elevation of 1852 meters. (Colors are for dry soils unless otherwise noted. When described on April 20, 2015 the soil was slightly moist throughout.)\nOi--0 to 5 cm; slightly decomposed plant material, dark brown (10YR 3/3) moist; about 100 percent fiber, 90 percent rubbed; moderately acid (pH 5.6); abrupt smooth boundary. (2 to 5 cm thick)\nA--5 to 14 cm; dark grayish brown (10YR 4/2) sandy loam, very dark brown (10YR 2/2) moist; 4 percent clay; weak thick platy structure; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; many very fine and common fine irregular pores; 10 percent subangular indurated granodiorite fine gravel; NaF pH 9.5; slightly acid (pH 6.2); abrupt wavy boundary. (3 to 15 cm thick)\nBw--14 to 30 cm; brown (10YR 5/3) gravelly loamy sand, very dark grayish brown (10YR 3/2) moist; 4 percent clay; weak medium subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; many very fine and fine and common medium irregular pores; 15 percent subrounded very strongly cemented granodiorite fine gravel; NaF pH 9.0; slightly acid (pH 6.4); clear smooth boundary. (10 to 30 cm thick)\nC--30 to 68 cm; pale brown (10YR 6/3) gravelly loamy sand, dark grayish brown (10YR 4/2) moist; 3 percent clay; weak fine subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, medium, coarse, and very coarse roots throughout; common very fine, fine, and medium irregular pores; 25 percent subrounded strongly cemented granodiorite fine gravel, 2 percent rounded moderately cemented granodiorite paracobbles; NaF pH 8.5; slightly acid (pH 6.4); abrupt wavy boundary. (15 to 60 cm thick)\nCr--68 to 147 cm; moderately cemented granite bedrock, fractured at intervals of greater than 200 cm; few fine and common medium, coarse, and very coarse roots top of horizon." + "content": "TYPICAL PEDON: Cabincove sandy loam on a southeast-facing (152 degree), 43 percent slope under mixed conifer and hardwood forest at an elevation of 1852 meters. (Colors are for dry soils unless otherwise noted. When described on April 20, 2015 the soil was slightly moist throughout.)\nOi--0 to 5 cm; slightly decomposed plant material, dark brown (10YR 3/3) moist; about 100 percent fiber, 90 percent rubbed; moderately acid (pH 5.6); abrupt smooth boundary. (2 to 5 cm thick)\nA--5 to 14 cm; dark grayish brown (10YR 4/2) sandy loam, very dark brown (10YR 2/2) moist; 4 percent clay; weak thick platy structure; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; many very fine and common fine irregular pores; 10 percent subangular indurated granite fine gravel; NaF pH 9.5; slightly acid (pH 6.2); abrupt wavy boundary. (3 to 15 cm thick)\nBw--14 to 30 cm; brown (10YR 5/3) gravelly loamy sand, very dark grayish brown (10YR 3/2) moist; 4 percent clay; weak medium subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; many very fine and fine and common medium irregular pores; 15 percent subrounded very strongly cemented granite fine gravel; NaF pH 9.0; slightly acid (pH 6.4); clear smooth boundary. (10 to 30 cm thick)\nC--30 to 68 cm; pale brown (10YR 6/3) gravelly loamy sand, dark grayish brown (10YR 4/2) moist; 3 percent clay; weak fine subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, medium, coarse, and very coarse roots throughout; common very fine, fine, and medium irregular pores; 25 percent subrounded strongly cemented granite fine gravel, 2 percent rounded moderately cemented granite paracobbles; NaF pH 8.5; slightly acid (pH 6.4); abrupt wavy boundary. (15 to 60 cm thick)\nCr--68 to 147 cm; moderately cemented granite bedrock, fractured at intervals of greater than 200 cm; few fine and common medium, coarse, and very coarse roots top of horizon." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -23,7 +23,7 @@ }, "COMPETING SERIES": { "section": "COMPETING SERIES", - "content": "COMPETING SERIES: There are no other series in this family at this time." + "content": "COMPETING SERIES: These are the Azalea, Generalgrant and Tharpslog soils. The Azalea soils are on convex shoulders and backslopes of mountain slopes and have a lithic contact between 50 and 100 cm. The Generalgrant soils are on concave footslopes of stream terraces and drainageways on mountain slopes and are moderately well drained. The Tharpslog soils are on broadly concave backslopes on mountain slopes and are somewhat excessively drained." }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", diff --git a/inst/extdata/OSD/C/CAHOON.json b/inst/extdata/OSD/C/CAHOON.json index 61a53ac842..6384d5675a 100644 --- a/inst/extdata/OSD/C/CAHOON.json +++ b/inst/extdata/OSD/C/CAHOON.json @@ -1,13 +1,13 @@ { "SERIES": "CAHOON", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Cahoon series consists of very deep, moderately well drained soils formed in outwash over till derived from granitic rocks. The Cahoon soils are on moraines and outwash plains of the Sierra Nevada Mountains. Slopes range from 5 to 20 percent. The mean annual precipitation is about 1000 mm and the mean annual air temperature is about 6 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, frigid Vitrandic Humixerepts" + "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, frigid Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 5 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 75 cm\nCambic horizon thickness: 0 to 50 cm\nOrganic matter: 2 to 6 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm\nDepth to redoximorphic features: 25 to 75 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 5 to 35 percent gravel, 0 to 35 percent cobbles, 0 to 15 percent stones and 0 to 15 percent boulders\nClay content: 5 to 12 percent\nNaF pH: 9.0 to 11.0\nA horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 or 4 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, fine sandy loam\nClay content: 6 to 12 percent\nRock fragments: 0 to 35 percent\n0 to 15 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\n0 to 15 percent boulders\nReaction: very strongly to strongly acid\nBw horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 or 4 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, fine sandy loam\nClay content: 6 to 12 percent\nRock fragments: 35 to 75 percent\n5 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 15 percent stones\n0 to 15 percent boulders\nReaction: strongly to moderately acid\nC horizon(s)\nHue: 10YR, 2.5Y\nValue: 3 or 4 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: loamy sand, loamy fine sand, sand, fine sand\nClay content: 1 to 5 percent\nRock fragments: 15 to 60 percent\n5 to 35 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\n0 to 15 percent boulders\nReaction: strongly to moderately acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 5 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 75 cm\nCambic horizon thickness: 0 to 50 cm\nOrganic matter: 2 to 6 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm\nDepth to redoximorphic features: 50 to 75 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 5 to 35 percent gravel, 0 to 35 percent cobbles, 0 to 15 percent stones and 0 to 15 percent boulders\nClay content: 5 to 12 percent\nNaF pH: 9.0 to 11.0\nA horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 or 4 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, fine sandy loam\nClay content: 6 to 12 percent\nRock fragments: 0 to 40 percent\n0 to 15 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\n0 to 20 percent boulders\nReaction: very strongly to strongly acid\nBw horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 or 4 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, fine sandy loam\nClay content: 6 to 12 percent\nRock fragments: 35 to 75 percent\n5 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 15 percent stones\n0 to 20 percent boulders\nReaction: strongly to moderately acid\nC horizon(s)\nHue: 10YR, 2.5Y\nValue: 3 or 4 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: loamy sand, loamy fine sand, sand, fine sand\nClay content: 1 to 5 percent\nRock fragments: 15 to 60 percent\n5 to 40 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\n0 to 15 percent boulders\nReaction: strongly to moderately acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/C/CANYONVIEW.json b/inst/extdata/OSD/C/CANYONVIEW.json index f9cb643c08..f55b9980f4 100644 --- a/inst/extdata/OSD/C/CANYONVIEW.json +++ b/inst/extdata/OSD/C/CANYONVIEW.json @@ -1,8 +1,8 @@ { "SERIES": "CANYONVIEW", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Canyonview series consists of very deep, well drained soils formed in colluvium over till derived from granitic rocks. The Canyonview soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 780 mm and the mean annual air temperature is about 10 degrees C.", "TAXONOMIC CLASS": { @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 8 to 13 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about June to October (about 150 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 20 to 50 cm\nOrganic matter: 1 to 5 percent in the epipedon\nBase saturation: less than 50 percent in one or more horizons between the mineral soil surface and a depth of 180 cm (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 2.0 percent (by weight) throughout one or more horizons with a total thickness of 18 cm or more within 75 cm of the mineral soil surface.\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 15 to 50 percent gravel, 15 to 35 percent cobbles, 0 to 35 percent stones and 0 to 25 percent boulders.\nClay content: 1 to 8 percent\nNaF pH: 9.0 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 moist\nChroma: 2 or 3 dry, 1 or 2 moist\nTexture: loamy sand, coarse sandy loam, sandy loam\nClay content: 1 to 8 percent\nRock fragments: 5 to 60 percent\n5 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 20 percent stones\n0 to 5 percent boulders\nVolcanic glass: 5 to 10 percent\nReaction: moderately acid to neutral\nAB horizon\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 3 moist\nChroma: 3 or 4 dry, 2 or 3 moist\nTexture: loamy sand, coarse sandy loam, sandy loam\nClay content: 2 to 8 percent\nRock fragments: 15 to 60 percent\n15 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 20 percent stones\n0 to 5 percent boulders\nVolcanic glass: 5 to 10 percent\nReaction: moderately to slightly acid\nBw horizon\nHue: 7.5YR, 10YR\nValue: 5 or 6 dry, 3 or 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy coarse sand, loamy fine sand\nClay content: 1 to 8 percent\nRock fragments: 35 to 80 percent\n15 to 60 percent gravel\n0 to 25 percent cobbles\n0 to 35 percent stones\n0 to 25 percent boulders\nReaction: strongly to slightly acid\nC horizons\nHue: 10YR, 2.5YR\nValue: 5 or 6 dry, 3 to 5 moist\nChroma: 3 or 4, dry or moist\nTexture: loamy coarse sand, coarse sand, sand\nClay content: 0 to 8 percent\nRock fragments: 35 to 80 percent\n15 to 50 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 25 percent boulders\nReaction: strongly to slightly acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 8 to 13 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about June to October (about 150 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 50 cm\nOrganic matter: 1 to 5 percent in the epipedon\nBase saturation: less than 50 percent in one or more horizons between the mineral soil surface and a depth of 180 cm (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 2.0 percent (by weight) throughout one or more horizons with a total thickness of 18 cm or more within 75 cm of the mineral soil surface.\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 15 to 50 percent gravel, 15 to 35 percent cobbles, 0 to 35 percent stones and 0 to 25 percent boulders.\nClay content: 1 to 8 percent\nNaF pH: 9.0 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 moist\nChroma: 2 or 3 dry, 1 or 2 moist\nTexture: loamy sand, coarse sandy loam, sandy loam\nClay content: 1 to 8 percent\nRock fragments: 5 to 60 percent\n5 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 20 percent stones\n0 to 5 percent boulders\nVolcanic glass: 5 to 10 percent\nReaction: moderately acid to neutral\nAB horizon\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 3 moist\nChroma: 3 or 4 dry, 2 or 3 moist\nTexture: loamy sand, coarse sandy loam, sandy loam\nClay content: 2 to 8 percent\nRock fragments: 15 to 60 percent\n15 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 20 percent stones\n0 to 5 percent boulders\nVolcanic glass: 5 to 10 percent\nReaction: moderately to slightly acid\nBw horizon\nHue: 7.5YR, 10YR\nValue: 5 or 6 dry, 3 or 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy coarse sand, loamy fine sand\nClay content: 1 to 8 percent\nRock fragments: 35 to 80 percent\n15 to 60 percent gravel\n0 to 25 percent cobbles\n0 to 35 percent stones\n0 to 25 percent boulders\nReaction: strongly to slightly acid\nC horizons\nHue: 10YR, 2.5YR\nValue: 5 or 6 dry, 3 to 5 moist\nChroma: 3 or 4, dry or moist\nTexture: loamy coarse sand, coarse sand, sand\nClay content: 0 to 8 percent\nRock fragments: 35 to 80 percent\n15 to 50 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 25 percent boulders\nReaction: strongly to slightly acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/C/COLONYMILL.json b/inst/extdata/OSD/C/COLONYMILL.json index 7f08eded50..9627528b67 100644 --- a/inst/extdata/OSD/C/COLONYMILL.json +++ b/inst/extdata/OSD/C/COLONYMILL.json @@ -1,8 +1,8 @@ { "SERIES": "COLONYMILL", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Colonymill series consists of very deep, well drained soils formed in colluvium and residuum derived from schist and other metasedimentary rocks. The Colonymill soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 945 mm and the mean annual air temperature is about 11 degrees C.", "TAXONOMIC CLASS": { @@ -11,15 +11,15 @@ }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Colonymill loam on a southwest-facing (220 degree), 60 percent slope under a cover of live oak and manzanita at an elevation of 1518 meters. (Colors are for dry soils unless otherwise noted. When described on April 16, 2014 the soil was moist throughout.)\nOi--0 to 2 cm; brown (7.5YR 4/2) slightly decomposed plant material, very dark brown (7.5YR 2/2) moist; slightly acid (pH 6.4); very abrupt wavy boundary. (2 to 8 cm thick)\nA--2 to 9 cm; brown (7.5YR 4/2) loam, very dark brown (7.5YR 2/2) moist; 10 percent clay; moderate fine granular structure; soft, very friable, slightly sticky, nonplastic; common very fine and fine roots throughout; many very fine irregular pores; 1 percent subangular indurated schist channers; NaF pH 9.0; slightly acid (pH 6.4); abrupt wavy boundary. (7 to 25 cm thick)\nBA--9 to 20 cm; brown (7.5YR 4/3) loam, dark reddish brown (5YR 2.5/2) moist; 20 percent clay; weak medium subangular blocky parts to moderate fine granular structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, fine, and coarse roots throughout; many very fine irregular and common fine tubular pores; 5 percent subangular indurated schist channers; NaF pH 9.0; slightly acid (pH 6.4); clear smooth boundary. (10 to 40 cm thick)\nBw--20 to 55 cm; brown (7.5YR 4/3) loam, dark reddish brown (5YR 2.5/2) moist; 26 percent clay; moderate medium subangular blocky structure; slightly hard, friable, slightly sticky, slightly plastic; common very fine, fine, medium, and coarse roots throughout; common very fine irregular and common fine tubular pores; 5 percent angular indurated schist channers, 5 percent subangular indurated schist gravel, 1 percent subangular indurated schist cobbles; NaF pH 9.0; moderately acid (pH 6.0); gradual smooth boundary. (10 to 40 cm thick)\nBt1--55 to 98 cm; brown (7.5YR 4/3) clay loam, dark reddish brown (5YR 3/2) moist; 29 percent clay; moderate coarse subangular blocky structure; slightly hard, friable, moderately sticky, slightly plastic; common very fine, fine, medium, and very coarse roots throughout; common very fine irregular and common fine and medium tubular pores; 5 percent faint clay films on surfaces along pores; 15 percent coarse dark reddish brown (2.5YR 3/4) masses of oxidized iron; 7 percent subangular indurated schist gravel, 7 percent subangular indurated schist cobbles; NaF pH 9.0; moderately acid (pH 5.8); clear wavy boundary. (20 to 45 cm thick)\nBt2--98 to 129 cm; brown (7.5YR 5/4) cobbly clay loam, reddish brown (5YR 4/3) moist; 37 percent clay; moderate medium subangular blocky structure; moderately hard, firm, slightly sticky, moderately plastic; common medium, coarse, and very coarse roots throughout; common very fine irregular and common fine and medium tubular pores; 5 percent faint clay films on surfaces along pores and 10 percent faint clay films on all faces of peds; 10 percent subangular strongly cemented schist gravel, 5 percent subangular very weakly cemented schist paragravel, 15 percent subangular strongly cemented schist cobbles; NaF pH 9.0; moderately acid (pH 5.8); gradual wavy boundary.\nBt3--129 to 160 cm; brown (7.5YR 5/4) very stony clay loam, reddish brown (5YR 4/3) moist; 33 percent clay; moderate medium subangular blocky structure; moderately hard, firm, slightly sticky, moderately plastic; few fine and medium roots throughout and common very coarse roots top of horizon; common fine and medium tubular pores; 5 percent faint clay films on surfaces along pores and 10 percent faint clay films on all faces of peds; 10 percent subangular strongly cemented schist gravel, 25 percent subangular strongly cemented schist cobbles, 10 percent subangular strongly cemented schist stones; NaF pH 9.0; moderately acid (pH 5.8). (combined thickness of the lower Bt horizons is 30 to 100 cm)" + "content": "TYPICAL PEDON: Colonymill loam on a southwest-facing (220 degree), 60 percent slope under a cover of live oak and manzanita at an elevation of 1518 meters. (Colors are for dry soils unless otherwise noted. When described on April 16, 2014 the soil was moist throughout.)\nOi--0 to 2 cm; brown (7.5YR 4/2) slightly decomposed plant material, very dark brown (7.5YR 2/2) moist; slightly acid (pH 6.4); very abrupt wavy boundary. (2 to 8 cm thick)\nA--2 to 9 cm; brown (7.5YR 4/2) loam, very dark brown (7.5YR 2/2) moist; 10 percent clay; moderate fine granular structure; soft, very friable, slightly sticky, nonplastic; common very fine and fine roots throughout; many very fine irregular pores; 1 percent subangular indurated schist channers; NaF pH 9.0; slightly acid (pH 6.4); abrupt wavy boundary. (7 to 25 cm thick)\nBA--9 to 20 cm; brown (7.5YR 4/3) loam, dark reddish brown (5YR 2.5/2) moist; 20 percent clay; weak medium subangular blocky parts to moderate fine granular structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, fine, and coarse roots throughout; many very fine irregular and common fine tubular pores; 5 percent subangular indurated schist channers; NaF pH 9.0; slightly acid (pH 6.4); clear smooth boundary. (10 to 40 cm thick)\nBw--20 to 55 cm; brown (7.5YR 4/3) loam, dark reddish brown (5YR 2.5/2) moist; 26 percent clay; moderate medium subangular blocky structure; slightly hard, friable, slightly sticky, slightly plastic; common very fine, fine, medium, and coarse roots throughout; common very fine irregular and common fine tubular pores; 5 percent angular indurated schist channers, 5 percent subangular indurated schist gravel, 1 percent subangular indurated schist cobbles; NaF pH 9.0; moderately acid (pH 6.0); gradual smooth boundary. (10 to 40 cm thick)\nBt1--55 to 98 cm; brown (7.5YR 4/3) clay loam, dark reddish brown (5YR 3/2) moist; 29 percent clay; moderate coarse subangular blocky structure; slightly hard, friable, moderately sticky, slightly plastic; common very fine, fine, medium, and very coarse roots throughout; common very fine irregular and common fine and medium tubular pores; 5 percent faint clay films on surfaces along pores; 15 percent coarse dark reddish brown (2.5YR 3/4) masses of oxidized iron; 7 percent subangular indurated schist gravel, 7 percent subangular indurated schist cobbles; NaF pH 9.0; moderately acid (pH 5.8); clear wavy boundary. (20 to 45 cm thick)\nBt2--98 to 129 cm; brown (7.5YR 5/4) cobbly clay loam, reddish brown (5YR 4/3) moist; 37 percent clay; moderate medium subangular blocky structure; moderately hard, firm, slightly sticky, moderately plastic; common medium, coarse, and very coarse roots throughout; common very fine irregular and common fine and medium tubular pores; 5 percent faint clay films on surfaces along pores and 10 percent faint clay films on all faces of peds; 10 percent subangular strongly cemented schist gravel, 5 percent subangular very weakly cemented schist paragravel, 15 percent subangular strongly cemented schist cobbles; NaF pH 9.0; moderately acid (pH 5.8); gradual wavy boundary.\nBt3--129 to 160 cm; brown (7.5YR 5/4) very cobbly clay loam, reddish brown (5YR 4/3) moist; 33 percent clay; moderate medium subangular blocky structure; moderately hard, firm, slightly sticky, moderately plastic; few fine and medium roots throughout and common very coarse roots top of horizon; common fine and medium tubular pores; 5 percent faint clay films on surfaces along pores and 10 percent faint clay films on all faces of peds; 10 percent subangular strongly cemented schist gravel, 25 percent subangular strongly cemented schist cobbles, 10 percent subangular strongly cemented schist stones; NaF pH 9.0; moderately acid (pH 5.8). (combined thickness of the lower Bt horizons is 30 to 100 cm)" }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, near Crystal Cave parking area in Sequoia National Park; USGS 7.5 minute topographic quadrangle: Giant Forest, California; WGS84 36.585556 latitude and -118.826483 longitude; UTM zone 11 4050452 meters N 336601 meters E NAD83." + "content": "TYPE LOCATION: Tulare County, California, near Crystal Cave parking area in Sequoia National Park; USGS 7.5 minute topographic quadrangle: Giant Forest, California; WGS84 36.585556 latitude and -118.826483 longitude; UTM zone 11 4050452 meters N 336601 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 11 to 15 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nMollic epipedon thickness: 50 to 75 cm\nArgillic horizon thickness: 70 to greater than 150 cm\nOrganic matter: 1 to 5 percent in the epipedon\nBase saturation: greater than 50 percent in the epipedon (by ammonium acetate) and 35 to 75 percent in one or more horizons between 25 and 75 cm from the mineral soil surface (by sum of cations).\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 35 percent gravel and 0 to 5 percent cobbles.\nClay content: 18 to 32 percent\nNaF pH: 8.5 to 10.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 4 dry, 2 or 3 moist\nChroma: 3 or 4 dry, 2 or 3 moist\nTexture: loam, sandy loam\nClay content: 12 to 20 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel or channers\n0 to 5 percent cobbles\nReaction: strongly acid to neutral\nBA, ABt or Bw horizons (where present)\nHue: 5YR, 7.5YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 3 or 4 dry, 2 or 3 moist\nTexture: loam, sandy loam, clay loam\nClay content: 15 to 30 percent\nRock fragments: 0 to 25 percent\n0 to 15 percent gravel or channers\n0 to 10 percent cobbles\nReaction: moderately acid to slightly acid\nBt1 horizon\nHue: 5YR, 7.5YR\nValue: 4 5 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: loam, clay loam\nClay content: 18 to 32 percent\nRock fragments: 0 to 35 percent\n0 to 30 percent gravel\n0 to 5 percent cobbles\nReaction: moderately acid to slightly acid\nLower Bt horizons (Bt2, Bt3)\nHue: 5YR, 7.5YR\nValue: 5 dry, 3 or 4 moist\nChroma: 4 or 6 dry, 3 or 4 moist\nTexture: clay loam, loam\nClay content: 25 to 38 percent\nRock fragments: 0 to 60 percent\n0 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 15 percent stones\nReaction: strongly acid to moderately acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 11 to 15 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nMollic epipedon thickness: 50 to 75 cm\nArgillic horizon thickness: 70 to greater than 150 cm\nOrganic matter: 1 to 5 percent in the epipedon\nBase saturation: greater than 50 percent in the epipedon (by ammonium acetate) and 35 to 75 percent in one or more horizons between 25 and 75 cm from the mineral soil surface (by sum of cations).\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 35 percent gravel and 0 to 5 percent cobbles.\nClay content: 18 to 32 percent\nNaF pH: 8.5 to 10.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 4 dry, 2 or 3 moist\nChroma: 3 or 4 dry, 2 or 3 moist\nTexture: loam, sandy loam\nClay content: 12 to 20 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel or channers\n0 to 5 percent cobbles\nReaction: strongly acid to neutral\nBA, ABt or Bw horizons (where present)\nHue: 5YR, 7.5YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 3 or 4 dry, 2 or 3 moist\nTexture: loam, sandy loam, clay loam\nClay content: 15 to 30 percent\nRock fragments: 0 to 25 percent\n0 to 15 percent gravel or channers\n0 to 10 percent cobbles\nReaction: moderately acid to slightly acid\nBt1 horizon\nHue: 5YR, 7.5YR\nValue: 4 5 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: loam, clay loam\nClay content: 18 to 32 percent\nRock fragments: 0 to 35 percent\n0 to 30 percent gravel\n0 to 15 percent cobbles\nReaction: moderately acid to slightly acid\nLower Bt horizons (Bt2, Bt3)\nHue: 5YR, 7.5YR\nValue: 5 dry, 3 or 4 moist\nChroma: 4 or 6 dry, 3 or 4 moist\nTexture: clay loam, loam\nClay content: 25 to 38 percent\nRock fragments: 0 to 60 percent\n0 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 15 percent stones\nReaction: strongly acid to moderately acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/D/DORST.json b/inst/extdata/OSD/D/DORST.json index c7fe7114ec..c642989071 100644 --- a/inst/extdata/OSD/D/DORST.json +++ b/inst/extdata/OSD/D/DORST.json @@ -1,8 +1,8 @@ { "SERIES": "DORST", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Dorst series consists of shallow, somewhat excessively drained soils formed in colluvium and residuum derived from granitic rocks. Dorst soils are on structural benches and mountain slopes in the Sierra Nevada Mountains. Slopes range from 15 to 60 percent. The mean annual precipitation is about 980 mm and the mean annual air temperature is about 6 degrees C.", "TAXONOMIC CLASS": { @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 3 to 9 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 18 to 40 cm\nDepth to lithic contact: 18 to 50 cm\nReaction: slightly to strongly acid\nBase saturation: less than 50 percent (by ammonium acetate)\nParticle size control section weighted average:\nRock fragments: 35 to 70 percent, with 15 to 65 percent gravel, 0 to 45 percent channers, 0 to20 percent cobbles, 0 to 50 percent stones, and 0 to 40 percent flagstones.\nClay content: 1 to 8 percent\nNaF pH: 8.5 to 11\nA horizon\nHue: 7.5YR or 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 2 moist\nTexture: coarse sand, loamy coarse sand, loamy sand\nClay content: 1 to 6 percent\nRock fragments: 15 to 65 percent\n0 to 45 percent gravel\n0 to 40 percent channers\n0 to 30 percent cobbles\n0 to 30 percent flagstones\n0 to 30 percent stones\nBw horizon\nHue: 7.5YR or 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 2 moist\nTexture: loamy coarse sand, loamy sand\nClay content: 1 to 6 percent\nRock fragments: 35 to 70 percent\n0 to 45 percent gravel\n0 to 40 percent channers\n0 to 30 percent cobbles\n0 to 35 percent flagstones\n0 to 35 percent stones\nC horizon (when present)\nHue: 10YR\nValue: 4 to 6 dry, 2 to 4 moist\nChroma: 2 or 3, dry or moist\nTexture: sand, loamy sand\nClay content: 1 to 4 percent\nRock fragments: 35 to 70 percent\n35 to 65 percent gravel\n0 to 45 percent channers\n0 to 15 percent cobbles\n0 to 15 percent flagstones\n0 to 15 percent stones" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 3 to 9 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 40 cm\nDepth to lithic contact: 25 to 50 cm\nReaction: slightly to strongly acid\nBase saturation: less than 50 percent (by ammonium acetate)\nParticle size control section weighted average:\nRock fragments: 35 to 70 percent, with 15 to 65 percent gravel, 0 to 45 percent channers, 0 to 20 percent cobbles, 0 to 50 percent stones, and 0 to 40 percent flagstones.\nClay content: 1 to 8 percent\nNaF pH: 8.5 to 11\nA horizon\nHue: 7.5YR or 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 2 moist\nTexture: coarse sand, loamy coarse sand, loamy sand\nClay content: 1 to 6 percent\nRock fragments: 15 to 65 percent\n0 to 45 percent gravel\n0 to 40 percent channers\n0 to 30 percent cobbles\n0 to 30 percent flagstones\n0 to 30 percent stones\nBw horizon\nHue: 7.5YR or 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 2 moist\nTexture: loamy coarse sand, loamy sand\nClay content: 1 to 6 percent\nRock fragments: 35 to 70 percent\n0 to 45 percent gravel\n0 to 40 percent channers\n0 to 30 percent cobbles\n0 to 35 percent flagstones\n0 to 35 percent stones\nC horizon (when present)\nHue: 10YR\nValue: 4 to 6 dry, 2 to 4 moist\nChroma: 2 or 3, dry or moist\nTexture: sand, loamy sand\nClay content: 1 to 4 percent\nRock fragments: 35 to 70 percent\n35 to 65 percent gravel\n0 to 45 percent channers\n0 to 15 percent cobbles\n0 to 15 percent flagstones\n0 to 15 percent stones" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/E/EDENCREEK.json b/inst/extdata/OSD/E/EDENCREEK.json index 670496be55..594581f895 100644 --- a/inst/extdata/OSD/E/EDENCREEK.json +++ b/inst/extdata/OSD/E/EDENCREEK.json @@ -1,10 +1,10 @@ { "SERIES": "EDENCREEK", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Edencreek series consists of moderately deep, well drained soils formed in colluvium over residuum weathered from granitic rocks. The Edencreek soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 60 percent. The mean annual precipitation is about 885 mm and the mean annual air temperature is about 13 degrees C.", + "OVERVIEW": "The Edencreek series consists of moderately deep, well drained soils formed in colluvium over residuum weathered from granitic rocks. The Edencreek soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 60 percent. The mean annual precipitation is about 835 mm and the mean annual air temperature is about 13 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Coarse-loamy, isotic, mesic Ultic Haploxeralfs" @@ -27,7 +27,7 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Edencreek soils are on convex backslopes of mountain slopes. Slopes range from 15 to 60 percent. These soils formed in colluvium over residuum derived from granite and granodiorite. Elevation is 970 to 1835 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 730 to 1025 mm and the mean annual air temperature is 10 to 15 degrees C. The frost free season is 165 to 245 days." + "content": "GEOGRAPHIC SETTING: The Edencreek soils are on convex backslopes of mountain slopes. Slopes range from 15 to 60 percent. These soils formed in colluvium over residuum derived from granite and granodiorite. Elevation is 980 to 1950 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 730 to 1005 mm and the mean annual air temperature is 9 to 15 degrees C. The frost free season is 165 to 245 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 28 to 65 cm.\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 2 to 28 cm\nArgillic Horizon 28 to 65 cm\nParalithic Contact 65 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7924008\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 28 to 65 cm.\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 2 to 28 cm\nArgillic Horizon 28 to 65 cm\nParalithic Contact 65 cm\nParalithic Materials 65 to 92 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7924008\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/F/FORGOTTEN.json b/inst/extdata/OSD/F/FORGOTTEN.json index fc8ae919b0..792d609825 100644 --- a/inst/extdata/OSD/F/FORGOTTEN.json +++ b/inst/extdata/OSD/F/FORGOTTEN.json @@ -1,10 +1,10 @@ { "SERIES": "FORGOTTEN", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "10/2019", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Forgotten series consists of very deep, moderately well drained soils formed in alluvium, colluvium, and till derived from granitic rocks. The Forgotten soils are on high gradient drainageways on mountain slopes, moraines, and glacial valley walls of the Sierra Nevada Mountains. Slopes range from 10 to 35 percent. The mean annual precipitation is about 860 mm and the mean annual air temperature is about 1 degree C.", + "OVERVIEW": "The Forgotten series consists of very deep, moderately well drained soils formed in alluvium, colluvium, and till derived from granitic rocks. The Forgotten soils are on high gradient drainageways on mountain slopes, moraines, and glacial valley walls of the Sierra Nevada Mountains. Slopes range from 10 to 45 percent. The mean annual precipitation is about 860 mm and the mean annual air temperature is about 1 degree C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Sandy-skeletal, isotic Oxyaquic Humicryepts" @@ -27,7 +27,7 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Forgotten soils are on linear to concave positions; they form in channels and floodplain steps of high-gradient drainageways on mountain slopes, glacial valley walls, and moraines. Slopes range from 10 to 35 percent. These soils formed in alluvium, colluvium, and till derived from granite and granodiorite. Elevation is 2570 to 3955 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 550 to 1505 mm and the mean annual air temperature is -1 to 5 degrees C. The frost free season is 45 to 95 days." + "content": "GEOGRAPHIC SETTING: The Forgotten soils are on linear to concave positions; they form in channels and floodplain steps of high-gradient drainageways on mountain slopes, glacial valley walls, and moraines. Slopes range from 10 to 45 percent. These soils formed in alluvium, colluvium, and till derived from granite and granodiorite. Elevation is 2570 to 3955 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 550 to 1505 mm and the mean annual air temperature is -1 to 5 degrees C. The frost free season is 45 to 95 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", @@ -35,7 +35,7 @@ }, "DRAINAGE AND PERMEABILITY": { "section": "DRAINAGE AND PERMEABILITY", - "content": "DRAINAGE AND PERMEABILITY: Moderately well drained, high to very high saturated hydraulic conductivity. Occasional flooding for very brief (4 to 48 hours) duration in April through June, no ponding. Seasonal high water table between 50 to 100 cm." + "content": "DRAINAGE AND PERMEABILITY: Moderately well drained, high to very high saturated hydraulic conductivity. Occasional to frequent flooding for very brief (4 to 48 hours) duration in April through June, no ponding. Seasonal high water table between 50 to 100 cm." }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", diff --git a/inst/extdata/OSD/G/GENERALGRANT.json b/inst/extdata/OSD/G/GENERALGRANT.json index dcc786a545..6aeff388ed 100644 --- a/inst/extdata/OSD/G/GENERALGRANT.json +++ b/inst/extdata/OSD/G/GENERALGRANT.json @@ -1,13 +1,13 @@ { "SERIES": "GENERALGRANT", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Generalgrant series consists of very deep, moderately well drained soils formed in slope alluvium derived from granite. The Generalgrant soils are on stream terraces and drainageways on mountain slopes of the Sierra Nevada Mountains. Slopes range from 5 to 45 percent. The mean annual precipitation is about 1050 mm and the mean annual air temperature is about 8 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Sandy, isotic, mesic Vitrandic Humixerepts" + "content": "TAXONOMIC CLASS: Sandy, isotic, mesic Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 26 to 101 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 1 to 48 cm\nRedox Concentrations 48 to 230 cm\nRedox Depletions with Chroma 2 or Less 95 to 130 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nPedon Type: OSD pedon Lab Source ID: KSSL\nPedon Purpose: soil survey inventory Lab Pedon #: 16N2139\nNASIS User Pedon ID: S2016CA019001\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 26 to 101 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 1 to 48 cm\nRedox Concentrations 95 to 230 cm\nRedox Depletions with Chroma 2 or Less 95 to 130 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nPedon Type: OSD pedon Lab Source ID: KSSL\nPedon Purpose: soil survey inventory Lab Pedon #: 16N2139\nNASIS User Pedon ID: S2016CA019001\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/G/GRATWELL.json b/inst/extdata/OSD/G/GRATWELL.json index 11a61c3fa8..24fbfe4248 100644 --- a/inst/extdata/OSD/G/GRATWELL.json +++ b/inst/extdata/OSD/G/GRATWELL.json @@ -1,13 +1,13 @@ { "SERIES": "GRATWELL", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Gratwell series consists of very deep, well drained soils formed in colluvium and/or slope alluvium over residuum derived from granodiorite and schist. The Gratwell soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 5 to 60 percent. The mean annual precipitation is about 1025 mm and the mean annual air temperature is about 10 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Coarse-loamy, isotic, mesic Vitrandic Humixerepts" + "content": "TAXONOMIC CLASS: Coarse-loamy, isotic, mesic Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 33 to 108 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 8 to 81 cm\nCambic Horizon 81 to 108 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2015CA7925014\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 33 to 108 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 8 to 42 cm\nCambic Horizon 42 to 108 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2015CA7925014\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/H/HALSTEAD.json b/inst/extdata/OSD/H/HALSTEAD.json index a20b178593..2a39c7e581 100644 --- a/inst/extdata/OSD/H/HALSTEAD.json +++ b/inst/extdata/OSD/H/HALSTEAD.json @@ -1,37 +1,37 @@ { "SERIES": "HALSTEAD", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Halstead series consists of moderately deep, well drained soils formed in colluvium derived from granitic rocks. The Halstead soils are on glacial valley walls and mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 60 percent. The mean annual precipitation is about 940 millimeters and the mean annual air temperature is about 6 degrees C.", + "OVERVIEW": "The Halstead series consists of moderately deep, somewhat excessively drained soils formed in colluvium and till derived from granitic rocks. The Halstead soils are on glacial valley walls and mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 60 percent. The mean annual precipitation is about 940 millimeters and the mean annual air temperature is about 6 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Sandy-skeletal, isotic, frigid Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Halstead gravelly loamy sand on a north facing (12 degree), 30 percent slope under Sierra juniper, Jeffrey pine, greanleaf manzanita, and sagebrush at an elevation of 2271 meters. When described on September 11, 2014 the soil was dry throughout. Colors are for dry soils unless otherwise noted.\nOi--0 to 6 cm; very dark brown (10YR 2/2) slightly decomposed plant material, black (10YR 2/1) moist; slightly acid (pH 6.2); abrupt smooth boundary. (0 to 10 cm thick)\nA--6 to 14 cm; dark grayish brown (10YR 4/2) gravelly loamy sand, very dark gray (10YR 3/1) moist; 4 percent clay; moderate very fine and fine granular structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, medium, coarse and very coarse, and many fine roots throughout; common very fine and many fine dendritic tubular, and common medium irregular pores; 12 percent subangular strongly cemented granite gravel, 2 percent subangular strongly cemented granite cobbles; NaF pH ; neutral (pH 6.6); abrupt smooth boundary. (6 to 20 cm thick)\nBw--14 to 30 cm; olive brown (2.5Y 4/4) gravelly loamy sand, very dark brown (10YR 2/2) moist; 4 percent clay; weak fine and medium subangular blocky structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse, and many very coarse roots throughout; common very fine and fine dendritic tubular, and common medium and very coarse irregular pores; 20 percent subangular strongly cemented granite gravel, 5 percent subangular strongly cemented granite cobbles; NaF pH ; slightly acid (pH 6.4); clear smooth boundary. (12 to 40 cm thick)\nC--30 to 66 cm; brown (10YR 4/3) extremely gravelly loamy fine sand, very dark brown (10YR 2/2) moist; 3 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; few very fine and fine, and common medium, coarse, and very coarse roots throughout; common fine and medium dendritic tubular, and common medium and coarse irregular pores; 48 percent subangular strongly cemented granite gravel, 10 percent subangular strongly cemented granite cobbles; NaF pH : moderately acid (pH 6.0); clear smooth boundary. (10 to 50 cm thick)\nR--66 to 200 cm; strongly cemented granite bedrock, fractured at intervals of 10 to <45 cm; common medium roots around fragments and common coarse roots around fragments." + "content": "TYPICAL PEDON: Halstead gravelly loamy sand on a north facing (12 degree), 30 percent slope under Sierra juniper, Jeffrey pine, greenleaf manzanita, and sagebrush at an elevation of 2271 meters. When described on September 11, 2014 the soil was dry throughout. Colors are for dry soils unless otherwise noted.\nOi--0 to 6 cm; very dark brown (10YR 2/2) slightly decomposed plant material, black (10YR 2/1) moist; slightly acid (pH 6.2); abrupt smooth boundary. (0 to 10 cm thick)\nA--6 to 14 cm; dark grayish brown (10YR 4/2) loamy sand, very dark gray (10YR 3/1) moist; 4 percent clay; moderate very fine and fine granular structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, medium, coarse and very coarse, and many fine roots throughout; common very fine and many fine dendritic tubular, and common medium irregular pores; 12 percent subangular strongly cemented granite gravel, 2 percent subangular strongly cemented granite cobbles; NaF pH 10.0; neutral (pH 6.6); abrupt smooth boundary. (6 to 20 cm thick)\nBw--14 to 30 cm; olive brown (2.5Y 4/4) gravelly loamy sand, very dark brown (10YR 2/2) moist; 4 percent clay; weak fine and medium subangular blocky structure; slightly hard, friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse, and many very coarse roots throughout; common very fine and fine dendritic tubular, and common medium and very coarse irregular pores; 20 percent subangular strongly cemented granite gravel, 5 percent subangular strongly cemented granite cobbles; NaF pH 10.5; slightly acid (pH 6.4); clear smooth boundary. (12 to 40 cm thick)\nC--30 to 66 cm; brown (10YR 4/3) very gravelly loamy fine sand, very dark brown (10YR 2/2) moist; 3 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; few very fine and fine, and common medium, coarse, and very coarse roots throughout; common fine and medium dendritic tubular, and common medium and coarse irregular pores; 48 percent subangular strongly cemented granite gravel, 10 percent subangular strongly cemented granite cobbles; NaF pH 11.0: moderately acid (pH 6.0); clear smooth boundary. (10 to 50 cm thick)\nR--66 to 200 cm; strongly cemented granite bedrock, fractured at intervals of 10 to <45 cm; common medium roots around fragments and common coarse roots around fragments." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, 0.8 kilometer NW of Roaring River ranger station; USGS 7.5 minute topographic quadrangle: Sphinx Lakes, California; WGS84 36.715400 latitude and -118.591189 longitude; UTM zone 11 4064482 meters N 357891 meters E WGS84." + "content": "TYPE LOCATION: Tulare County, California, 0.8 kilometer NW of Roaring River ranger station; USGS 7.5 minute topographic quadrangle: Sphinx Lakes, California; WGS84 36.715400 latitude and -118.591189 longitude; UTM zone 11 4064482 meters N 357891 meters E WGS84." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 75 cm\nDepth to lithic contact: 50 to 100 cm\nReaction: slightly to moderately acid\nBase saturation: less than 50 percent in some or all parts of the epipedon (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm or to bedrock.\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 5 to 50 percent gravel, 0 to 35 percent cobbles, 0 to 25 percent stones, 0 to 5 percent boulders, 0 to 15 percent channers, and 0 to 15 percent flagstones.\nClay content: 2 to 6 percent\nNaF pH: 8.5 to 10.5\nA horizon\nHue: 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 to 3 moist\nTexture: loamy sand, loamy fine sand\nClay content: 3 to 8 percent\nRock fragments: 5 to 60 percent\n0 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 15 percent stones\nReaction: moderately acid to neutral\nBw horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 6 dry, 2 to 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy fine sand\nClay content: 2 to 6 percent\nRock fragments: 5 to 60 percent\n0 to 60 percent gravel\n0 to 25 percent cobbles\n0 to 25 percent stones\n0 to 5 percent boulders\n0 to 15 percent channers\n0 to 15 percent flagstones\nReaction: moderately to slightly acid\nC horizon\nHue: 10YR, 2.5Y\nValue: 4 to 7 dry, 2 to 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy coarse sand\nClay content: 2 to 6 percent\nRock fragments: 5 to 60 percent\n0 to 50 percent gravel\n0 to 45 percent cobbles\n0 to 25 percent stones\n0 to 5 percent boulders\n0 to 15 percent channers\n0 to 15 percent flagstones\nReaction: strongly to slightly acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 75 cm\nDepth to lithic contact: 50 to 100 cm\nReaction: slightly to moderately acid\nBase saturation: less than 50 percent in some or all parts of the epipedon (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm or to bedrock.\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 5 to 50 percent gravel, 0 to 35 percent cobbles, 0 to 25 percent stones, 0 to 5 percent boulders, 0 to 15 percent channers, and 0 to 15 percent flagstones.\nClay content: 2 to 6 percent\nNaF pH: 9.0 to 11.0\nA horizon\nHue: 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 to 3 moist\nTexture: loamy sand, loamy fine sand\nClay content: 3 to 8 percent\nRock fragments: 5 to 60 percent\n0 to 35 percent gravel\n0 to 25 percent cobbles\n0 to 15 percent stones\nReaction: moderately acid to neutral\nBw horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 6 dry, 2 to 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy fine sand\nClay content: 2 to 6 percent\nRock fragments: 5 to 60 percent\n0 to 60 percent gravel\n0 to 25 percent cobbles\n0 to 25 percent stones\n0 to 5 percent boulders\n0 to 15 percent channers\n0 to 15 percent flagstones\nReaction: moderately to slightly acid\nC horizon\nHue: 10YR, 2.5Y\nValue: 4 to 7 dry, 2 to 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy fine sand, loamy sand, loamy coarse sand\nClay content: 2 to 6 percent\nRock fragments: 15 to 60 percent\n0 to 50 percent gravel\n0 to 45 percent cobbles\n0 to 25 percent stones\n0 to 5 percent boulders\n0 to 15 percent channers\n0 to 15 percent flagstones\nReaction: strongly to slightly acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", - "content": "COMPETING SERIES: These are the Doncecil, Kanawyer, Pajo (MLRA 43B), Tripod (MLRA 43B), and Windowpeak soils. Doncecil, Kanawyer, Tripod, and Windowpeak soils do not have a lithic contact within 150 cm of the mineral soil surface. Pajo and Tripod soils have ashy textures in the epipedon." + "content": "COMPETING SERIES: These are the Doncecil, Kanawyer, Pajo (MLRA 43B), Tripod (MLRA 43B), and Windowpeak soils. Doncecil, Kanawyer, Tripod, and Windowpeak soils do not have a lithic contact within 150 cm of the mineral soil surface. Pajo and Tripod soils have ashy textures in the epipedon." }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Halstead soils are on convex backslopes of mountain slopes and glacial valley walls. Slopes range from 15 to 60 percent. These soils formed in colluvium derived from granite and granodiorite. Elevation is 1745 to 2870 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 445 to 1215 mm and the mean annual air temperature is 3 to 10 degrees C. The frost free season is 75 to 175 days." + "content": "GEOGRAPHIC SETTING: The Halstead soils are on convex backslopes of mountain slopes and glacial valley walls. Slopes range from 15 to 60 percent. These soils formed in colluvium and till derived from granite and granodiorite. Elevation is 1745 to 2870 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 445 to 1215 mm and the mean annual air temperature is 3 to 10 degrees C. The frost free season is 75 to 175 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", - "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Bellecanyon, Dorst, Lackey, and Windowpeak soils. Bellcanyon soils formed in glacial outwash, are on linear footslopes of ground moraines, and are more than 150 cm to a lithic contact. Dorst soils formed on linear to convex summits and shoulders of structural benches on mountain slopes and have a lithic contact within 50 cm. Lackey soils formed in colluvium on linear backslopes of mountain slopes and are more than 150 cm to a lithic contact. Windowpeak soils formed in colluvium and till on linear backslopes and footslopes of moraines and mountainslopes, and are more than 150 cm to a lithic contact." + "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Bellecanyon, Dorst, Lackey, and Windowpeak soils. Bellecanyon soils formed in glacial outwash, are on linear footslopes of ground moraines, and are more than 150 cm to a lithic contact. Dorst soils formed on linear to convex summits and shoulders of structural benches on mountain slopes and have a lithic contact within 50 cm. Lackey soils formed in colluvium on linear backslopes of mountain slopes and are more than 150 cm to a lithic contact. Windowpeak soils formed in colluvium and till on linear backslopes and footslopes of moraines and mountainslopes, and are more than 150 cm to a lithic contact." }, "DRAINAGE AND PERMEABILITY": { "section": "DRAINAGE AND PERMEABILITY", diff --git a/inst/extdata/OSD/H/HOCKETT.json b/inst/extdata/OSD/H/HOCKETT.json index bf6428e3ea..2130d64c70 100644 --- a/inst/extdata/OSD/H/HOCKETT.json +++ b/inst/extdata/OSD/H/HOCKETT.json @@ -1,13 +1,13 @@ { "SERIES": "HOCKETT", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Hockett series consists of moderately deep, well drained soils formed in slope alluvium, colluvium, and till over residuum derived from granitic rocks. The Hockett soils are on structural benches in the Sierra Nevada mountains. Slopes range from 1 to 25 percent. The mean annual precipitation is about 720 mm and the mean annual air temperature is about 4 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Sandy, isotic, frigid Vitrandic Humixerepts" + "content": "TAXONOMIC CLASS: Sandy, isotic, frigid Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 50 cm\nDepth to lithic contact: 50 to 100 cm\nBase saturation: less than 50 percent. (By ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 2.0 percent (by weight) in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 15 to 30 percent, with 0 to 30 percent gravel, 0 to 30 percent paragravel, 0 to 15 percent cobbles, and 0 to 15 percent stones\nClay content: 2 to 8 percent\nNaF pH: 8.5 to 11.5\nA horizon\nHue: 7.5 YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 to 4 dry, 2 or 3 moist\nTexture: sandy loam, loamy fine sand, loamy sand, loamy coarse sand\nClay content: 2 to 8 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 5 percent cobbles\nPararock fragments: 0 to 15 percent paragravel\nReaction: very strongly to moderately acid\nBw horizon(s)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 7 dry, 3 to 5 moist\nChroma: 3 to 6 dry, 2 to 4 moist\nTexture: loamy fine sand, loamy sand, loamy coarse sand\nClay content: 2 to 8 percent\nRock fragments: 0 to 30 percent\n0 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\nPararock fragments: 0 to 30 percent paragravel\nReaction: very strongly to moderately acid\nC horizon(s), where present\nHue: 10YR, 2.5Y\nValue: 6 or 7 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: fine sandy loam, sandy loam, loamy fine sand, loamy sand\nClay content: 2 to 6 percent\nRock fragments: 0 to 30 percent\n0 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\nPararock fragments: 0 to 10 percent paragravel\nReaction: strongly to moderately acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 25 to 50 cm\nDepth to lithic contact: 50 to 100 cm\nBase saturation: less than 50 percent. (By ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 2.0 percent (by weight) in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 15 to 30 percent, with 0 to 30 percent gravel, 0 to 30 percent paragravel, 0 to 15 percent cobbles, and 0 to 15 percent stones\nClay content: 2 to 8 percent\nNaF pH: 8.5 to 11.5\nA horizon\nHue: 7.5 YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 to 4 dry, 2 or 3 moist\nTexture: sandy loam, loamy fine sand, loamy sand, loamy coarse sand\nClay content: 2 to 8 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 5 percent cobbles\nPararock fragments: 0 to 15 percent paragravel\nReaction: very strongly to moderately acid\nBw horizon(s)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 7 dry, 3 to 5 moist\nChroma: 3 to 6 dry, 2 to 4 moist\nTexture: loamy fine sand, loamy sand, loamy coarse sand\nClay content: 2 to 8 percent\nRock fragments: 0 to 40 percent\n0 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\nPararock fragments: 0 to 30 percent paragravel\nReaction: very strongly to moderately acid\nC horizon(s), where present\nHue: 10YR, 2.5Y\nValue: 6 or 7 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: fine sandy loam, sandy loam, loamy fine sand, loamy sand\nClay content: 1 to 6 percent\nRock fragments: 0 to 35 percent\n0 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\nPararock fragments: 0 to 10 percent paragravel\nReaction: strongly to moderately acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/I/ISOSCELES.json b/inst/extdata/OSD/I/ISOSCELES.json index 6b41f5308b..84f154ef12 100644 --- a/inst/extdata/OSD/I/ISOSCELES.json +++ b/inst/extdata/OSD/I/ISOSCELES.json @@ -1,8 +1,8 @@ { "SERIES": "ISOSCELES", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "10/2019", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Isosceles series consists of very shallow and shallow, well drained soils formed in residuum weathered from granitic rocks. The Isosceles soils are on structural benches on cirques and mountain slopes of the Sierra Nevada Mountains. Slopes range from 2 to 30 percent. The mean annual precipitation is about 1075 mm and the mean annual air temperature is about 2 degrees C.", "TAXONOMIC CLASS": { @@ -11,15 +11,15 @@ }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Isosceles flaggy sandy loam on a southwest-facing (215 degree), 6 percent slope under threadleaf sedge and scattered whitebark pine at an elevation of 3354 meters. (Colors are for dry soils unless otherwise noted. When described on August 12, 2013 the soil was dry to 8 cm.)\nA1--0 to 8 cm; very dark grayish brown (10YR 3/2) flaggy sandy loam, very dark brown (10YR 2/2) moist; 5 percent clay; moderate very fine granular structure; soft, very friable, nonsticky, nonplastic; many very fine and common fine roots throughout; common very fine irregular pores; 5 percent indurated granite gravel, 5 percent indurated granite channers, 15 percent indurated granite flagstones; NaF pH 10.5; very strongly acid (pH 4.6); gradual smooth boundary.\nA2--8 to 19 cm; brown (10YR 4/3) sandy loam, very dark brown (10YR 2/2) moist; 7 percent clay; moderate fine granular structure; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; common very fine irregular pores; 5 percent indurated granite gravel, 2 percent indurated granite channers, 5 percent indurated granite flagstones; NaF pH 10.5; very strongly acid (pH 4.6); clear smooth boundary.\nA3--19 to 40 cm; brown (10YR 4/3) sandy loam, dark brown (10YR 3/3) moist; 6 percent clay; weak fine granular structure; soft, very friable, slightly sticky, nonplastic; few very fine and fine roots throughout; common very fine irregular pores; 5 percent indurated granite gravel, 2 percent indurated granite channers; NaF pH 10.5; very strongly acid (pH 4.8); abrupt smooth boundary. (combined thickness of A horizons is 10 to 40 cm)\nR--40 cm; Indurated granite bedrock, fractured at intervals of <200 cm." + "content": "TYPICAL PEDON: Isosceles loamy fine sand on a northeast facing (40 degree), 2 percent slope under a cover of threadleaf sedge, Parry's rush, and scattered whitebark pine at an elevation of 3368 meters. (Colors are for dry soils unless otherwise noted. When described on July 21, 2013 the soil was dry throughout.)\nA--0 to 10 cm; dark grayish brown (10YR 4/2) loamy fine sand, very dark brown (10YR 2/2) moist; 4 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; many very fine and common fine roots throughout; many very fine irregular pores; 5 percent subangular indurated granite gravel, 1 percent subangular indurated granite cobbles; NaF pH 10.0; strongly acid (pH 5.2); abrupt wavy boundary. (3 to 30 cm thick)\nBA--10 to 24 cm; brown (10YR 5/3) gravelly fine sandy loam, very dark grayish brown (10YR 3/2) moist; 10 percent clay; weak very fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; many very fine, and common fine and medium roots throughout; common very fine irregular pores; 15 percent subangular indurated granite gravel, 5 percent subangular indurated granite cobbles; NaF pH 10.0; strongly acid (pH 5.2); clear wavy boundary. (0 to 15 cm thick)\nBw--24 to 44 cm; yellowish brown (10YR 5/4) gravelly fine sandy loam, brown (10YR 4/3) moist; 14 percent clay; weak medium subangular blocky structure; slightly hard, friable, slightly sticky, nonplastic; common fine and medium roots throughout; common very fine and fine tubular pores; 2 percent fine distinct irregular masses of oxidized iron with clear boundaries on surfaces along pores; 10 percent subangular indurated granite gravel, 5 percent subangular indurated granite cobbles; NaF pH 10.0; strongly acid (pH 5.2); very abrupt wavy boundary. (5 to 35 cm thick)\nR--44 to 200 cm; indurated granite bedrock, fractured at intervals of greater than 200 cm." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Fresno County, California, near Twin Lakes in Kings Canyon National Park; USGS 7.5 minute topographic quadrangle: Mount Pinchot, California; WGS84 36.917828 latitude and -118.392931 longitude; UTM zone 11 4086663 meters N 375926 meters E NAD83." + "content": "TYPE LOCATION: Fresno County, California, about 0.5 km north of Lake Marjorie, Kings Canyon National Park; USGS 7.5 minute topographic quadrangle: Mount Pinchot, California; WGS84 36.951008 latitude and -118.433464 longitude; UTM zone 11 4090397 meters N 372372 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is -1 to 5 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a cryic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 10 to 40 cm\nDepth to lithic contact: 10 to 50 cm\nOrganic matter: 1 to 5 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate).\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 25 percent gravel, 0 to 15 percent cobbles, 0 to 5 percent stones, 0 to 15 percent channers, and 0 to 15 percent flagstones.\nClay content: 4 to 12 percent\nNaF pH: 10.0 to 11.0\nA horizons\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, fine sandy loam\nClay content: 2 to 12 percent\nRock fragments: 0 to 35 percent\n0 to 25 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\n0 to 15 percent channers\n0 to 15 percent flagstones\nReaction: very strongly to moderately acid\nBw horizons (where present)\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 3 or 4 dry, 2 to 4 moist\nTexture: sandy loam, fine sandy loam\nClay content: 5 to 12 percent\nRock fragments: 10 to 35 percent\n10 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\nReaction: extremely to moderately acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is -1 to 5 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a cryic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 10 to 40 cm\nDepth to lithic contact: 10 to 50 cm\nOrganic matter: 1 to 5 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate).\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 25 percent gravel, 0 to 15 percent cobbles, 0 to 5 percent stones, 0 to 15 percent channers, and 0 to 15 percent flagstones.\nClay content: 4 to 12 percent\nNaF pH: 10.0 to 11.0\nA horizons\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: loamy fine sand, sandy loam, fine sandy loam\nClay content: 2 to 12 percent\nRock fragments: 0 to 35 percent\n0 to 25 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\n0 to 15 percent channers\n0 to 15 percent flagstones\nReaction: very strongly to moderately acid\nBA or Bw horizons (where present)\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 to 4 moist\nChroma: 3 or 4 dry, 2 to 4 moist\nTexture: sandy loam, fine sandy loam\nClay content: 5 to 15 percent\nRock fragments: 0 to 35 percent\n0 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\nReaction: extremely to moderately acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -39,7 +39,7 @@ }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is whitebark pine, western needlegrass, threadleaf sedge, mountain pride, Ross sedge, bottlebrush squirreltail,and Parry's rush. Sierra juniper may be present in some areas." + "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is whitebark pine, western needlegrass, threadleaf sedge, mountain pride, Ross sedge, bottlebrush squirreltail, and Parry's rush. Sierra juniper may be present in some areas." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 25 to 40 cm.\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 0 to 40 cm\nLithic Contact 40 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2013CA7927511\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 25 to 40 cm.\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 0 to 24 cm\nLithic Contact 44 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2013CA7925002\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/K/KAWEAH.json b/inst/extdata/OSD/K/KAWEAH.json index 2496787a90..fa4ece0dcc 100644 --- a/inst/extdata/OSD/K/KAWEAH.json +++ b/inst/extdata/OSD/K/KAWEAH.json @@ -1,10 +1,10 @@ { "SERIES": "KAWEAH", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Kaweah series consists of very deep, well drained soils formed in colluvium derived from metasedimentary rock. The Kaweah soils are on steep mountain slopes of the Sierra Nevada Mountains. Slopes range from 30 to 90 percent. The mean annual precipitation is about 895 mm and the mean annual air temperature is about 12 degrees C.", + "OVERVIEW": "The Kaweah series consists of very deep, well drained soils formed in colluvium derived from granitic and metasedimentary rock. The Kaweah soils are on steep mountain slopes of the Sierra Nevada Mountains. Slopes range from 30 to 90 percent. The mean annual precipitation is about 895 mm and the mean annual air temperature is about 12 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, mesic Pachic Ultic Haploxerolls" @@ -15,7 +15,7 @@ }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, on the Ladybug Trail from South Fork Rd in Sequoia National Park; USGS 7.5 minute topographic quadrangle: Dennison Peak, California; WGS84 36.348557 latitude and -118.753191 longitude; UTM zone 11 4024037 meters N 342679 meters E NAD83." + "content": "TYPE LOCATION: Tulare County, California, on the Ladybug Trail from South Fork Rd in Sequoia National Park; USGS 7.5 minute topographic quadrangle: Dennison Peak, California; WGS84 36.348557 latitude and -118.753191 longitude; UTM zone 11 4024037 meters N 342679 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", @@ -27,11 +27,11 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Kaweah soils are on steep linear to concave backslopes of mountain slopes or drainageways. Slopes range from 30 to 90 percent. These soils formed in colluvium derived from metasedimentary rock. Elevation is 900 to 1940 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 730 to 1030 mm and the mean annual air temperature is 10 to 15 degrees C. The frost free season is 160 to 245 days." + "content": "GEOGRAPHIC SETTING: The Kaweah soils are on steep linear to concave backslopes of mountain slopes or drainageways. Slopes range from 30 to 90 percent. These soils formed in colluvium derived from granitic and metasedimentary rocks. Elevation is 900 to 1940 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 730 to 1030 mm and the mean annual air temperature is 10 to 15 degrees C. The frost free season is 160 to 245 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", - "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Colonymill, Ladybug, and Whiskeylog soils. The Colonymill soils are on broadly convex, less steep backslopes of mountain slopes and have a clay increase that meets the requirements of an argillic horizon. The Ladybug soils are on shoulders of mountain slopes and are less than 50 cm to a lithic contact. The Whiskeylog soils are on convex mountain slopes and lack a mollic epipedon (dark surface)." + "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Colonymill, Ladybug, and Whiskeylog soils. The Colonymill soils are on broadly convex backslopes of mountain slopes and have an argillic horizon. The Ladybug soils are on shoulders of mountain slopes, have an argillic horizon, and are less than 150 cm to a lithic contact. The Whiskeylog soils are on convex mountain slopes and have an argillic horizon but lack a mollic epipedon (dark surface)." }, "DRAINAGE AND PERMEABILITY": { "section": "DRAINAGE AND PERMEABILITY", diff --git a/inst/extdata/OSD/L/LACKEY.json b/inst/extdata/OSD/L/LACKEY.json index b6ba68b94c..5b9e0a6898 100644 --- a/inst/extdata/OSD/L/LACKEY.json +++ b/inst/extdata/OSD/L/LACKEY.json @@ -1,25 +1,25 @@ { "SERIES": "LACKEY", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Lackey series consists of very deep, somewhat excessively drained soils formed in colluvium and till over residuum weathered from granitic rocks. The Lackey soils are on mountain slopes and moraines of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 800 mm and the mean annual air temperature is about 6 degrees C.", + "OVERVIEW": "The Lackey series consists of very deep, somewhat excessively drained soils formed in colluvium and till weathered from granitic rocks. The Lackey soils are on mountain slopes and moraines of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 800 mm and the mean annual air temperature is about 6 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Sandy-skeletal, isotic, frigid Vitrandic Xerorthents" + "content": "TAXONOMIC CLASS: Sandy-skeletal, isotic, frigid Vitrandic Xerorthents" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Lackey gravelly loamy sand on an east facing (110 degree), 62 percent slope under Jeffrey pine, western white pine, greenleaf manzanita, and white fir at an elevation of 2378 meters. (Colors are for dry soils unless otherwise noted. When described on June 14, 2014 the soil was dry to 12 cm.)\nOi--0 to 2 cm; yellowish brown (10YR 5/4) slightly decomposed plant material, yellowish brown (10YR 5/4) moist; about 100 percent fiber, 90 percent rubbed; moderately acid (pH 6.0); abrupt smooth boundary. (0 to 10 cm thick)\nA--2 to 12 cm; grayish brown (10YR 5/2) gravelly loamy sand, brown (10YR 4/3) moist; 5 percent clay; weak fine and medium subangular blocky parts to structureless single grain; loose, loose, nonsticky, nonplastic; many very fine roots throughout; many very fine and fine interstitial pores; 25 percent subangular very strongly cemented granite fine gravel; NaF pH 10.5; neutral (pH 6.8); clear smooth boundary. (5 to 30 cm thick)\nAB--12 to 32 cm; pale brown (10YR 6/3) gravelly loamy sand, brown (10YR 4/3) moist; 6 percent clay; weak fine and medium subangular blocky parts to structureless single grain; loose, loose, nonsticky, nonplastic; many very fine and common fine, medium, and coarse roots throughout; many very fine and fine, and common medium interstitial pores; 20 percent subangular very strongly cemented granite fine gravel, 10 percent subrounded very strongly cemented granite stones; NaF pH 10.5; slightly acid (pH 6.4); clear smooth boundary. (0 to 30 cm thick)\nBw--32 to 55 cm; light gray (10YR 7/2) gravelly loamy sand, brown (10YR 4/3) moist; 6 percent clay; weak fine subangular blocky parts to structureless single grain; loose, loose, nonsticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; many very fine and fine, and common medium interstitial pores; 30 percent subrounded very strongly cemented granite fine gravel; NaF pH 9.5; moderately acid (pH 5.8); gradual smooth boundary. (15 to 75 cm thick)\nC1--55 to 110 cm; light gray (10YR 7/2) very gravelly loamy coarse sand, grayish brown (10YR 5/2) moist; 5 percent clay; weak very fine subangular blocky parts to structureless single grain; loose, loose, nonsticky, nonplastic; few very fine, and common fine, medium, coarse, and very coarse roots throughout; common very fine, fine, and medium interstitial pores; 40 percent subrounded very strongly cemented granite fine gravel, 15 percent subrounded weakly cemented granite parastones; NaF pH 9.0; strongly acid (pH 5.4); gradual smooth boundary.\nC2--110 to 155 cm; white (10YR 8/1) very gravelly loamy coarse sand, pale brown (10YR 6/3) moist; 4 percent clay; structureless massive; loose, loose, nonsticky, nonplastic; few fine and medium roots throughout; 45 percent subrounded strongly cemented granite gravel; NaF pH 8.5; strongly acid (pH 5.2).\nCr--155 to 187 cm; weakly cemented granite bedrock." + "content": "TYPICAL PEDON: Lackey cobbly loamy sand on a northeast facing (50 degree), 53 percent slope under a canopy of Jeffrey pine and white fir at an elevation of 2457 meters. (Colors are for dry soils unless otherwise noted. When described on September 14, 2014 the soil was dry throughout.)\nOi--0 to 7 cm; yellowish brown (10YR 5/4) slightly decomposed plant material, dark yellowish brown (10YR 4/4) moist; very strongly acid (pH 5.0); clear smooth boundary. (0 to 10 cm thick)\nA--7 to 16 cm; grayish brown (10YR 5/2) cobbly loamy sand, very dark grayish brown (10YR 3/2) moist; 6 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, and medium roots throughout; many very fine irregular pores; 10 percent subrounded indurated granite gravel, 10 percent subrounded indurated granite cobbles, 5 percent subrounded indurated granite stones; NaF pH 9.0; slightly acid (pH 6.4); clear smooth boundary. (5 to 30 cm thick)\nBw1--16 to 34 cm; pale brown (10YR 6/3) very cobbly loamy sand, brown (10YR 4/3) moist; 6 percent clay; weak fine subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, and medium roots throughout; many very fine irregular pores; 15 percent subrounded indurated granite gravel, 15 percent subrounded indurated granite cobbles, 5 percent subrounded indurated granite stones; NaF pH 9.0; moderately acid (pH 6.0); gradual smooth boundary.\nBw2--34 to 68 cm; pale brown (10YR 6/3) very cobbly loamy sand, brown (10YR 4/3) moist; 5 percent clay; weak fine subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; many very fine irregular pores; 25 percent subrounded indurated granite gravel, 20 percent subrounded indurated granite cobbles, 5 percent subrounded indurated granite stones; NaF pH 9.0; moderately acid (pH 5.8); clear smooth boundary. (combined thickness of Bw horizons is 15 to 75 cm)\nC1--68 to 92 cm; pale brown (10YR 6/3) very gravelly sand, brown (10YR 4/3) moist; 3 percent clay; structureless single grain; loose, loose, nonsticky, nonplastic; common very fine , fine, medium, and coarse roots throughout; many very fine irregular pores; 30 percent subrounded indurated granite gravel, 15 percent subrounded indurated granite cobbles, 2 percent subrounded indurated granite stones; NaF pH 9.0; moderately acid (pH 5.8); gradual smooth boundary.\nC2--92 to 150 cm; light brownish gray (2.5Y 6/2) very gravelly sand, dark grayish brown (2.5Y 4/2) moist; 2 percent clay; structureless single grain; loose, loose, nonsticky, nonplastic; common fine and medium roots throughout; many very fine interstitial pores; 30 percent subrounded indurated granite gravel, 15 percent subrounded indurated granite cobbles, 2 percent subrounded indurated granite stones; NaF pH 9.0; moderately acid (pH 5.8)." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Fresno County, California, off the Don Cecil trail; USGS 7.5 minute topographic quadrangle: Cedar Grove, California; WGS84 36.773238 latitude and -118.712750 longitude; UTM zone 11 4071085 meters N 347148 meters E NAD83." + "content": "TYPE LOCATION: Tulare County, California, Deadman's Canyon; USGS 7.5 minute topographic quadrangle: Sphinx Lakes, California; WGS84 36.705306 latitude and -118.585094 longitude; UTM zone 11 4063353 meters N 358417 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 100 days).\nDiagnostic Feature(s):\nOchric epipedon thickness: 18 cm\nDepth to paralithic contact: greater than 150 cm\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm.\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 80 percent, with 15 to 50 percent gravel, 0 to 35 percent cobbles, 0 to 35 percent stones and 0 to 35 percent boulders.\nClay content: 1 to 10 percent\nNaF pH: 8.5 to 11.0\nA horizon (and AB horizons, where present)\nHue: 10YR\nValue: 4 to 6 dry, 2 to 4 moist\nChroma: 2 or 3, dry or moist\nTexture: loamy sand, loamy coarse sand\nClay content: 1 to 12 percent\nRock fragments: 15 to 75 percent\n10 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 15 percent stones\n0 to 15 percent boulders\nReaction: strongly acid to neutral\nBw horizon(s)\nHue: 10YR\nValue: 5 to 7 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: loamy sand, loamy coarse sand, coarse sand\nClay content: 1 to 10 percent\nRock fragments: 15 to 80 percent\n15 to 45 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 35 percent boulders\nReaction: strongly to slightly acid\nC horizon(s)\nHue: 10YR, 2.5Y\nValue: 5 to 8 dry, 3 to 5 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy coarse sand, coarse sand\nClay content: 1 to 10 percent\nRock fragments: 15 to 85 percent\n15 to 60 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 35 percent boulders\nPararock fragments: 0 to 15 percent\nReaction: very strongly to slightly acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 100 days).\nDiagnostic Feature(s):\nOchric epipedon thickness: 18 cm\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 80 percent, with 15 to 50 percent gravel, 0 to 35 percent cobbles, 0 to 35 percent stones and 0 to 35 percent boulders.\nClay content: 1 to 10 percent\nNaF pH: 8.5 to 11.0\nA horizon (and AB horizons, where present)\nHue: 10YR\nValue: 4 to 6 dry, 2 to 4 moist\nChroma: 2 or 3, dry or moist\nTexture: loamy sand, loamy coarse sand\nClay content: 1 to 12 percent\nRock fragments: 10 to 75 percent\n10 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 15 percent stones\n0 to 15 percent boulders\nReaction: strongly acid to neutral\nBw horizon(s)\nHue: 10YR\nValue: 5 to 7 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: loamy sand, loamy coarse sand, coarse sand\nClay content: 1 to 10 percent\nRock fragments: 15 to 80 percent\n15 to 45 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 35 percent boulders\nReaction: strongly to slightly acid\nC horizon(s)\nHue: 10YR, 2.5Y\nValue: 5 to 8 dry, 3 to 5 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, sand, coarse sand\nClay content: 1 to 10 percent\nRock fragments: 15 to 85 percent\n15 to 60 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 35 percent boulders\nPararock fragments: 0 to 15 percent\nReaction: very strongly to slightly acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -39,7 +39,7 @@ }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is white fir, Jeffrey pine, western white pine, greenleaf manzanita, and chinquapin." + "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is red fir, white fir, Jeffrey pine, lodgepole pine, western white pine, greenleaf manzanita, and chinquapin." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 27 to 102 cm\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 0 to 18 cm\nParalithic Contact 155 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7921008\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 32 to 107 cm\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 0 to 18 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7925076\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/L/LADDERLAKE.json b/inst/extdata/OSD/L/LADDERLAKE.json index 8a686431eb..f9a79725c6 100644 --- a/inst/extdata/OSD/L/LADDERLAKE.json +++ b/inst/extdata/OSD/L/LADDERLAKE.json @@ -1,8 +1,8 @@ { "SERIES": "LADDERLAKE", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Ladderlake series consists of very deep, poorly or very poorly drained soils formed in alluvium and/or till derived from granitic rocks. The Ladderlake soils are on flood-plain steps on glacial valley floors and basin floors of the Sierra Nevada Mountains. Slopes range from 0 to 4 percent. Mean annual precipitation is about 865 mm and the mean annual air temperature is about 1 degree C.", "TAXONOMIC CLASS": { @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil Temperature: The mean annual soil temperature at 50 centimeters is 0 to 6 degrees C, and the mean summer soil temperature is 0 to 6 degrees C. The soils have a cryic soil temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nHistic epipedon thickness: 20 to 40 cm\nAquic conditions: present within 25 cm of soil surface\nOrganic matter: 20 to 60 percent in the epipedon\nReaction: moderately to strongly acid\nDepth to redoximorphic features: 10 to 50 cm\nParticle size control section weighted average:\nRock fragments: 35 to 70 percent, with 15 to 50 percent gravel, 5 to 35 percent cobbles, 0 to 35 percent stones and 0 to 15 percent boulders.\nClay content: 1 to 6 percent\nNaF pH: 8.0 to 11.0\nOa horizon\nHue: 7.5YR, 10YR\nValue: 2 to 5 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: muck, peat\nRock fragments: 0 to 60 percent\n0 to 5 percent gravel\n0 to 20 percent cobbles\n0 to 30 percent stones\n0 to 5 percent boulders\nBw horizon\nHue: 10YR, 2.5Y\nValue: 5 or 6 dry, 3 or 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, sandy loam, fine sandy loam\nClay content: 2 to 10 percent\nRock fragments: 15 to 50 percent\n10 to 30 percent gravel\n10 to 30 percent cobbles\n5 to 20 percent stones\n0 to 5 percent boulders\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: few to common\nSize: fine, medium, and coarse\nAb horizon (where present)\nHue: 10YR, 2.5Y\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: sandy loam, fine sandy loam\nClay content: 2 to 6 percent\nRock fragments: 10 to 15 percent gravel\nl\nC horizon\nHue: 10YR, 2.5Y\nValue: 5 to 7 dry, 3 to 5 moist\nChroma: 1 or 2, dry or moist\nTexture: coarse sand, sand, loamy sand, loamy coarse sand, sandy loam\nClay content: 0 to 10 percent\nRock fragments: 35 to 70 percent\n30 to 50 percent gravel\n5 to 45 percent cobbles\n0 to 5 percent stones\n0 to 5 percent boulders\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: few to many\nSize: fine, medium, and coarse\nIron depletions in matrix\nQuantity: none to common\nSize: fine, medium, and coarse\nCg horizon\nHue: 10YR, 2.5Y, 5Y\nValue: 6 to 8 dry, 4 to 6 moist\nChroma: 1 or 2, dry or moist\nTexture: silt loam, sandy loam, loam, loamy fine sand\nClay content: 5 to 25 percent\nRock fragments: 20 to 60 percent\n15 to 40 percent gravel\n5 to 20 percent cobbles\n0 to 20 percent stones\n0 to 5 percent boulders\nRedoximorphic Features:\nReduced iron masses in matrix\nQuantity: many\nSize: medium to extremely coarse" + "content": "RANGE IN CHARACTERISTICS:\nSoil Temperature: The mean annual soil temperature at 50 centimeters is 0 to 6 degrees C, and the mean summer soil temperature is 0 to 6 degrees C. The soils have a cryic soil temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nHistic epipedon thickness: 20 to 40 cm\nAquic conditions: present within 25 cm of soil surface\nOrganic matter: 20 to 60 percent in the epipedon\nReaction: moderately to strongly acid\nDepth to redoximorphic features: 10 to 50 cm\nParticle size control section weighted average:\nRock fragments: 35 to 70 percent, with 15 to 50 percent gravel, 5 to 35 percent cobbles, 0 to 35 percent stones and 0 to 15 percent boulders.\nClay content: 1 to 6 percent\nNaF pH: 8.0 to 11.0\nOa horizon\nHue: 7.5YR, 10YR\nValue: 2 to 5 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: muck\nRock fragments: 0 to 60 percent\n0 to 5 percent gravel\n0 to 20 percent cobbles\n0 to 30 percent stones\n0 to 5 percent boulders\nBw horizon\nHue: 10YR, 2.5Y\nValue: 5 or 6 dry, 3 or 4 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, sandy loam, fine sandy loam\nClay content: 2 to 10 percent\nRock fragments: 15 to 50 percent\n10 to 30 percent gravel\n10 to 30 percent cobbles\n5 to 20 percent stones\n0 to 5 percent boulders\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: few to common\nSize: fine, medium, and coarse\nAb horizon (where present)\nHue: 10YR, 2.5Y\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: sandy loam, fine sandy loam\nClay content: 2 to 6 percent\nRock fragments: 10 to 15 percent gravel\nC horizon\nHue: 10YR, 2.5Y\nValue: 5 to 7 dry, 3 to 5 moist\nChroma: 1 or 2, dry or moist\nTexture: coarse sand, sand, loamy sand, loamy coarse sand, sandy loam\nClay content: 0 to 10 percent\nRock fragments: 35 to 70 percent\n30 to 50 percent gravel\n5 to 45 percent cobbles\n0 to 5 percent stones\n0 to 5 percent boulders\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: few to many\nSize: fine, medium, and coarse\nIron depletions in matrix\nQuantity: none to common\nSize: fine, medium, and coarse\nCg horizon\nHue: 10YR, 2.5Y, 5Y\nValue: 6 to 8 dry, 4 to 6 moist\nChroma: 1 or 2, dry or moist\nTexture: silt loam, sandy loam, loam, loamy fine sand\nClay content: 5 to 25 percent\nRock fragments: 20 to 60 percent\n15 to 40 percent gravel\n5 to 20 percent cobbles\n0 to 20 percent stones\n0 to 5 percent boulders\nRedoximorphic Features:\nReduced iron masses in matrix\nQuantity: many\nSize: medium to extremely coarse" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 46 to 121 cm\nDiagnostic horizons and features recognized in this pedon are:\nHistic Epipedon 0 to 21 cm\nSapric Soil Materials 0 to 21 cm\nRedox Concentrations 21 to 44 and 49 to 117 cm\nAquic Conditions 0 to 150 cm\nRedox Depletions with Chroma 2 Or Less 30 to 44 and 49 to 117 cm\nReduced Matrix 117 to 150 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2015CA7923081\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 46 to 121 cm\nDiagnostic horizons and features recognized in this pedon are:\nHistic Epipedon 0 to 21 cm\nRedox Concentrations 21 to 44 and 49 to 117 cm\nAquic Conditions 0 to 150 cm\nRedox Depletions with Chroma 2 Or Less 30 to 44 and 49 to 117 cm\nReduced Matrix 117 to 150 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2015CA7923081\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/L/LITTLEPETE.json b/inst/extdata/OSD/L/LITTLEPETE.json index 4304f27081..b0e9c528b6 100644 --- a/inst/extdata/OSD/L/LITTLEPETE.json +++ b/inst/extdata/OSD/L/LITTLEPETE.json @@ -1,10 +1,10 @@ { "SERIES": "LITTLEPETE", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "10/2019", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Littlepete series consists of very deep, poorly drained soils formed in alluvium derived from granitic rocks. Littlepete soils are on flood-plain steps of glacial-valley floors and basin floors of the Sierra Nevada Mountains. Slopes range from 1 to 4 percent. The mean annual precipitation is about 920 mm and the mean annual air temperature is about 3 degrees C.", + "OVERVIEW": "The Littlepete series consists of very deep, poorly drained soils formed in alluvium derived from granitic rocks. Littlepete soils are on floodplains of glacial-valley floors and basin floors of the Sierra Nevada Mountains. Slopes range from 1 to 4 percent. The mean annual precipitation is about 920 mm and the mean annual air temperature is about 3 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Sandy, isotic Aquandic Cryaquents" @@ -27,11 +27,11 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Littlepete soils are on flood-plain steps of glacial-valley bottoms and basin floors. Slopes range from 1 to 4 percent. These soils formed in alluvium. Elevation is 2500 to 3885 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 560 to 1385 mm and the mean annual air temperature is 0 to 5 degrees C. The frost free season is 50 to 95 days." + "content": "GEOGRAPHIC SETTING: The Littlepete soils are on floodplains of glacial-valley bottoms and basin floors. Slopes range from 1 to 4 percent. These soils formed in alluvium. Elevation is 2500 to 3885 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 560 to 1385 mm and the mean annual air temperature is 0 to 5 degrees C. The frost free season is 50 to 95 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", - "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Ladderlake soils. The Ladderlake soils are poorly to poorly drained soils on slightly higher floodplain steps; they have histic epipedons, and average greater than 35 percent rock fragments in the particle size control section." + "content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are the Ladderlake soils. The Ladderlake soils are poorly to poorly drained soils on flood-plain steps; they have histic epipedons, and average greater than 35 percent rock fragments in the particle size control section." }, "DRAINAGE AND PERMEABILITY": { "section": "DRAINAGE AND PERMEABILITY", diff --git a/inst/extdata/OSD/M/MARMOT.json b/inst/extdata/OSD/M/MARMOT.json index 86f3702f0d..79ce6227e1 100644 --- a/inst/extdata/OSD/M/MARMOT.json +++ b/inst/extdata/OSD/M/MARMOT.json @@ -1,25 +1,25 @@ { "SERIES": "MARMOT", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Marmot series consists of moderately deep, well drained soils formed in colluvium and till derived from metamorphic rock. The Marmot soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 865 mm and the mean annual air temperature is about 5 degrees C.", + "OVERVIEW": "The Marmot series consists of moderately deep, well drained soils formed in colluvium and till over residuum derived from metamorphic rock. The Marmot soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 865 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, frigid Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Marmot very cobbly fine sandy loam on a south-facing (176 degree), 50 percent slope under greenleaf manzanita at an elevation of 2577 meters. (Colors are for dry soils unless otherwise noted. When described on July 10, 2014 the soil was dry throughout.)\nOi--0 to 2 cm; very dark grayish brown (10YR 3/2) slightly decomposed plant material, very dark brown (7.5YR 2.5/2) moist; strongly acid (pH 5.2); abrupt smooth boundary. (0 to 5 cm thick)\nA--2 to 18 cm; very dark grayish brown (10YR 3/2) very cobbly fine sandy loam, very dark brown (7.5YR 2.5/2) moist; 10 percent clay; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; many very fine irregular pores; 10 percent subangular indurated metasedimentary channers, 10 percent subangular indurated metasedimentary gravel, 20 percent subangular indurated metasedimentary cobbles; NaF pH 9.0; strongly acid (pH 5.4); gradual smooth boundary. (5 to 25 cm thick)\nC1--18 to 76 cm; very dark grayish brown (10YR 3/2) extremely cobbly fine sandy loam, very dark brown (7.5YR 2.5/2) moist; 12 percent clay; soft, very friable, nonsticky, nonplastic; common very fine, fine, medium, and very coarse roots throughout; many very fine irregular pores; 20 percent subangular indurated metasedimentary channers, 20 percent subangular indurated metasedimentary gravel, 20 percent subangular indurated metasedimentary cobbles; NaF pH 10.5; moderately acid (pH 5.6); gradual smooth boundary.\nC2--76 to 95 cm; very dark grayish brown (10YR 3/2) extremely stony fine sandy loam, very dark brown (7.5YR 2.5/2) moist; 12 percent clay; soft, very friable, nonsticky, nonplastic; common fine and medium roots throughout; many very fine irregular pores; 10 percent subangular indurated metasedimentary channers, 10 percent subangular indurated metasedimentary cobbles, 60 percent subangular indurated metasedimentary stones; NaF pH 10.5; strongly acid (pH 5.4); very abrupt smooth boundary. (combined thickness of C horizons is 25 to 75 cm)\nR--95 to 200 cm; indurated metasedimentary bedrock, fractured at intervals of 10 to <45 cm." + "content": "TYPICAL PEDON: Marmot very gravelly sandy loam on a south-facing (175 degree), 45 percent slope under a canopy of Jeffrey pine and Sierra juniper at an elevation of 2368 meters. (Colors are for dry soils unless otherwise noted. When described on July 11, 2014 the soil was dry to 17 cm and moist to 65 cm.)\nOi--0 to 3 cm; yellowish brown (10YR 5/4) slightly decomposed plant material, dark yellowish brown (10YR 4/4) moist; about 100 percent fiber, 90 percent rubbed; moderately acid (pH 5.6); abrupt smooth boundary. (0 to 5 cm thick)\nA1--3 to 7 cm; very dark grayish brown (10YR 3/2) very gravelly sandy loam, black (10YR 2/1) moist; 65 percent sand; 8 percent clay; weak fine subangular blocky, and weak medium subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine and fine roots throughout; common very fine irregular pores; 5 percent subangular indurated schist channers, 20 percent subangular indurated schist gravel, 5 percent subangular indurated schist flagstones, 5 percent subangular indurated schist stones; NaF pH 8.0; moderately acid (pH 5.6); abrupt smooth boundary.\nA2--7 to 17 cm; dark grayish brown (10YR 4/2) very stony fine sandy loam, very dark brown (10YR 2/2) moist; 58 percent sand; 10 percent clay; weak very fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, and medium roots throughout, and common very fine, fine, and medium roots around fragments; common very fine and fine irregular pores; 20 percent subangular indurated schist gravel, 5 percent subangular indurated schist cobbles, 5 percent subangular indurated schist flagstones, 25 percent subangular indurated schist stones; NaF pH 8.5; moderately acid (pH 5.8); clear smooth boundary. (combined thickness of A horizons is 5 to 25 cm)\nBw--17 to 65 cm; brown (10YR 4/3) extremely cobbly fine sandy loam, very dark brown (10YR 2/2) moist; 55 percent sand; 12 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common very fine and fine irregular pores; 35 percent subangular indurated schist gravel, 35 percent subangular indurated schist cobbles, 2 percent subangular indurated schist stones; NaF pH 9.0; moderately acid (pH 5.8); very abrupt smooth boundary. (15 to 50 cm thick)\nR--65 to 200 cm; Indurated biotite schist bedrock, fractured at intervals of 45 to <100 cm; common fine, medium, and coarse roots top of horizon." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, Timber Gap Trail, about 0.5 km north of trailhead parking lot; USGS 7.5 minute topographic quadrangle: Mineral King, California; WGS84 36.457842 latitude and -118.595294 longitude; UTM zone 11 4035915 meters N 357050 meters E WGS84." + "content": "TYPE LOCATION: Tulare County, California, about 0.5 km ENE of the Mineral King ranger station; USGS 7.5 minute topographic quadrangle: Mineral King, California; WGS84 36.454661 latitude and -118.606933 longitude; UTM zone 11 4035578 meters N 356002 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 9 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 18 to 75 cm\nDepth to lithic contact: 50 to 100 cm\nOrganic matter: 1 to 5 percent\nReaction: strongly to moderately acid\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm or to a lithic contact\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 0 to 35 percent gravel, 0 to 35 percent cobbles, 0 to 60 percent stones, 0 to 35 percent channers, and 0 to 35 percent flagstones\nClay content: 3 to 12 percent\nNaF pH: 8.5 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 4 dry, 2 to 3 moist\nChroma: 1 or 2, dry or moist\nTexture: fine sandy loam, sandy loam, loamy fine sand\nClay content: 3 to 10 percent\nRock fragments: 35 to 75 percent\n0 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 15 percent stones\n0 to 35 percent channers\nBw horizon (where present)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 or 5 dry, 2 to 4 moist\nChroma: 2 to 6 dry, 2 to 4 moist\nTexture: fine sandy loam, sandy loam, loam\nClay content: 5 to 15 percent\nRock fragments: 35 to 75 percent\n0 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 60 percent stones\n0 to 35 percent channers\n0 to 35 percent flagstones\nC horizon(s)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 3 to 6 dry, 2 to 5 moist\nChroma: 2 to 4, dry or moist\nTexture: fine sandy loam, sandy loam, loamy fine sand\nClay content: 2 to 12 percent\nRock fragments: 15 to 80 percent\n0 to 60 percent gravel\n0 to 35 percent cobbles\n0 to 60 percent stones\n0 to 35 percent channers\n0 to 35 percent flagstones" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 9 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 18 to 75 cm\nDepth to lithic contact: 50 to 100 cm\nOrganic matter: 1 to 5 percent\nReaction: strongly to moderately acid\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm or to a lithic contact\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 0 to 35 percent gravel, 0 to 35 percent cobbles, 0 to 60 percent stones, 0 to 35 percent channers, and 0 to 35 percent flagstones\nClay content: 3 to 12 percent\nNaF pH: 8.5 to 11.0\nA horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 to 4 dry, 2 to 3 moist\nChroma: 1 or 2, dry or moist\nTexture: fine sandy loam, sandy loam, loamy fine sand\nClay content: 3 to 10 percent\nRock fragments: 35 to 75 percent\n0 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 25 percent stones\n0 to 35 percent channers\n0 to 10 percent flagstones\nBw horizon (where present)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 or 5 dry, 2 to 4 moist\nChroma: 2 to 6 dry, 2 to 4 moist\nTexture: fine sandy loam, sandy loam, loam\nClay content: 5 to 15 percent\nRock fragments: 35 to 75 percent\n0 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 60 percent stones\n0 to 35 percent channers\n0 to 35 percent flagstones\nC horizon (where present)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 3 to 6 dry, 2 to 5 moist\nChroma: 2 to 4, dry or moist\nTexture: fine sandy loam, sandy loam, loamy fine sand\nClay content: 2 to 12 percent\nRock fragments: 15 to 80 percent\n0 to 60 percent gravel\n0 to 35 percent cobbles\n0 to 60 percent stones\n0 to 35 percent channers\n0 to 35 percent flagstones" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -39,7 +39,7 @@ }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is greenleaf manzanita and scattered Sierra juniper." + "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is Sierra juniper, Jeffrey pine, greenleaf manzanita, mountain big sagebrush, oceanspray, and threadleaf sedge." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 27 to 95 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 2 to 76 cm\nLithic Contact 76 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7925056\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 27 to 65 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 3 to 65 cm\nLithic Contact 65 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7921025\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/M/MCDERMAND.json b/inst/extdata/OSD/M/MCDERMAND.json index 313b020f6c..84b4380107 100644 --- a/inst/extdata/OSD/M/MCDERMAND.json +++ b/inst/extdata/OSD/M/MCDERMAND.json @@ -1,25 +1,25 @@ { "SERIES": "MCDERMAND", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB/JTW", - "REVDATE": "12/2019", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The McDermand series consists of moderately deep, moderately well drained soils formed in slope alluvium, colluvium and till over residuum weathered from granite. The McDermand soils are on cirque floors of the Sierra Nevada Mountains. Slopes range from 2 to 15 percent. The mean annual precipitation is about 1075 mm and the mean annual air temperature is about 2 degrees C.", + "OVERVIEW": "The McDermand series consists of moderately deep, moderately well drained soils formed in slope alluvium, colluvium and till over residuum weathered from granite. The McDermand soils are in cirques and mountain slopes of the Sierra Nevada Mountains. Slopes range from 2 to 30 percent. The mean annual precipitation is about 1075 mm and the mean annual air temperature is about 2 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Sandy-skeletal, isotic Vitrandic Cryorthents" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: McDermand mucky fine sandy loam on a south-facing (200 degree), 10 percent slope under purple mountainheath and dwarf bilberry at an elevation of 3352 meters. (Colors are for dry soils unless otherwise noted. When described on July 24, 2012 the soil was moist throughout.)\nA1--0 to 5 cm; dark grayish brown (10YR 4/2) mucky fine sandy loam, very dark gray (10YR 3/1) moist; 65 percent sand; 26 percent silt; 9 percent clay; moderate very fine granular structure; soft, very friable, nonsticky, nonplastic; many very fine and few fine roots throughout; many very fine irregular pores; NaF pH 7.4; strongly acid (pH 5.2); clear wavy boundary. Lab sample # 13N02214\nA2--5 to 15 cm; grayish brown (10YR 5/2) loamy sand, very dark grayish brown (10YR 3/2) moist; 84 percent sand; 14 percent silt; 2 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; few very fine and many fine roots throughout; many very fine irregular pores; 15 percent fine yellowish brown (10YR 5/6) moist, masses of oxidized iron with clear boundaries in matrix; 7 percent subrounded indurated granite gravel, 5 percent subrounded indurated granite cobbles, 2 percent subrounded indurated granite stones; NaF pH 10.4; strongly acid (pH 5.2); clear wavy boundary. Lab sample # 13N02215\nA3--15 to 25 cm; grayish brown (10YR 5/2) gravelly coarse sand, dark grayish brown (10YR 4/2) moist; 90 percent sand; 9 percent silt; 1 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; few very fine and common fine roots throughout; many very fine irregular pores; 20 percent subangular indurated granite gravel, 8 percent subangular indurated granite cobbles, 5 percent subangular indurated granite stones; NaF pH 10.6; strongly acid (pH 5.5); clear smooth boundary. (combined thickness of A horizons is 5 to 30 cm) Lab sample # 13N02216\nBw1--25 to 34 cm; light yellowish brown (2.5Y 6/3) gravelly coarse sand, brown (10YR 5/3) moist; 90 percent sand; 8 percent silt; 2 percent clay; structureless massive; soft, very friable, nonsticky, nonplastic; few very fine and common fine roots throughout; many very fine irregular pores; 22 percent subangular indurated granite gravel, 8 percent subangular indurated granite cobbles; NaF pH 10.3; moderately acid (pH 5.6); gradual smooth boundary. Lab sample # 13N02217\nBw2--34 to 49 cm; light yellowish brown (2.5Y 6/3) very gravelly coarse sand, dark yellowish brown (10YR 4/4) moist; 89 percent sand; 10 percent silt; 0 percent clay; structureless massive; soft, very friable, nonsticky, nonplastic; few very fine and fine roots throughout; many very fine irregular pores; 15 percent medium strong brown (7.5YR 5/6) moist, masses of oxidized iron with diffuse boundaries in matrix; 33 percent subangular indurated granite gravel, 7 percent subangular indurated granite cobbles; NaF pH 10.2; strongly acid (pH 5.4); clear wavy boundary. Lab sample # 13N02218\n2Bw3--49 to 51 cm; very pale brown (10YR 7/3) very gravelly loamy sand, pale yellow (2.5Y 7/4) moist; 75 percent sand; 4 percent clay; structureless massive; soft, friable, nonsticky, nonplastic; few fine roots throughout; few very fine irregular pores; 15 percent medium strong brown (7.5YR 5/8) moist, masses of oxidized iron with clear boundaries in matrix; 40 percent subangular indurated granite gravel; abrupt broken boundary. (combined thickness of Bw horizons is 15 to 50 cm)\n3R--51 to 200 cm; Indurated granite bedrock, fractured at intervals of 45 to <100 cm." + "content": "TYPICAL PEDON: McDermand mucky fine sandy loam on a south-facing (200 degree), 10 percent slope under purple mountainheath and dwarf bilberry at an elevation of 3352 meters. (Colors are for dry soils unless otherwise noted. When described on July 24, 2012 the soil was moist throughout.)\nA1--0 to 5 cm; dark grayish brown (10YR 4/2) mucky fine sandy loam, very dark gray (10YR 3/1) moist; 65 percent sand; 26 percent silt; 9 percent clay; moderate very fine granular structure; soft, very friable, nonsticky, nonplastic; many very fine and few fine roots throughout; many very fine irregular pores; NaF pH 7.4; strongly acid (pH 5.2); clear wavy boundary. Lab sample # 13N02214\nA2--5 to 15 cm; grayish brown (10YR 5/2) loamy sand, very dark grayish brown (10YR 3/2) moist; 84 percent sand; 14 percent silt; 2 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; few very fine and many fine roots throughout; many very fine irregular pores; 15 percent fine yellowish brown (10YR 5/6) moist, masses of oxidized iron with clear boundaries in matrix; 7 percent subrounded indurated granite gravel, 5 percent subrounded indurated granite cobbles, 2 percent subrounded indurated granite stones; NaF pH 10.4; strongly acid (pH 5.2); clear wavy boundary. Lab sample # 13N02215\nA3--15 to 25 cm; grayish brown (10YR 5/2) gravelly coarse sand, dark grayish brown (10YR 4/2) moist; 90 percent sand; 9 percent silt; 1 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; few very fine and common fine roots throughout; many very fine irregular pores; 20 percent subangular indurated granite gravel, 8 percent subangular indurated granite cobbles, 5 percent subangular indurated granite stones; NaF pH 10.6; strongly acid (pH 5.5); clear smooth boundary. (combined thickness of A horizons is 5 to 30 cm) Lab sample # 13N02216\nC1--25 to 34 cm; light yellowish brown (2.5Y 6/3) gravelly coarse sand, brown (10YR 5/3) moist; 90 percent sand; 8 percent silt; 2 percent clay; structureless massive; soft, very friable, nonsticky, nonplastic; few very fine and common fine roots throughout; many very fine irregular pores; 22 percent subangular indurated granite gravel, 8 percent subangular indurated granite cobbles; NaF pH 10.3; moderately acid (pH 5.6); gradual smooth boundary. Lab sample # 13N02217\nC2--34 to 51 cm; light yellowish brown (2.5Y 6/3) very gravelly coarse sand, dark yellowish brown (10YR 4/4) moist; 89 percent sand; 10 percent silt; 0 percent clay; structureless massive; soft, very friable, nonsticky, nonplastic; few very fine and fine roots throughout; many very fine irregular pores; 15 percent medium strong brown (7.5YR 5/6) moist, masses of oxidized iron with diffuse boundaries in matrix; 33 percent subangular indurated granite gravel, 7 percent subangular indurated granite cobbles; NaF pH 10.2; strongly acid (pH 5.4); clear wavy boundary. Lab sample # 13N02218\n2R--51 to 200 cm; Indurated granite bedrock, fractured at intervals of 45 to <100 cm." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Fresno County, California, near Sapphire Lake in Evolution Valley in Kings Canyon National Park; USGS 7.5 minute topographic quadrangle: Mount Darwin, California; WGS84 37.152236 latitude and -118.693357 longitude; UTM zone 11 4113103 meters N 349627 meters E NAD83." + "content": "TYPE LOCATION: Fresno County, California, near Sapphire Lake in Evolution Valley in Kings Canyon National Park; USGS 7.5 minute topographic quadrangle: Mount Darwin, California; WGS84 37.152236 latitude and -118.693357 longitude; UTM zone 11 4113103 meters N 349627 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is -1 to 5 degrees C and the difference between mean summer and mean winter soil temperature is less than 6 degrees C. The soils have a cryic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about September to October (about 50 days). The soils contain a seasonal water table as high as 30 cm during the winter, spring and early summer months, falling to below 100 cm during late summer and fall.\nDiagnostic Feature(s):\nOchric epipedon thickness: 18 cm\nDepth to lithic contact: 50 to 100 cm\nDepth to redoximorphic features: 10 to 50 cm\nParticle size control section weighted average:\nRock fragments: 35 to 60 percent, with 15 to 50 percent gravel, 0 to 15 percent cobbles, and 0 to 5 percent stones.\nClay content: 1 to 8 percent\nNaF pH: 9.0 to 11.0\nA horizons\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 to 4 moist\nChroma: 2 or 3 dry, 1 or 2 moist\nTexture: fine sandy loam, sandy loam, loamy sand, coarse sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 35 percent\n0 to 20 percent gravel\n0 to 15 percent cobbles\n0 to 10 percent stones\nReaction: very strongly to strongly acid\nNaF pH: 7.0 to 11.0\nBw horizons\nHue: 10YR, 2.5Y\nValue: 6 or 7 dry, 4 or 5 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, coarse sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 35 percent\n15 to 50 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\nPararock fragments: 0 to 35 percent paragravel\nReaction: strongly to moderately acid\nNaF pH: 9.0 to 11.5\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix\nQuantity: none to common\nSize: fine, medium, and coarse" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is -1 to 5 degrees C and the difference between mean summer and mean winter soil temperature is less than 6 degrees C. The soils have a cryic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about September to October (about 50 days). The soils contain a seasonal water table as high as 30 cm during the winter, spring and early summer months, falling to below 100 cm during late summer and fall.\nDiagnostic Feature(s):\nOchric epipedon thickness: 18 cm\nDepth to lithic contact: 50 to 100 cm\nDepth to redoximorphic features: 10 to 50 cm\nParticle size control section weighted average:\nRock fragments: 35 to 60 percent, with 15 to 50 percent gravel, 0 to 15 percent cobbles, and 0 to 5 percent stones.\nClay content: 1 to 8 percent\nNaF pH: 9.0 to 11.0\nA horizons\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 to 4 moist\nChroma: 2 or 3 dry, 1 or 2 moist\nTexture: fine sandy loam, sandy loam, loamy sand, coarse sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 35 percent\n0 to 20 percent gravel\n0 to 15 percent cobbles\n0 to 10 percent stones\nReaction: very strongly to strongly acid\nNaF pH: 7.0 to 11.0\nC horizons\nHue: 10YR, 2.5Y\nValue: 6 or 7 dry, 4 or 5 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, coarse sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 35 percent\n15 to 50 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\nPararock fragments: 0 to 35 percent paragravel\nReaction: strongly to moderately acid\nNaF pH: 9.0 to 11.5\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix\nQuantity: none to common\nSize: fine, medium, and coarse" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -27,7 +27,7 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The McDermand soils are in swales on structural benches in cirques. Slopes range from 2 to 15 percent. These soils formed in slope alluvium, colluvium, and till over residuum weathered from granite. Elevation is 2540 to 4140 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 620 to 1505 mm and the mean annual air temperature is -2 to 4 degrees C. The frost free season is 40 to 90 days." + "content": "GEOGRAPHIC SETTING: The McDermand soils are in swales on structural benches in cirques and on mountain slopes. Slopes range from 2 to 30 percent. These soils formed in slope alluvium, colluvium, and till over residuum weathered from granite. Elevation is 2540 to 4140 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 620 to 1505 mm and the mean annual air temperature is -2 to 4 degrees C. The frost free season is 40 to 90 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 25 to 51 cm.\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 0 to 25 cm\nRedox Concentrations 5 to 15 cm and 34 to 51 cm\nLithic Contact 51 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nPedon Type: representative pedon for component Lab Source ID: SSL\nPedon Purpose: laboratory sampling site Lab Pedon #: 13N0502\nNASIS User Pedon ID: S2012CA019003\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 25 to 51 cm.\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 0 to 18 cm\nRedox Concentrations 5 to 15 cm and 34 to 51 cm\nLithic Contact 51 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nPedon Type: representative pedon for component Lab Source ID: SSL\nPedon Purpose: laboratory sampling site Lab Pedon #: 13N0502\nNASIS User Pedon ID: S2012CA019003\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/M/MINERALKING.json b/inst/extdata/OSD/M/MINERALKING.json index 729bc32ce9..744b9ac7fe 100644 --- a/inst/extdata/OSD/M/MINERALKING.json +++ b/inst/extdata/OSD/M/MINERALKING.json @@ -1,17 +1,17 @@ { "SERIES": "MINERALKING", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Mineralking series consists of very deep, well drained soils formed in colluvium from metasedimentary rocks. The Mineralking soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 865 mm and the mean annual air temperature is about 5 degrees C.", + "OVERVIEW": "The Mineralking series consists of very deep, well drained soils formed in colluvium from granitic and metamorphic rocks. The Mineralking soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 15 to 75 percent. The mean annual precipitation is about 865 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, frigid Vitrandic Humixerepts" + "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, frigid Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Mineralking gravelly fine sandy loam on a west facing (248 degree), 62 percent slope under red fir at an elevation of 2610 meters. (Colors are for dry soils unless otherwise noted. When described on July 10, 2014 the soil was moist throughout.)\nOi--0 to 3 cm; brown (7.5YR 4/2) slightly decomposed plant material, very dark brown (7.5YR 2.5/3) moist; slightly acid (pH 6.4); abrupt smooth boundary. (3 to 8 cm thick) Lab sample # 15N02521\nA--3 to 15 cm; brown (10YR 4/3) gravelly fine sandy loam, dark brown (7.5YR 3/2) moist; 46 percent sand; 49 percent silt; 6 percent clay; weak very fine subangular blocky parts to weak very fine granular structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, and medium roots throughout; common very fine and fine dendritic tubular, and common medium irregular pores; 20 percent subangular strongly cemented schist gravel, 5 percent subangular strongly cemented schist cobbles, 2 percent subangular strongly cemented schist stones; NaF pH 10.1; moderately acid (pH 6.0); clear smooth boundary. (5 to 25 cm thick) Lab sample # 15N02522\nBA--15 to 27 cm; grayish brown (10YR 5/2) gravelly silt loam, very dark grayish brown (10YR 3/2) moist; 45 percent sand; 50 percent silt; 5 percent clay; moderate medium subangular blocky structure; slightly hard, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common very fine and fine dendritic tubular, and common fine and medium irregular pores; 20 percent subangular strongly cemented schist gravel, 5 percent subangular strongly cemented schist cobbles, 2 percent subangular strongly cemented schist stones; NaF pH 10.1; slightly acid (pH 6.4); clear wavy boundary. (0 to 15 cm thick) Lab sample # 15N02523\nBw--27 to 61 cm; light yellowish brown (10YR 6/4) gravelly silt loam, dark yellowish brown (10YR 4/4) moist; 44 percent sand; 51 percent silt; 5 percent clay; moderate medium subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, coarse, and very coarse roots throughout; common very fine and fine dendritic tubular, and common fine and medium irregular pores; 40 percent subangular strongly cemented schist gravel, 5 percent subangular strongly cemented schist cobbles, 2 percent subangular strongly cemented schist stones; NaF pH 9.9; slightly acid (pH 6.4); clear smooth boundary. (15 to 100 cm thick) Lab sample # 15N02524\nBC--61 to 98 cm; light yellowish brown (10YR 6/4) very gravelly coarse sandy loam, dark yellowish brown (10YR 4/4) moist; 50 percent sand; 46 percent silt; 5 percent clay; weak fine subangular blocky structure; soft, very friable, moderately sticky, slightly plastic; many very fine and fine, and common medium, coarse, and very coarse roots throughout; common very fine and fine irregular pores; 30 percent subrounded strongly cemented schist gravel, 10 percent subrounded strongly cemented schist cobbles, 3 percent subrounded strongly cemented schist stones; NaF pH 10.1; slightly acid (pH 6.1); clear smooth boundary. (0 to 60 cm thick) Lab sample # 15N02525\nCB--98 to 123 cm; very pale brown (10YR 7/4) gravelly sandy loam, dark yellowish brown (10YR 4/4) moist; 50 percent sand; 46 percent silt; 4 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common fine irregular pores; 30 percent subrounded strongly cemented schist gravel, 10 percent subrounded strongly cemented schist cobbles, 3 percent subrounded strongly cemented schist stones; NaF pH 10.0; moderately acid (pH 5.9); clear smooth boundary. (0 to 40 cm thick) Lab sample # 15N02526\nC--123 to 160 cm; pale yellow (2.5Y 8/3) very gravelly sandy loam, light yellowish brown (2.5Y 6/4) moist; 48 percent sand; 48 percent silt; 4 percent clay; structureless massive; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common fine irregular pores; 40 percent subrounded strongly cemented schist gravel, 5 percent subrounded strongly cemented schist cobbles, 5 percent subrounded strongly cemented schist stones; NaF pH 10.0; moderately acid (pH 6.0). Lab sample # 15N02527" + "content": "TYPICAL PEDON: Mineralking gravelly fine sandy loam on a west facing (248 degree), 62 percent slope under red fir at an elevation of 2610 meters. (Colors are for dry soils unless otherwise noted. When described on July 10, 2014 the soil was moist throughout.)\nOi--0 to 3 cm; brown (7.5YR 4/2) slightly decomposed plant material, very dark brown (7.5YR 2.5/3) moist; slightly acid (pH 6.4); abrupt smooth boundary. (3 to 8 cm thick) Lab sample # 15N02521\nA--3 to 15 cm; brown (10YR 4/3) gravelly fine sandy loam, dark brown (7.5YR 3/2) moist; 46 percent sand; 49 percent silt; 6 percent clay; weak very fine subangular blocky parts to weak very fine granular structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, and medium roots throughout; common very fine and fine dendritic tubular, and common medium irregular pores; 20 percent subangular strongly cemented schist gravel, 5 percent subangular strongly cemented schist cobbles, 2 percent subangular strongly cemented schist stones; NaF pH 10.1; moderately acid (pH 6.0); clear smooth boundary. (5 to 25 cm thick) Lab sample # 15N02522\nBA--15 to 27 cm; grayish brown (10YR 5/2) very gravelly silt loam, very dark grayish brown (10YR 3/2) moist; 45 percent sand; 50 percent silt; 5 percent clay; moderate medium subangular blocky structure; slightly hard, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common very fine and fine dendritic tubular, and common fine and medium irregular pores; 20 percent subangular strongly cemented schist gravel, 5 percent subangular strongly cemented schist cobbles, 2 percent subangular strongly cemented schist stones; NaF pH 10.1; slightly acid (pH 6.4); clear wavy boundary. (0 to 15 cm thick) Lab sample # 15N02523\nBw--27 to 61 cm; light yellowish brown (10YR 6/4) gravelly silt loam, dark yellowish brown (10YR 4/4) moist; 44 percent sand; 51 percent silt; 5 percent clay; moderate medium subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, coarse, and very coarse roots throughout; common very fine and fine dendritic tubular, and common fine and medium irregular pores; 40 percent subangular strongly cemented schist gravel, 5 percent subangular strongly cemented schist cobbles, 2 percent subangular strongly cemented schist stones; NaF pH 9.9; slightly acid (pH 6.4); clear smooth boundary. (15 to 100 cm thick) Lab sample # 15N02524\nBC--61 to 98 cm; light yellowish brown (10YR 6/4) very gravelly coarse sandy loam, dark yellowish brown (10YR 4/4) moist; 50 percent sand; 46 percent silt; 5 percent clay; weak fine subangular blocky structure; soft, very friable, moderately sticky, slightly plastic; many very fine and fine, and common medium, coarse, and very coarse roots throughout; common very fine and fine irregular pores; 30 percent subrounded strongly cemented schist gravel, 10 percent subrounded strongly cemented schist cobbles, 3 percent subrounded strongly cemented schist stones; NaF pH 10.1; slightly acid (pH 6.1); clear smooth boundary. (0 to 60 cm thick) Lab sample # 15N02525\nCB--98 to 123 cm; very pale brown (10YR 7/4) very gravelly sandy loam, dark yellowish brown (10YR 4/4) moist; 50 percent sand; 46 percent silt; 4 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common fine irregular pores; 30 percent subrounded strongly cemented schist gravel, 10 percent subrounded strongly cemented schist cobbles, 3 percent subrounded strongly cemented schist stones; NaF pH 10.0; moderately acid (pH 5.9); clear smooth boundary. (0 to 40 cm thick) Lab sample # 15N02526\nC--123 to 160 cm; pale yellow (2.5Y 8/3) very gravelly sandy loam, light yellowish brown (2.5Y 6/4) moist; 48 percent sand; 48 percent silt; 4 percent clay; structureless massive; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common fine irregular pores; 40 percent subrounded strongly cemented schist gravel, 5 percent subrounded strongly cemented schist cobbles, 5 percent subrounded strongly cemented schist stones; NaF pH 10.0; moderately acid (pH 6.0). Lab sample # 15N02527" }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -27,7 +27,7 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Mineralking soils are on linear backslopes of mountain slopes. Slopes range from 15 to 75 percent. These soils formed in colluvium from metasedimentary rocks. Elevation is 1955 to 2980 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 740 to 1090 mm and the mean annual air temperature is 3 to 9 degrees C. The frost free season is 80 to 150 days." + "content": "GEOGRAPHIC SETTING: The Mineralking soils are on linear backslopes of mountain slopes. Slopes range from 15 to 75 percent. These soils formed in colluvium from granitic and metamorphic rocks. Elevation is 1955 to 2980 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 740 to 1090 mm and the mean annual air temperature is 3 to 9 degrees C. The frost free season is 80 to 150 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", diff --git a/inst/extdata/OSD/P/PIGCHUTE.json b/inst/extdata/OSD/P/PIGCHUTE.json index c9956a17c5..ef4d167645 100644 --- a/inst/extdata/OSD/P/PIGCHUTE.json +++ b/inst/extdata/OSD/P/PIGCHUTE.json @@ -1,25 +1,25 @@ { "SERIES": "PIGCHUTE", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Pigchute series consists of very deep, well drained soils formed in colluvium, residuum, and till derived from granitic and metamorphic rocks. The Pigchute soils are on mountain slopes and lateral moraines of the Sierra Nevada Mountains. Slopes range from 25 to 60 percent. The mean annual precipitation is about 865 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, frigid Vitrandic Dystroxerepts" + "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, frigid Vitrandic Dystroxerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Pigchute very stony fine sandy loam on a south facing (168 degree), 35 percent slope under a canopy of red fir at an elevation of 2863 meters. (Colors are for dry soils unless otherwise noted. When described on July 10, 2014 the soil was moist throughout.)\nOi--0 to 6 cm; very dark brown (7.5YR 2.5/2) slightly decomposed plant material, very dark brown (7.5YR 2.5/2) moist; 5 percent subangular indurated metamorphic gravel, 5 percent subangular indurated metamorphic cobbles, 1 percent subangular indurated metamorphic stones; moderately acid (pH 5.8); abrupt smooth boundary. (0 to 10 cm thick)\nA--6 to 15 cm; dark grayish brown (10YR 4/2) very stony fine sandy loam, very dark brown (7.5YR 2.5/2) moist; 12 percent clay; weak very fine granular structure; soft, very friable, nonsticky, nonplastic; common very fine, fine, and medium roots throughout; common very fine interstitial pores; 10 percent subangular indurated metamorphic gravel, 15 percent subangular indurated metamorphic cobbles, 10 percent subangular indurated metamorphic stones; NaF pH 9.0; very strongly acid (pH 5.0); abrupt smooth boundary. (3 to 15 cm thick)\nBw1--15 to 30 cm; yellowish brown (10YR 5/4) very cobbly loam, dark yellowish brown (10YR 4/4) moist; 14 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common very fine interstitial pores; 30 percent subangular indurated metamorphic gravel, 30 percent subangular indurated metamorphic cobbles, 5 percent subangular indurated metamorphic stones; NaF pH 9.5; strongly acid (pH 5.2); clear smooth boundary.\nBw2--30 to 53 cm; light yellowish brown (10YR 6/4) extremely cobbly sandy loam, brown (10YR 4/3) moist; 15 percent clay; weak medium subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, coarse, and very coarse roots throughout; common very fine interstitial pores; 35 percent subangular indurated metamorphic gravel, 30 percent subangular indurated metamorphic cobbles, 1 percent subangular indurated metamorphic stones; NaF pH 9.5; very strongly acid (pH 5.0); clear smooth boundary.\nBw3--53 to 87 cm; very pale brown (10YR 7/4) extremely cobbly sandy loam, yellowish brown (10YR 5/4) moist; 13 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine, fine, medium, and coarse roots throughout; common very fine interstitial pores; 35 percent subangular indurated metamorphic gravel, 30 percent subangular indurated metamorphic cobbles, 1 percent subangular indurated metamorphic stones; NaF pH 9.5; very strongly acid (pH 5.0); clear smooth boundary. (combined thickness of Bw horizons is 25 to 100 cm)\nC--87 to 150 cm; pale yellow (2.5Y 7/3) very gravelly fine sandy loam, light yellowish brown (10YR 6/4) moist; 12 percent clay; structureless massive; soft, very friable, slightly sticky, nonplastic; common fine roots throughout; common very fine interstitial pores; 35 percent subangular indurated metamorphic gravel, 25 percent subangular indurated metamorphic cobbles, 1 percent subangular indurated metamorphic stones; NaF pH 9.0; very strongly acid (pH 5.0); clear smooth boundary." + "content": "TYPICAL PEDON: Pigchute very gravelly sandy loam on an east facing (107 degree), 36 percent slope under a canopy of red fir and white fir at an elevation of 2393 meters. (Colors are for dry soils unless otherwise noted. When described on August 24, 2017 the soil was dry to 59 cm and slightly moist to 163 cm.)\nOi--0 to 3 cm; slightly decomposed plant material; moderately acid (pH 6.0); abrupt smooth boundary. (0 to 10 cm thick)\nOe--3 to 8 cm; moderately decomposed plant material; common very fine roots throughout; many very fine irregular pores; NaF pH 8.0; moderately acid (pH 5.8); abrupt wavy boundary. (0 to 6 cm thick)\nA--8 to 20 cm; light olive brown (2.5Y 5/3) very gravelly sandy loam, very dark grayish brown (2.5Y 3/2) moist; 12 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; many very fine and fine, and common medium roots throughout; many very fine irregular pores; 35 percent subangular indurated metasedimentary gravel, 20 percent subangular indurated metasedimentary cobbles; NaF pH 10.0; moderately acid (pH 5.6); abrupt smooth boundary. (3 to 15 cm thick)\nBw1--20 to 59 cm; light yellowish brown (2.5Y 6/4) very gravelly sandy loam, dark yellowish brown (10YR 4/4) moist; 14 percent clay; weak fine and medium subangular blocky structure; soft, very friable, slightly sticky, nonplastic; many very fine, and common fine and medium roots throughout; many very fine irregular and few fine tubular pores; 35 percent subangular indurated metasedimentary gravel, 20 percent subangular indurated metasedimentary cobbles; NaF pH 10.0; strongly acid (pH 5.4); clear smooth boundary.\nBw2--59 to 118 cm; 20 percent olive yellow (2.5Y 6/6) and 80 percent pale yellow (2.5Y 7/4) very gravelly very fine sandy loam, light olive brown (2.5Y 5/4) moist; 16 percent clay; weak fine and medium subangular blocky structure; slightly hard, friable, slightly sticky, slightly plastic; few fine, and common medium and very coarse roots throughout; many very fine irregular and few fine tubular pores; 30 percent subangular indurated metasedimentary gravel, 15 percent subangular indurated metasedimentary cobbles; NaF pH 9.0; strongly acid (pH 5.2).\nBw3--118 to 163 cm; 50 percent pale yellow (2.5Y 7/4) and 50 percent olive yellow (2.5Y 6/6) very fine sandy loam, light olive brown (2.5Y 5/4) moist; 17 percent clay; weak fine subangular blocky structure; slightly hard, friable, slightly sticky, slightly plastic; common very fine irregular pores; 15 percent subangular indurated metasedimentary gravel; NaF pH 8.0; strongly acid (pH 5.2)." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, about 300 m southeast of Timber Gap, Sequoia National Park; USGS 7.5 minute topographic quadrangle: Mineral King, California; WGS84 36.466469 latitude and -118.597247 longitude; UTM zone 11 4036875 meters N 356891 meters E NAD83." + "content": "TYPE LOCATION: Tulare County, California, near the Big Baldy Trail, Kings Canyon National Park; USGS 7.5 minute topographic quadrangle: General Grant Grove, California; WGS84 36.692794 latitude and -118.880102 longitude; UTM zone 11 4062441 meters N 332037 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 3 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 100 days).\nDiagnostic Feature(s):\nOchric epipedon thickness: 18 cm\nCambic horizon thickness: 25 to 100 cm\nReaction: very strongly to moderately acid\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm.\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 25 to 40 percent gravel, 10 to 30 percent cobbles, and 0 to 50 percent stones\nClay content: 5 to 18 percent\nNaF pH: 8.5 to 11.0\nA horizon (s)\nHue: 7.5YR, 10YR\nValue: 4 to 6 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 to 3 moist\nTexture: sandy loam, fine sandy loam, loam\nClay content: 4 to 12 percent\nRock fragments: 0 to 65 percent\n0 to 40 percent gravel\n0 to 35 percent cobbles\n0 to 30 percent stones\nBw horizon (s)\nHue: 10YR\nValue: 5 to 7 dry, 3 or 5 moist\nChroma: 4 or 6 dry, 2 to 4 moist\nTexture: sandy loam, fine sandy loam, silt loam, loam\nClay content: 5 to 18 percent\nRock fragments: 35 to 75 percent\n25 to 40 percent gravel\n10 to 30 percent cobbles\n0 to 40 percent stones\nC horizon (where present)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 8 dry, 2 to 6 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, sandy loam, fine sandy loam\nClay content: 2 to 12 percent\nRock fragments: 35 to 75 percent\n25 to 65 percent gravel\n10 to 40 percent cobbles\n0 to 30 percent stones" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 3 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nOchric epipedon thickness: 18 cm\nCambic horizon thickness: 25 to 100 cm\nReaction: very strongly to moderately acid\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 100 cm.\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 25 to 40 percent gravel, 10 to 30 percent cobbles, and 0 to 50 percent stones\nClay content: 5 to 18 percent\nNaF pH: 8.0 to 11.0\nA horizon(s)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 6 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 to 3 moist\nTexture: sandy loam, fine sandy loam, loam\nClay content: 4 to 12 percent\nRock fragments: 0 to 65 percent\n0 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\nBw horizon(s)\nHue: 10YR, 2.5Y\nValue: 5 to 7 dry, 3 to 5 moist\nChroma: 4 or 6 dry, 2 to 4 moist\nTexture: sandy loam, fine sandy loam, very fine sandy loam, silt loam, loam\nClay content: 5 to 18 percent\nRock fragments: 35 to 75 percent\n15 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\nC horizon (where present)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 8 dry, 2 to 6 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, sandy loam, fine sandy loam\nClay content: 2 to 12 percent\nRock fragments: 35 to 80 percent\n15 to 60 percent gravel\n0 to 35 percent cobbles\n0 to 15percent stones" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 31 to 106 cm.\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 0 to 18 cm\nCambic Horizon 15 to 87cm\nADDITIONAL DATA:\nPedon information for this type location only:\nNASIS User Pedon ID: 2014CA7925055\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 33 to 108 cm.\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 0 to 18 cm\nCambic Horizon 20 to 163cm\nADDITIONAL DATA:\nPedon information for this type location only:\nNASIS User Pedon ID: 2017CA7926003\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/P/PINERIDGE.json b/inst/extdata/OSD/P/PINERIDGE.json index d909c59da4..ccb877f768 100644 --- a/inst/extdata/OSD/P/PINERIDGE.json +++ b/inst/extdata/OSD/P/PINERIDGE.json @@ -1,13 +1,13 @@ { "SERIES": "PINERIDGE", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Pineridge series consists of very deep, somewhat poorly or poorly drained soils formed in alluvium derived from granitic rocks. The Pineridge soils are on flood-plain steps on glacial valley floors, mountains, and plateaus of the Sierra Nevada Mountains. Slopes range from 1 to 10 percent. The mean annual precipitation is about 1000 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Sandy, isotic, frigid Hydraquentic Humaquepts" + "content": "TAXONOMIC CLASS: Sandy, isotic, frigid Hydraquentic Humaquepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nUmbric epipedon thickness: 30 to 100 cm\nAquic conditions: present within 25 cm of the mineral soil surface\nReaction: slightly to strongly acid\nOrganic matter: 2 to 10 percent in the epipedon\nDepth to redoximorphic features: 25 to 50 cm\nBase saturation: less than 50 percent (by ammonium acetate)\nParticle size control section weighted average:\nRock fragments: 0 to 15 percent, with 0 to 15 percent gravel and 0 to 5 percent cobbles\nClay content: 2 to 10 percent\nNaF pH: 8.5 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 1 to 3, dry or moist\nTexture: loamy sand, coarse sandy loam, sandy loam, fine sandy loam\nClay content: 2 to 12 percent\nRock fragments: 0 to 15 percent\n0 to 5 percent gravel\n0 to 5 percent cobbles\n0 to 10 percent channers\nBw1 horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 or 5 dry, 3 moist\nChroma: 1 to 3, dry or moist\nTexture: loamy coarse sand, loamy sand, coarse sandy loam, sandy loam\nClay content: 2 to 12 percent\nRock fragments: 0 to 15 percent\n0 to 5 percent gravel\n0 to 5 percent cobbles\n0 to 5 percent stones\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: few to common\nSize: very fine and fine\nBw2 horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 5 to 7 dry, 2 to 5 moist\nChroma: 2 to 4 dry, 1 to 3 moist\nTexture: loamy coarse sand, loamy sand, coarse sandy loam, sandy loam\nClay content: 2 to 8 percent\nRock fragments: 0 to 15 percent\n0 to 5 percent gravel\n0 to 5 percent cobbles\n0 to 5 percent stones\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: common to many\nSize: fine, medium, and coarse\nC horizons\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 7 dry, 2 to 5 moist\nChroma: 1 to 3, dry or moist\nTexture: coarse sand, sand, loamy coarse sand, loamy sand, sandy loam\nClay content: 1 to 7 percent\nRock fragments: 0 to 60 percent\n0 to 60 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 60 percent channers\n0 to 60 percent flagstones\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: common to many\nSize: medium and coarse" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nUmbric epipedon thickness: 30 to 100 cm\nAquic conditions: present within 25 cm of the mineral soil surface\nReaction: slightly to strongly acid\nOrganic matter: 2 to 10 percent in the epipedon\nDepth to redoximorphic features: 20 to 50 cm\nBase saturation: less than 50 percent (by ammonium acetate)\nParticle size control section weighted average:\nRock fragments: 0 to 15 percent, with 0 to 15 percent gravel and 0 to 5 percent cobbles\nClay content: 2 to 10 percent\nNaF pH: 8.5 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 1 to 3, dry or moist\nTexture: loamy sand, coarse sandy loam, sandy loam, fine sandy loam\nClay content: 2 to 12 percent\nRock fragments: 0 to 15 percent\n0 to 5 percent gravel\n0 to 5 percent cobbles\n0 to 10 percent channers\nBw1 horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 or 5 dry, 3 moist\nChroma: 1 to 3, dry or moist\nTexture: loamy coarse sand, loamy sand, coarse sandy loam, sandy loam\nClay content: 2 to 12 percent\nRock fragments: 0 to 15 percent\n0 to 5 percent gravel\n0 to 5 percent cobbles\n0 to 5 percent stones\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: few to common\nSize: very fine and fine\nBw2 horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 5 to 7 dry, 2 to 5 moist\nChroma: 2 to 4 dry, 1 to 3 moist\nTexture: loamy coarse sand, loamy sand, coarse sandy loam, sandy loam\nClay content: 2 to 8 percent\nRock fragments: 0 to 15 percent\n0 to 5 percent gravel\n0 to 5 percent cobbles\n0 to 5 percent stones\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: common to many\nSize: fine, medium, and coarse\nC horizons\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 7 dry, 2 to 5 moist\nChroma: 1 to 3, dry or moist\nTexture: coarse sand, sand, loamy coarse sand, loamy sand, sandy loam\nClay content: 1 to 7 percent\nRock fragments: 0 to 60 percent\n0 to 60 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\n0 to 60 percent channers\n0 to 60 percent flagstones\nRedoximorphic Features:\nOxidized iron and iron-manganese masses in matrix and along linings of pores\nQuantity: common to many\nSize: medium and coarse" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/R/RHODE_RIVER.json b/inst/extdata/OSD/R/RHODE_RIVER.json index 9a2bf05c12..8a9ebbed3a 100644 --- a/inst/extdata/OSD/R/RHODE_RIVER.json +++ b/inst/extdata/OSD/R/RHODE_RIVER.json @@ -2,7 +2,7 @@ "SERIES": "RHODE RIVER", "STATUS": "Established Series", "BYREV": "BMW/DCS/RBT", - "REVDATE": "04/2021", + "REVDATE": "06/2021", "STATES": "MD", "OVERVIEW": "MLRA(s): 149A\nSoil Survey Regional Office (SSRO) Responsible: Raleigh, North Carolina\nDepth Class: Very deep\nDrainage Class: Subaqueous (permanently submersed / continuously inundated)\nSaturated Hydraulic Conductivity: Moderately high to high\nParent Material: coarse-loamy estuarine deposits over glauconitic coarse-loamy fluviomarine deposits\nSlope: 0 to 3 percent\nMean Annual Air Temperature: 57 degrees F. (14 degrees C)\nMean Annual Water Temperature: 57 degrees F. (14 degrees C)", "TAXONOMIC CLASS": { diff --git a/inst/extdata/OSD/T/THARPSLOG.json b/inst/extdata/OSD/T/THARPSLOG.json index 63ec967c46..b3a89c52d8 100644 --- a/inst/extdata/OSD/T/THARPSLOG.json +++ b/inst/extdata/OSD/T/THARPSLOG.json @@ -1,13 +1,13 @@ { "SERIES": "THARPSLOG", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Tharpslog series consists of very deep, somewhat excessively drained soils formed in colluvium over residuum derived from granite. The Tharpslog soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 10 to 50 percent. The mean annual precipitation is about 1050 mm and the mean annual air temperature is about 8 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Sandy, isotic, mesic Vitrandic Humixerepts" + "content": "TAXONOMIC CLASS: Sandy, isotic, mesic Vitrandic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 6 to 12 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 18 to 85 cm\nOrganic matter: 1 to 8 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 75 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 35 percent gravel, predominantly 2 to 20 mm, and 0 to 15 percent cobbles.\nClay content: 2 to 10 percent\nNaF pH: 9.0 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, coarse sandy loam, loamy sand, loamy coarse sand\nClay content: 3 to 12 percent\nRock fragments: 0 to 35 percent gravel\nReaction: moderately acid to neutral\nAB horizon (where present)\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, coarse sandy loam, loamy sand, loamy coarse sand\nClay content: 3 to 12 percent\nRock fragments: 0 to 35 percent gravel\nReaction: moderately acid to neutral\nBw horizon(s)\nHue: 7.5YR, 10YR\nValue: 4 to 6 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: loamy sand, loamy coarse sand\nClay content: 1 to 10 percent\nRock fragments: 0 to 35 percent\n0 to 35 percent gravel\n0 to 15 percent cobbles\nReaction: strongly to slightly acid\nC horizon(s)\nHue: 10YR, 2.5Y\nValue: 5 to 7 dry, 4 or 5 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy coarse sand, sand, coarse sand\nClay content: 1 to 10 percent\nRock fragments: 0 to 35 percent\n0 to 35 percent gravel\n0 to 15 percent cobbles\nReaction: strongly to slightly acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 6 to 12 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 18 to 75 cm\nOrganic matter: 1 to 8 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 75 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 35 percent gravel, predominantly 2 to 20 mm, and 0 to 15 percent cobbles.\nClay content: 2 to 10 percent\nNaF pH: 9.0 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, coarse sandy loam, loamy sand, loamy coarse sand\nClay content: 3 to 12 percent\nRock fragments: 0 to 35 percent gravel\nReaction: moderately acid to neutral\nAB horizon (where present)\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sandy loam, coarse sandy loam, loamy sand, loamy coarse sand\nClay content: 3 to 12 percent\nRock fragments: 0 to 35 percent gravel\nReaction: moderately acid to neutral\nBw horizon(s)\nHue: 7.5YR, 10YR\nValue: 4 to 6 dry, 3 or 4 moist\nChroma: 3 or 4, dry or moist\nTexture: loamy sand, loamy coarse sand\nClay content: 1 to 10 percent\nRock fragments: 0 to 35 percent\n0 to 35 percent gravel\n0 to 15 percent cobbles\nReaction: strongly to slightly acid\nC horizon(s)\nHue: 10YR, 2.5Y\nValue: 5 to 7 dry, 4 or 5 moist\nChroma: 2 to 4, dry or moist\nTexture: loamy sand, loamy coarse sand, sand, coarse sand\nClay content: 1 to 10 percent\nRock fragments: 0 to 35 percent\n0 to 35 percent gravel\n0 to 15 percent cobbles\nReaction: strongly to slightly acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/T/TIGERLILY.json b/inst/extdata/OSD/T/TIGERLILY.json index 6625fc674f..438bc7e267 100644 --- a/inst/extdata/OSD/T/TIGERLILY.json +++ b/inst/extdata/OSD/T/TIGERLILY.json @@ -1,25 +1,25 @@ { "SERIES": "TIGERLILY", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Tigerlily series consists of very deep, very poorly drained soils formed in organic material over alluvium derived from granitic and metasedimentary rocks. The Tigerlily soils are in drainageways and on discharge slopes of the Sierra Nevada Mountains. Slopes range from 2 to 50 percent. The mean annual precipitation is about 1000 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, nonacid, frigid Hydraquentic Humaquepts" + "content": "TAXONOMIC CLASS: Loamy-skeletal, isotic, nonacid, frigid Hydraquentic Humaquepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Tigerlily muck on a south facing (180 degree), 50 percent slope with a cover of tiger lily, horsetail, corn lily, bigleaf lupine, and sedges at an elevation of 2355 meters. (Colors are for dry soils unless otherwise noted. When described on July 11, 2014 the soil was wet throughout. Seasonal water table was observed at 40 cm.)\nOa--0 to 13 cm; black (7.5YR 2.5/1) mucky peat, very dark gray (7.5YR 3/1) moist; structureless massive; hard, very friable, nonsticky, nonplastic; common very fine roots and fine roots throughout; many very fine irregular pores; neutral (pH 6.8); clear smooth boundary. (0 to 25 cm thick)\nOe--13 to 42 cm; black (7.5YR 2.5/1) stony mucky peat, very dark gray (7.5YR 3/1) moist; structureless massive; hard, very friable, nonsticky, nonplastic; common very fine, fine, and medium roots throughout; many very fine irregular pores; 5 percent rounded indurated mixed gravel, 10 percent subrounded indurated mixed stones; slightly acid (pH 6.3); abrupt smooth boundary. (0 to 35 cm thick)\nC1--42 to 85 cm; very dark grayish brown (10YR 3/2) very stony loamy sand, very dark gray (10YR 3/1) moist; 2 percent clay; structureless single grain; loose, loose, nonsticky, nonplastic; common very fine, fine, and medium roots throughout; many very fine irregular pores; 20 percent subrounded indurated mixed gravel, 15 percent subrounded indurated mixed cobbles, 15 percent subrounded indurated mixed stones; NaF pH 8.5; slightly acid (pH 6.1); abrupt smooth boundary.(0 to 45 cm thick)\nC2--85 to 150 cm; dark gray (10YR 4/1) extremely stony sandy loam, black (10YR 2/1) moist; 10 percent clay; structureless massive; loose, loose, nonsticky, nonplastic; common very fine and fine roots throughout; many very fine irregular pores; 20 percent subrounded indurated mixed gravel, 20 percent subrounded indurated mixed cobbles, 20 percent subrounded indurated mixed stones; NaF pH 9.0; strongly acid (pH 5.3)." + "content": "TYPICAL PEDON: Tigerlily muck on an east facing (75 degree), 10 percent slope with a cover of lodgepole pine and willow at an elevation of 2695 meters. (Colors are for dry soils unless otherwise noted. When described on July 8, 2013 the soil was wet throughout. Seasonal water table was observed at 67 cm.)\nOe--0 to 15 cm; very dark gray (7.5YR 3/1) mucky peat, black (5YR 2.5/1) moist; common very fine and fine roots throughout; very strongly acid (4.6); clear wavy boundary. (0 to 25 cm thick)\nOa--15 to 23 cm; dark gray (2.5Y 4/1) muck, black (10YR 2/1) moist; common very fine and fine roots throughout; 5 percent subangular indurated metamorphic gravel; very strongly acid (4.8); clear wavy boundary. (0 to 35 cm thick)\nA--23 to 30 cm; dark grayish brown (10YR 4/2) very stony sandy loam, very dark brown (10YR 2/2) moist; 5 percent clay; weak fine subangular blocky structure; soft, very friable, slightly sticky, nonplastic; common very fine and fine roots throughout; common very fine irregular pores; 5 percent subangular indurated mixed gravel, 10 percent subangular indurated mixed cobbles, 25 percent subangular indurated mixed stones; NaF pH 9.0; strongly acid (pH 5.4); clear wavy boundary. (0 to 35 cm thick)\nC1--30 to 49 cm; grayish brown (2.5Y 5/2) extremely stony sandy loam, very dark grayish brown (10YR 3/2) moist; 8 percent clay; massive; soft, very friable, nonsticky, nonplastic; common very fine roots throughout; common very fine irregular pores; 20 percent subangular indurated mixed gravel, 30 percent subangular indurated mixed cobbles, 25 percent subrounded indurated mixed stones; NaF pH 9.0; strongly acid (pH 5.4); gradual wavy boundary. (0 to 45 cm thick)\nC2--49 to 150 cm; light yellowish brown (2.5Y 6/3) extremely cobbly sandy loam, olive brown (2.5Y 4/3) moist; 8 percent clay; massive; soft, very friable, nonsticky, nonplastic; common very fine roots throughout; common very fine irregular pores; 22 percent subangular indurated mixed gravel, 23 percent subrounded indurated mixed gravel, 25 percent subangular indurated metamorphic cobbles, 5 percent subrounded indurated granite stones; NaF pH 9.0; moderately acid (pH 5.6)." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, Mineral King Rd; USGS 7.5 minute topographic quadrangle: Mineral King, California; WGS84 36.454819 latitude and -118.604072 longitude; UTM zone 11 4035593 meters N 356258 meters E NAD83." + "content": "TYPE LOCATION: Fresno County, California, Goddard Canyon, about 1.2 miles south of trail junction of switchbacks to Evolution Valley; USGS 7.5 minute topographic quadrangle: Mount Henry, California; WGS84 37.175479 latitude and -118.791404 longitude; UTM zone 11 4115841 meters N 340969 meters E WGS84." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nHistic epipedon thickness: 20 to 50 cm\nAquic conditions: present within 10 cm\nOrganic matter: 20 to 60 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate)\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 0 to 65 percent gravel, 0 to 30 percent cobbles, and 0 to 25 percent stones.\nClay content: 8 to 15 percent\nNaF pH : 8.5 to 11.0\nOa horizon (where present)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 6 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: muck\nRock fragments: 0 to 5 percent gravel\nReaction: moderately to very strongly acid\nOe horizon (where present)\nHue: 5YR, 7.5YR, 10YR\nValue: 2 to 4 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: mucky peat\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\nReaction: moderately or strongly acid\nUpper C horizon(s), where present\nHue: 10YR, 2.5Y\nValue: 4 to 6 dry, 2 to 5 moist\nChroma: 1 to 3, dry or moist\nTexture: coarse sand, sand, fine sand, loamy coarse sand, loamy sand, sandy loam\nClay content: 1 to 10 percent\nRock fragments: 0 to 75 percent\n0 to 65 percent gravel\n0 to 30 percent cobbles\n0 to 25 percent stones\nReaction: slightly to strongly acid\nLower C horizon(s)\nHue: 10YR, 2.5Y\nValue: 4 to 6 dry, 2 to 5 moist\nChroma: 1 to 3, dry or moist\nTexture: loamy coarse sand, loamy sand, sandy loam\nClay content: 8 to 15 percent\nRock fragments: 35 to 75 percent\n0 to 65 percent gravel\n0 to 30 percent cobbles\n0 to 25 percent stones\nReaction: slightly to strongly acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nHistic epipedon thickness: 20 to 40 cm\nAquic conditions: present within 10 cm\nOrganic matter: 20 to 60 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate)\nParticle size control section weighted average:\nRock fragments: 35 to 75 percent, with 0 to 65 percent gravel, 0 to 30 percent cobbles, and 0 to 25 percent stones.\nClay content: 8 to 15 percent\nNaF pH : 8.5 to 11.0\nOe horizon (where present)\nHue: 5YR, 7.5YR, 10YR\nValue: 2 to 4 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: mucky peat\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 15 percent cobbles\n0 to 15 percent stones\nReaction: moderately or strongly acid\nOa horizon (where present)\nHue: 7.5YR, 10YR, 2.5Y\nValue: 4 to 6 dry, 2 or 3 moist\nChroma: 1 or 2, dry or moist\nTexture: muck\nRock fragments: 0 to 5 percent gravel\nReaction: moderately to very strongly acid\nA horizon (where present)\nHue: 10YR\nValue: 2 to 5, dry or moist\nChroma: 1 or 2, dry or moist\nTexture: loamy sand, coarse sandy loam, sandy loam\nRock fragments: 0 to 60 percent\n0 to 35 percent gravel\n0 to 35 percent cobbles\n0 to 35 percent stones\nReaction: moderately to very strongly acid\nUpper C horizon(s), where present\nHue: 10YR, 2.5Y\nValue: 4 to 6 dry, 2 to 5 moist\nChroma: 1 to 3, dry or moist\nTexture: coarse sand, sand, fine sand, loamy coarse sand, loamy sand, sandy loam\nClay content: 1 to 10 percent\nRock fragments: 0 to 75 percent\n0 to 65 percent gravel\n0 to 30 percent cobbles\n0 to 25 percent stones\nReaction: slightly to strongly acid\nLower C horizon(s)\nHue: 10YR, 2.5Y\nValue: 4 to 6 dry, 2 to 5 moist\nChroma: 1 to 3, dry or moist\nTexture: loamy coarse sand, loamy sand, sandy loam\nClay content: 8 to 15 percent\nRock fragments: 35 to 75 percent\n0 to 65 percent gravel\n0 to 30 percent cobbles\n0 to 25 percent stones\nReaction: slightly to strongly acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -39,7 +39,7 @@ }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is tiger lily, horsetail, corn lily, bigleaf lupine, Sierra willow, Lemmon's willow, bulrush, wild onion, carex, sedges, and grasses." + "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is Sierra lodgepole pine, tiger lily, horsetail, corn lily, bigleaf lupine, Sierra willow, Lemmon's willow, bulrush, wild onion, carex, sedges, and grasses." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 67 to 142 cm\nDiagnostic horizons and features recognized in this pedon are:\nHistic Epipedon 0 to 42 cm\nAquic Conditions 0 to 150 cm\nHemic Soil Materials 13 to 42 cm\nSapric Soil Materials 0 to 13 cm\nSome pedons have A horizons between the O and C horizons.\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7925058\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 48 to 123 cm\nDiagnostic horizons and features recognized in this pedon are:\nHistic Epipedon 0 to 23 cm\nAquic Conditions 0 to 150 cm\nHemic Soil Materials 0 to 15 cm\nSapric Soil Materials 15 to 23 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2013CA7921041\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/T/TUOHY.json b/inst/extdata/OSD/T/TUOHY.json index 172a0ec347..afe0acb59e 100644 --- a/inst/extdata/OSD/T/TUOHY.json +++ b/inst/extdata/OSD/T/TUOHY.json @@ -1,17 +1,17 @@ { "SERIES": "TUOHY", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB", - "REVDATE": "05/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Tuohy series consists of shallow, well drained soils formed in colluvium, residuum and till derived from granitic and metasedimentary rock. The Tuohy soils are on structural benches and mountain slopes in the Sierra Nevada mountains. Slopes range from 3 to 60 percent. The mean annual precipitation is about 680 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Loamy, isotic, frigid Lithic Humixerepts" + "content": "TAXONOMIC CLASS: Loamy, isotic, frigid Lithic Humixerepts" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Tuohy sandy loam on a southeast facing (130 degree), 24 percent slope under cover of threadleaf sedge and Parry's rush at an elevation of 2735 meters. (Colors are for dry soils unless otherwise noted. When described on August 12, 2012 the soil was slightly moist throughout.)\nA--0 to 5 cm; grayish brown (10YR 5/2) sandy loam, very dark grayish brown (10YR 3/2) moist; 7 percent clay; weak coarse subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; common very fine and fine dendritic tubular pores; 6 percent subrounded indurated granite gravel, 5 percent subrounded indurated granite cobbles; NaF pH 9.5; strongly acid (pH 5.4); clear smooth boundary. (5 to 30 cm thick)\nBw1--5 to 20 cm; light olive brown (2.5Y 5/4) gravelly sandy loam, very dark grayish brown (2.5Y 3/2) moist; 9 percent clay; weak medium granular structure; soft, very friable, nonsticky, nonplastic; common very fine and many fine roots throughout; common very fine and fine irregular pores; 10 percent subrounded indurated granite gravel, 7 percent subrounded indurated granite cobbles; NaF pH 10.5; moderately acid (pH 5.6); clear wavy boundary.\nBw2--20 to 39 cm; dark yellowish brown (10YR 4/4) gravelly sandy loam, very dark grayish brown (2.5Y 3/2) moist; 8 percent clay; weak medium subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; common very fine, fine, and medium irregular pores; 70 percent distinct dark yellowish brown (10YR 4/4) dry, sand coats on rock fragments; 5 percent subrounded indurated granite fine gravel, 8 percent subrounded indurated granite medium gravel, 5 percent subrounded indurated granite cobbles; NaF pH 10.5; moderately acid (pH 5.6); very abrupt smooth boundary. (combined thickness of Bw horizons is 15 to 35 cm)\nR--39 to 200 cm; indurated granite bedrock with fractures 45 to less than 100 cm apart; many very fine and fine, and common medium roots in mat at top of horizon." + "content": "TYPICAL PEDON: Tuohy sandy loam on a southeast facing (130 degree), 24 percent slope under cover of threadleaf sedge and Parry's rush at an elevation of 2735 meters. (Colors are for dry soils unless otherwise noted. When described on August 12, 2012 the soil was slightly moist throughout.)\nA--0 to 5 cm; grayish brown (10YR 5/2) sandy loam, very dark grayish brown (10YR 3/2) moist; 7 percent clay; weak coarse subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; common very fine and fine dendritic tubular pores; 6 percent subrounded indurated granite gravel, 5 percent subrounded indurated granite cobbles; NaF pH 9.5; strongly acid (pH 5.4); clear smooth boundary. (5 to 30 cm thick)\nBw1--5 to 20 cm; light olive brown (2.5Y 5/4) cobbly sandy loam, very dark grayish brown (2.5Y 3/2) moist; 9 percent clay; weak medium granular structure; soft, very friable, nonsticky, nonplastic; common very fine and many fine roots throughout; common very fine and fine irregular pores; 10 percent subrounded indurated granite gravel, 7 percent subrounded indurated granite cobbles; NaF pH 10.5; moderately acid (pH 5.6); clear wavy boundary.\nBw2--20 to 39 cm; dark yellowish brown (10YR 4/4) gravelly sandy loam, very dark grayish brown (2.5Y 3/2) moist; 8 percent clay; weak medium subangular blocky structure; soft, very friable, nonsticky, nonplastic; common very fine and fine roots throughout; common very fine, fine, and medium irregular pores; 70 percent distinct dark yellowish brown (10YR 4/4) dry, sand coats on rock fragments; 5 percent subrounded indurated granite fine gravel, 8 percent subrounded indurated granite medium gravel, 5 percent subrounded indurated granite cobbles; NaF pH 10.5; moderately acid (pH 5.6); very abrupt smooth boundary. (combined thickness of Bw horizons is 15 to 35 cm)\nR--39 to 200 cm; indurated granite bedrock with fractures 45 to less than 100 cm apart; many very fine and fine, and common medium roots in mat at top of horizon." }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 18 to 40 cm\nCambic horizon thickness: 15 to 35 cm\nDepth to lithic contact: 25 to 50 cm\nReaction: very strongly to moderately acid\nBase saturation: less than 50 percent. (By ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 2.0 percent (by weight) in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 5 to 30 percent, with 5 to 30 percent gravel, 0 to 15 percent cobbles, and 0 to 5 percent stones.\nClay content: 6 to 15 percent\nNaF pH: 8.5 to 11.0\nA horizon (s)\nHue: 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 to 3 moist\nTexture: fine sandy loam, sandy loam\nClay content: 5 to 10 percent\nRock fragments: 5 to 30 percent\n5 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\nBw horizon (s)\nHue: 2.5YR, 10YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 2 to 4 dry, 1 to 3 moist\nTexture: loam, fine sandy loam, sandy loam\nClay content: 6 to 15 percent\nRock fragments: 10 to 35 percent\n10 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 4 to 10 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 18 to 35 cm\nCambic horizon thickness: 15 to 32 cm\nDepth to lithic contact: 25 to 50 cm\nReaction: very strongly to moderately acid\nBase saturation: less than 50 percent. (By ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 2.0 percent (by weight) in an 18 cm thick layer within a depth of 75 cm from the mineral soil surface\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 5 to 30 percent, with 5 to 30 percent gravel, 0 to 15 percent cobbles, and 0 to 5 percent stones.\nClay content: 6 to 15 percent\nNaF pH: 8.5 to 11.0\nA horizon (s)\nHue: 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3 dry, 1 to 3 moist\nTexture: fine sandy loam, sandy loam\nClay content: 5 to 10 percent\nRock fragments: 5 to 30 percent\n5 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones\nBw horizon (s)\nHue: 2.5YR, 10YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 2 to 4 dry, 1 to 3 moist\nTexture: loam, fine sandy loam, sandy loam\nClay content: 6 to 15 percent\nRock fragments: 10 to 35 percent\n10 to 30 percent gravel\n0 to 15 percent cobbles\n0 to 5 percent stones" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 25 to 39 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 0 to 20 cm\nCambic Horizon 5 to 39 cm\nLithic Contact 39 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nNASIS User Pedon ID: 2012CA7928008\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 25 to 39 cm\nDiagnostic horizons and features recognized in this pedon are:\nUmbric Epipedon 0 to 20 cm\nCambic Horizon 20 to 39 cm\nLithic Contact 39 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nNASIS User Pedon ID: 2012CA7928008\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/W/WAGER.json b/inst/extdata/OSD/W/WAGER.json index 070a503127..a985361db3 100644 --- a/inst/extdata/OSD/W/WAGER.json +++ b/inst/extdata/OSD/W/WAGER.json @@ -1,17 +1,17 @@ { "SERIES": "WAGER", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB", "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Wager series consists of very deep, very poorly drained soils formed in organic material over alluvium derived from granitic rocks. The Wager soils are on flood plains of the Sierra Nevada Mountains. Slopes range from 2 to 8 percent. The mean annual precipitation is about 1000 mm and the mean annual air temperature is about 5 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", - "content": "TAXONOMIC CLASS: Sandy or sandy-skeletal, isotic, euic, frigid Terric Haplosaprists" + "content": "TAXONOMIC CLASS: Sandy or sandy-skeletal, isotic, euic, frigid Terric Haplosaprists" }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Wager mucky peat on a west-facing (295 degree), 7 percent slope under a cover of shooting star, juncus, bulrush, Sierra willow, and Lemmon's willow at an elevation of 2135 meters. (Colors are for dry soils unless otherwise noted. When described on August 9, 2017 the soil was moist throughout.)\nOe--0 to 18 cm; brown (7.5YR 4/2) mucky peat, very dark brown (10YR 2/2) moist; about 60 percent fiber, 20 percent rubbed; massive; nonsticky, nonplastic; many very fine, fine, and medium roots throughout; many very fine and common fine and medium irregular pores; moderately acid (pH 5.6); clear smooth boundary. (0 to 20 cm thick) Lab sample # 17N04656\nOa--18 to 46 cm; dark grayish brown (10YR 4/2) muck, 20 percent black (10YR 2/1) and 80 percent very dark brown (10YR 2/2) moist; about 15 percent fiber, 5 percent rubbed; weak medium subangular blocky structure; slightly sticky, nonplastic; common very fine and fine roots throughout; many very fine and common fine irregular pores; very strongly acid (pH 5.0); abrupt smooth boundary. (0 to 65 cm thick) Lab sample # 17N04657\nCg1--46 to 95 cm; gray (2.5Y 6/1) loamy coarse sand, dark greenish gray (10Y 3/1) moist; 78 percent sand; 16 percent silt; 6 percent clay; massive; moderately hard, firm, slightly sticky, nonplastic; few very fine roots throughout; common very fine irregular pores; NaF pH 8.6; moderately acid (pH 5.7); abrupt smooth boundary. (5 to 60 cm thick) Lab sample # 17N04658\nCg2--95 to 178 cm; light gray (2.5Y 7/1) coarse sand, gray (2.5Y 5/1) moist; 91 percent sand; 8 percent silt; 1 percent clay; single grain; loose, loose, nonsticky, nonplastic; common very fine, fine, and medium interstitial pores; reduced matrix; 2 percent subrounded indurated granite fine gravel; NaF pH 9.1; moderately acid (pH 6.0). (5 to 85 cm thick) Lab sample # 17N04659" + "content": "TYPICAL PEDON: Wager mucky peat on a west-facing (295 degree), 7 percent slope under a cover of shooting star, juncus, bulrush, Sierra willow, and Lemmon's willow at an elevation of 2135 meters. (Colors are for dry soils unless otherwise noted. When described on August 9, 2017 the soil was moist throughout.)\nOe--0 to 18 cm; brown (7.5YR 4/2) mucky peat, very dark brown (10YR 2/2) moist; about 60 percent fiber, 20 percent rubbed; massive; nonsticky, nonplastic; many very fine, fine, and medium roots throughout; many very fine and common fine and medium irregular pores; moderately acid (pH 5.6); clear smooth boundary. (0 to 20 cm thick) Lab sample # 17N04656\nOa--18 to 46 cm; dark grayish brown (10YR 4/2) muck, 20 percent black (10YR 2/1) and 80 percent very dark brown (10YR 2/2) moist; about 15 percent fiber, 5 percent rubbed; weak medium subangular blocky structure; slightly sticky, nonplastic; common very fine and fine roots throughout; many very fine and common fine irregular pores; very strongly acid (pH 5.0); abrupt smooth boundary. (0 to 60 cm thick) Lab sample # 17N04657\nCg1--46 to 95 cm; gray (2.5Y 6/1) loamy coarse sand, dark greenish gray (10Y 3/1) moist; 78 percent sand; 16 percent silt; 6 percent clay; massive; moderately hard, firm, slightly sticky, nonplastic; few very fine roots throughout; common very fine irregular pores; NaF pH 8.6; moderately acid (pH 5.7); abrupt smooth boundary. (5 to 60 cm thick) Lab sample # 17N04658\nCg2--95 to 178 cm; light gray (2.5Y 7/1) coarse sand, gray (2.5Y 5/1) moist; 91 percent sand; 8 percent silt; 1 percent clay; single grain; loose, loose, nonsticky, nonplastic; common very fine, fine, and medium interstitial pores; reduced matrix; 2 percent subrounded indurated granite fine gravel; NaF pH 9.1; moderately acid (pH 6.0). (5 to 85 cm thick) Lab sample # 17N04659" }, "TYPE LOCATION": { "section": "TYPE LOCATION", @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nHistic epipedon thickness: 20 to 40 cm\nAquic conditions: present within 10 cm\nOrganic matter: 20 to 75 percent in the epipedon\nBase saturation: less than 50 percent (by ammonium acetate)\nParticle size control section weighted average:\nRock fragments: 0 to 10 percent gravel\nClay content: 1 to 8 percent\nNaF pH: 8.0 to 11\nOe horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 or 4 dry, 2 moist\nChroma: 1 or 2, dry or moist\nTexture: mucky peat\nRock fragments: 0 to 20 percent gravel\nReaction: moderately to very strongly acid\nOa horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 to 6 dry, 2 moist\nChroma: 1 or 2, dry or moist\nTexture: muck\nRock fragments: 0 to 20 percent gravel\nReaction: moderately to very strongly acid\nCg1 horizon\nHue: 2.5YR, 10YR\nValue: 4 to 6 dry, 3 or 4 moist\nChroma: 1 or 2, dry or moist\nTexture: coarse sand, loamy coarse sand, loamy sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 5 percent gravel\nReaction: moderately or strongly acid\nCg2 horizon\nHue: 2.5YR, 10YR\nValue: 4 to 7 dry, 3 to 5 moist\nChroma: 1 or 2, dry or moist\nTexture: coarse sand, loamy coarse sand, loamy sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 60 percent gravel\nReaction: strongly or very strongly acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil moisture: The soil is saturated in some part throughout the year, with a seasonal high water table dropping below 50 cm in late summer and fall. The soils have an aquic soil moisture regime.\nDiagnostic Feature(s):\nAquic conditions: present within 10 cm\nOrganic matter: 20 to 75 percent in the organic horizons\nBase saturation: less than 50 percent (by ammonium acetate)\nDepth to redoximorphic features: 25 to 50 cm\nParticle size control section weighted average:\nRock fragments: 0 to 10 percent gravel\nClay content: 1 to 8 percent\nNaF pH: 8.0 to 11\nOe horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 or 4 dry, 2 moist\nChroma: 1 or 2, dry or moist\nTexture: mucky peat\nRock fragments: 0 to 20 percent gravel\nReaction: moderately to very strongly acid\nOa horizon(s)\nHue: 7.5YR, 10YR\nValue: 3 to 6 dry, 2 moist\nChroma: 1 or 2, dry or moist\nTexture: muck\nRock fragments: 0 to 20 percent gravel\nReaction: moderately to very strongly acid\nCg1 horizon\nHue: 10YR, 2.5Y\nValue: 4 to 6 dry, 3 or 4 moist\nChroma: 1 or 2, dry or moist\nTexture: coarse sand, loamy coarse sand, loamy sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 5 percent gravel\nReaction: moderately or strongly acid\nCg2 horizon\nHue: 10YR, 2.5Y\nValue: 4 to 7 dry, 3 to 5 moist\nChroma: 1 or 2, dry or moist\nTexture: coarse sand, loamy coarse sand, loamy sand\nClay content: 1 to 8 percent\nRock fragments: 0 to 60 percent gravel\nReaction: moderately or strongly acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 46 to 76 cm\nDiagnostic horizons and features recognized in this pedon are:\nHistic Epipedon 0 to 40 cm\nHemic Soil Materials 0 to 18 cm\nAquic Conditions 0 to 178 cm\nSapric Soil Materials 18 to 46 cm\nReduced Matrix 95 to 178 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nPedon Type: OSD pedon\nPedon Purpose: laboratory sampling site Lab Pedon #: 17N0931\nNASIS User Pedon ID: S2017CA107002\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 46 to 76 cm\nDiagnostic horizons and features recognized in this pedon are:\nHemic Soil Materials 0 to 18 cm\nAquic Conditions 0 to 178 cm\nSapric Soil Materials 18 to 46 cm\nReduced Matrix 95 to 178 cm\nADDITIONAL DATA:\nPedon information for this type location only:\nPedon Type: OSD pedon\nPedon Purpose: laboratory sampling site Lab Pedon #: 17N0931\nNASIS User Pedon ID: S2017CA107002\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/W/WHISKEYLOG.json b/inst/extdata/OSD/W/WHISKEYLOG.json index f75659e8d7..da1e9cc5e7 100644 --- a/inst/extdata/OSD/W/WHISKEYLOG.json +++ b/inst/extdata/OSD/W/WHISKEYLOG.json @@ -1,8 +1,8 @@ { "SERIES": "WHISKEYLOG", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "JBB/CES/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Whiskeylog series consists of very deep, well drained soils formed in colluvium and residuum derived from metamorphic rock. The Whiskeylog soils are on mountain slopes of the Sierra Nevada Mountains. Slopes range from 30 to 60 percent. The mean annual precipitation is about 895 mm and the mean annual air temperature is about 12 degrees C.", "TAXONOMIC CLASS": { @@ -11,15 +11,15 @@ }, "TYPICAL PEDON": { "section": "TYPICAL PEDON", - "content": "TYPICAL PEDON: Whiskeylog gravelly very fine sandy loam on a southeast-facing (163 degree), 36 percent slope under mixed oak woodland at an elevation of 1249 meters. (Colors are for dry soils unless otherwise noted. When described on March 13, 2014 the soil was moist throughout.)\nA1--0 to 6 cm; yellowish brown (10YR 5/4) gravelly very fine sandy loam, dark brown (7.5YR 3/3) moist; 10 percent clay; weak fine granular structure; soft, very friable, nonsticky, nonplastic; many very fine and common fine roots throughout; common very fine irregular pores; 15 percent subangular indurated metavolcanic fine gravel; NaF pH 9.0; slightly acid (pH 6.2); clear smooth boundary. (combined thickness of the A horizons is 5 to 18 cm)\nA2--6 to 17 cm; dark yellowish brown (10YR 4/4) very fine sandy loam, dark brown (7.5YR 3/4) moist; 10 percent clay; weak fine and medium subangular blocky structure; slightly hard, friable, nonsticky, nonplastic; many very fine and few fine roots throughout; common very fine irregular pores; 5 percent subangular indurated metavolcanic fine gravel; NaF pH 9.0; moderately acid (pH 6.0); abrupt smooth boundary.\nBt1--17 to 46 cm; strong brown (7.5YR 4/6) gravelly very fine sandy loam, dark reddish brown (5YR 3/4) moist; 18 percent clay; moderate medium subangular blocky structure; moderately hard, firm, slightly sticky, slightly plastic; common very fine and few fine roots throughout; common fine and medium dendritic tubular pores; 4 percent clay films on bottom faces of peds; 25 percent subangular indurated metavolcanic gravel, 1 percent subangular indurated metavolcanic cobbles; NaF pH 9.5; moderately acid (pH 5.8); gradual smooth boundary. (combined thickness of the upper Bt horizons is 20 to 75 cm)\nBt2--46 to 65 cm; reddish brown (5YR 4/4) very gravelly sandy clay loam, dark red (2.5YR 3/6) moist; 25 percent clay; moderate medium subangular blocky structure; moderately hard, firm, slightly sticky, slightly plastic; common very fine and few fine roots throughout; common fine and medium dendritic tubular pores; 15 percent clay films on all faces of peds; 30 percent subangular indurated metavolcanic gravel, 5 percent subangular indurated metavolcanics cobbles; NaF pH 9.5; moderately acid (pH 5.8); clear smooth boundary.\nBt3--65 to 134 cm; yellowish red (5YR 5/8) extremely gravelly sandy clay loam, red (2.5YR 4/6) moist; 23 percent clay; moderate medium subangular blocky structure; hard, very firm, slightly sticky, slightly plastic; few very fine roots throughout; common very fine and fine dendritic tubular pores; 7 percent clay films on bottom faces of peds; 55 percent subangular indurated metavolcanics gravel, 15 percent subangular indurated metavolcanics cobbles; NaF pH 9.0; moderately acid (pH 5.6)." + "content": "TYPICAL PEDON: Whiskeylog sandy loam on a southeast-facing (120 degree), 40 percent slope under mixed oak woodland at an elevation of 1469 meters. (Colors are for dry soils unless otherwise noted. When described on June 2, 2014 the soil was dry to 37 cm.)\nOi--0 to 2 cm; yellowish brown (10YR 5/4) slightly decomposed plant material, dark yellowish brown (10YR 4/4) moist; neutral (pH 6.6); clear smooth boundary. (0 to 5 cm thick)\nA--2 to 9 cm; brown (7.5YR 5/3) sandy loam, very dark brown (7.5YR 2.5/2) moist; 10 percent clay; weak very fine and fine granular structure; soft, very friable, slightly sticky, nonplastic; many very fine roots throughout; many very fine and fine irregular pores; 10 percent subangular indurated metasedimentary gravel; NaF pH 9.0; neutral (pH 6.8); clear smooth boundary. (5 to 18 cm thick)\nBw1--9 to 37 cm; brown (7.5YR 4/4) loam, dark brown (7.5YR 3/3) moist; 16 percent clay; moderate fine subangular blocky structure; slightly hard, very friable, slightly sticky, slightly plastic; common very fine and fine roots throughout; many very fine and common fine irregular pores; 7 percent subangular indurated metasedimentary gravel; NaF pH 9.5; slightly acid (pH 6.4); gradual smooth boundary.\nBw2--37 to 86 cm; brown (7.5YR 4/4) loam, dark brown (7.5YR 3/4) moist; 18 percent clay; weak fine subangular blocky structure; slightly hard, friable, moderately sticky, moderately plastic; common very fine, fine, medium, and coarse roots throughout; many very fine and fine irregular, and common medium tubular pores; 2 percent subrounded indurated metasedimentary gravel, 1 percent subrounded indurated metasedimentary cobbles; NaF pH 9.5; slightly acid (pH 6.4); gradual smooth boundary. (combined thickness of Bw horizons is 0 to 75 cm)\nBt--86 to 140 cm; strong brown (7.5YR 4/6) loam, reddish brown (5YR 4/4) moist; 22 percent clay; weak fine subangular blocky structure; slightly hard, friable, moderately sticky, moderately plastic; common fine, medium, and coarse roots throughout; many fine irregular and common medium tubular pores; 10 percent faint clay films on all faces of peds; 10 percent subrounded indurated metasedimentary gravel, 3 percent subrounded indurated metasedimentary cobbles; NaF pH 9.0; moderately acid (pH 6.0)." }, "TYPE LOCATION": { "section": "TYPE LOCATION", - "content": "TYPE LOCATION: Tulare County, California, on the Generals Highway; USGS 7.5 minute topographic quadrangle: Giant Forest, California; WGS84 36.539353 latitude and -118.779964 longitude; UTM zone 11 4045248 meters N 340668 meters E WGS84." + "content": "TYPE LOCATION: Tulare County, California, off the Ladybug Trail in the South Fork area of Sequoia National Park; USGS 7.5 minute topographic quadrangle: Moses Mountain, California; WGS84 36.353092 latitude and -118.737902 longitude; UTM zone 11 4024515 meters N 344061 meters E NAD83." }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 10 to 15 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nOchric epipedon thickness: 10 to 30 cm\nArgillic horizon thickness: 60 to 110 cm\nBase saturation35 to 75 percent in one or more subhorizons of the upper 75 cm of the argillic horizon (by sum of cations)\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 35 percent gravel and 0 to 15 percent cobbles.\nClay content: 18 to 27 percent\nNaF pH: 8.5 to 10.0\nA horizon(s)\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 to 4, dry or moist\nTexture: very fine sandy loam, sandy loam, loamy fine sand\nClay content: 6 to 16 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 5 percent cobbles\nReaction: slightly acid to neutral\nBw horizon (where present)\nHue: 7.5YR, 10YR\nValue: 4 to 6 dry, 3 or 4 moist\nChroma: 4 or 6 dry, 3 or 4 moist\nTexture: very fine sandy loam, sandy loam, loam\nClay content: 8 to 18 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 5 percent cobbles\nReaction: slightly acid to neutral\nUpper Bt horizon(s)\nHue: 2.5YR, 5YR, 7.5YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 4 or 6 dry, 3 to 6 moist\nTexture: very fine sandy loam, loam, sandy clay loam\nClay content: 18 to 27 percent\nRock fragments: 0 to 35 percent\n0 to 35 percent gravel\n0 to 15 percent cobbles\nReaction: moderately to slightly acid\nLower Bt horizon (Bt3)\nHue: 2.5YR, 5YR, 7.5YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 4 to 8 dry, 3 to 6 moist\nTexture: very fine sandy loam, loam, sandy clay loam\nClay content: 18 to 27 percent\nRock fragments: 0 to 75 percent\n0 to 60 percent gravel\n0 to 15 percent cobbles\nReaction: moderately to slightly acid" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 10 to 15 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a mesic temperature regime.\nSoil moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about July to October (about 120 days).\nDiagnostic Feature(s):\nOchric epipedon thickness: 10 to 30 cm\nCambic horizon thickness: 0 to 75 cm\nArgillic horizon thickness: 60 to 140 cm\nBase saturation: 35 to 75 percent in one or more subhorizons of the upper 75 cm of the argillic horizon (by sum of cations)\nParticle size control section weighted average:\nRock fragments: 0 to 35 percent, with 0 to 35 percent gravel and 0 to 15 percent cobbles.\nClay content: 18 to 27 percent\nNaF pH: 8.5 to 10.0\nA horizon(s)\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 to 4, dry or moist\nTexture: very fine sandy loam, sandy loam, loamy fine sand\nClay content: 6 to 16 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 5 percent cobbles\nReaction: slightly acid to neutral\nBw horizon(s) (where present)\nHue: 7.5YR, 10YR\nValue: 4 to 6 dry, 3 or 4 moist\nChroma: 4 or 6 dry, 3 or 4 moist\nTexture: very fine sandy loam, fine sandy loam, sandy loam, loam\nClay content: 8 to 18 percent\nRock fragments: 0 to 15 percent\n0 to 15 percent gravel\n0 to 5 percent cobbles\nReaction: slightly acid to neutral\nUpper Bt horizon(s)\nHue: 2.5YR, 5YR, 7.5YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 4 or 6 dry, 3 to 6 moist\nTexture: very fine sandy loam, fine sandy loam, loam, sandy clay loam\nClay content: 18 to 27 percent\nRock fragments: 0 to 35 percent\n0 to 35 percent gravel\n0 to 15 percent cobbles\nReaction: moderately to slightly acid\nLower Bt horizon(s) (where present)\nHue: 2.5YR, 5YR, 7.5YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 4 to 8 dry, 3 to 6 moist\nTexture: very fine sandy loam, loam, sandy clay loam\nClay content: 18 to 27 percent\nRock fragments: 0 to 75 percent\n0 to 60 percent gravel\n0 to 15 percent cobbles\nReaction: moderately to slightly acid" }, "COMPETING SERIES": { "section": "COMPETING SERIES", @@ -27,7 +27,7 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Whiskeylog soils are on linear to convex backslopes of mountain slopes. Slopes range from 30 to 60 percent. These soils formed in colluvium derived from metasedimentary and metavolcanics rock. Elevation is 900 to 1940 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 730 to 1030 mm and the mean annual air temperature is 10 to 15 degrees C. The frost free season is 160 to 245 days." + "content": "GEOGRAPHIC SETTING: The Whiskeylog soils are on linear to convex backslopes of mountain slopes. Slopes range from 30 to 60 percent. These soils formed in colluvium derived from metasedimentary and metavolcanic rock. Elevation is 900 to 1940 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 730 to 1030 mm and the mean annual air temperature is 10 to 15 degrees C. The frost free season is 160 to 245 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", @@ -39,7 +39,7 @@ }, "USE AND VEGETATION": { "section": "USE AND VEGETATION", - "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is black oak, canyon line oak, incense cedar, poison oak, alderleaf mountain mahogany, and annual grasses and forbs." + "content": "USE AND VEGETATION: This soil is used for recreation, wildlife habitat, and watershed. Vegetation is black oak, canyon live oak, incense cedar, poison oak, alderleaf mountain mahogany, and annual grasses and forbs." }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", @@ -55,6 +55,6 @@ }, "REMARKS": { "section": "REMARKS", - "content": "REMARKS:\nParticle Size Control Section for this pedon: 86 to 136 cm.\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 0 to 17 cm\nArgillic Horizon 17 to 150 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7927002\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." + "content": "REMARKS:\nParticle Size Control Section for this pedon: 86 to 136 cm\nDiagnostic horizons and features recognized in this pedon are:\nOchric Epipedon 2 to 20 cm\nCambic Horizon 9 to 86 cm\nArgillic Horizon 86 to 150 cm\nADDITIONAL DATA:\nNASIS User Pedon ID: 2014CA7921001\nSoil classified using the 12th Edition of the Keys to Soil Taxonomy.\nNational Cooperative Soil Survey\nU.S.A." } } diff --git a/inst/extdata/OSD/W/WINDOWPEAK.json b/inst/extdata/OSD/W/WINDOWPEAK.json index 09f1fba272..0a1eff0325 100644 --- a/inst/extdata/OSD/W/WINDOWPEAK.json +++ b/inst/extdata/OSD/W/WINDOWPEAK.json @@ -1,8 +1,8 @@ { "SERIES": "WINDOWPEAK", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", "OVERVIEW": "The Windowpeak series consists of very deep, well or somewhat excessively drained soils formed in colluvium and/or till derived from granite and granodiorite. Windowpeak soils are on moraines and mountain slopes in the Sierra Nevada mountains. Slopes range from 3 to 75 percent. The mean annual precipitation is about 1095 mm and the mean annual air temperature is about 6 degrees C.", "TAXONOMIC CLASS": { @@ -19,7 +19,7 @@ }, "RANGE IN CHARACTERISTICS": { "section": "RANGE IN CHARACTERISTICS", - "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 50 to 100 cm\nReaction: slightly to strongly acid\nBase saturation: less than 50 percent in some or all parts of the epipedon (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 150 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 70 percent, with 20 to 60 percent gravel, 15 to 35 percent cobbles, 5 to 35 percent stones, and 0 to 15 percent boulders.\nClay content: 2 to 10 percent\nNaF pH: 9.0 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 2 to 6 percent\nRock fragments: 5 to 65 percent\n5 to 50 percent gravel\n0 to 30 percent cobbles\n0 to 30 percent stones\n0 to 30 percent boulders\nBw1 horizon\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 to 4 dry, 2 or 3 moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 2 to 10 percent\nRock fragments: 15 to 70 percent\n10 to 45 percent gravel\n5 to 30 percent cobbles\n0 to 30 percent stones\n0 to 30 percent boulders\nBw2 horizon\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 3 or 4 dry, 2 to 4 moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 2 to 6 percent\nRock fragments: 35 to 70 percent\n15 to 45 percent gravel\n10 to 30 percent cobbles\n10 to 30 percent stones\n0 to 30 percent boulders\nC horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 5 or 6 dry, 3 or 4 moist\nChroma: 2 to 4, dry or moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 1 to 5 percent\nRock fragments: 35 to 70 percent\n15 to 50 percent gravel\n10 to 30 percent cobbles\n10 to 30 percent stones\n0 to 15 percent boulders" + "content": "RANGE IN CHARACTERISTICS:\nSoil temperature: The mean annual soil temperature at 50 cm is 0 to 8 degrees C and the difference between mean summer and mean winter soil temperature is greater than 6 degrees C. The soils have a frigid temperature regime.\nSoil Moisture: The soils have a xeric soil moisture regime. The soil moisture control section is dry in all parts from about August to October (about 90 days).\nDiagnostic Feature(s):\nUmbric epipedon thickness: 50 to 100 cm\nReaction: slightly to strongly acid\nBase saturation: less than 50 percent in some or all parts of the epipedon (by ammonium acetate)\nAcid-oxalate extractable Al plus 1/2 Fe: 0.4 to 1.0 percent (by weight) to a depth of 150 cm\nVolcanic glass: 5 to 30 percent in the 0.02 to 2.0 mm fraction in an 18 cm thick layer within a depth of 75cm from the mineral soil surface\nParticle size control section weighted average:\nRock fragments: 35 to 70 percent, with 20 to 60 percent gravel, 15 to 35 percent cobbles, 5 to 35 percent stones, and 0 to 15 percent boulders.\nClay content: 2 to 10 percent\nNaF pH: 9.0 to 11.0\nA horizon\nHue: 7.5YR, 10YR\nValue: 3 to 5 dry, 2 or 3 moist\nChroma: 2 or 3, dry or moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 2 to 6 percent\nRock fragments: 5 to 65 percent\n5 to 50 percent gravel\n0 to 30 percent cobbles\n0 to 30 percent stones\n0 to 30 percent boulders\nBw1 horizon\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 2 or 3 moist\nChroma: 2 to 4 dry, 2 or 3 moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 2 to 10 percent\nRock fragments: 15 to 70 percent\n10 to 45 percent gravel\n5 to 30 percent cobbles\n0 to 30 percent stones\n0 to 30 percent boulders\nBw2 horizon\nHue: 7.5YR, 10YR\nValue: 4 or 5 dry, 3 or 4 moist\nChroma: 3 or 4 dry, 2 to 4 moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 2 to 6 percent\nRock fragments: 30 to 70 percent\n15 to 45 percent gravel\n15 to 30 percent cobbles\n0 to 30 percent stones\n0 to 30 percent boulders\nC horizon\nHue: 7.5YR, 10YR, 2.5Y\nValue: 5 or 6 dry, 3 or 4 moist\nChroma: 2 to 4, dry or moist\nTexture: sand, loamy coarse sand, loamy sand, loamy fine sand\nClay content: 1 to 5 percent\nRock fragments: 35 to 70 percent\n15 to 50 percent gravel\n10 to 30 percent cobbles\n10 to 30 percent stones\n0 to 15 percent boulders" }, "COMPETING SERIES": { "section": "COMPETING SERIES", diff --git a/inst/extdata/OSD/Y/YUCCACREEK.json b/inst/extdata/OSD/Y/YUCCACREEK.json index ec8e7e3555..153158fb3e 100644 --- a/inst/extdata/OSD/Y/YUCCACREEK.json +++ b/inst/extdata/OSD/Y/YUCCACREEK.json @@ -1,10 +1,10 @@ { "SERIES": "YUCCACREEK", - "STATUS": "Tentative Series", + "STATUS": "Established Series", "BYREV": "CES/JBB/JTW", - "REVDATE": "01/2020", + "REVDATE": "06/2021", "STATES": "CA", - "OVERVIEW": "The Yuccacreek series consists of very deep, well drained soils formed in colluvium and residuum derived from metamorphic rock. Yuccacreek soils are on hills and mountains. Slopes range from 45 to 70 percent. The mean annual precipitation is about 750 mm and the mean annual air temperature is about 15 degrees C.", + "OVERVIEW": "The Yuccacreek series consists of very deep, well drained soils formed in colluvium and residuum derived from metamorphic and granitic rock. Yuccacreek soils are on hills and mountains. Slopes range from 45 to 70 percent. The mean annual precipitation is about 750 mm and the mean annual air temperature is about 15 degrees C.", "TAXONOMIC CLASS": { "section": "TAXONOMIC CLASS", "content": "TAXONOMIC CLASS: Coarse-loamy, mixed, superactive, thermic Ultic Argixerolls" @@ -27,7 +27,7 @@ }, "GEOGRAPHIC SETTING": { "section": "GEOGRAPHIC SETTING", - "content": "GEOGRAPHIC SETTING: The Yuccacreek soils are on linear backslopes of hills and mountain slopes. Slopes range from 45 to 70 percent. These soils formed in colluvium and residuum derived from metamorphic rock. Elevation is 545 to 1280 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 685 to 855 mm and the mean annual air temperature is 14 to 17 degrees C. The frost free season is 225 to 270 days." + "content": "GEOGRAPHIC SETTING: The Yuccacreek soils are on linear backslopes of hills and mountain slopes. Slopes range from 45 to 70 percent. These soils formed in colluvium and residuum derived from metamorphic and granitic rock. Elevation is 545 to 1280 meters. The climate is Mediterranean with warm, dry summers and cool, moist winters. The mean annual precipitation is 685 to 855 mm and the mean annual air temperature is 14 to 17 degrees C. The frost free season is 225 to 270 days." }, "GEOGRAPHICALLY ASSOCIATED SOILS": { "section": "GEOGRAPHICALLY ASSOCIATED SOILS", @@ -43,7 +43,7 @@ }, "DISTRIBUTION AND EXTENT": { "section": "DISTRIBUTION AND EXTENT", - "content": "DISTRIBUTION AND EXTENT: Sierra Nevada Mountains of California; MLRA 22A, Sequoia National Park. These soils are not extensive." + "content": "DISTRIBUTION AND EXTENT: Sierra Nevada Foothills of California; MLRA 18, Sequoia National Park. These soils are not extensive." }, "REGIONAL OFFICE": { "section": "SOIL SURVEY REGIONAL OFFICE (SSRO) RESPONSIBLE", From 41ae0056c698336b4e7008a3523f4bd016da6a9e Mon Sep 17 00:00:00 2001 From: Dylan Beaudette Date: Mon, 21 Jun 2021 13:39:43 -0700 Subject: [PATCH 3/3] adding examples, this documents some of the important challenges / solutions over the years --- misc/parseOSD-migration/example.R | 244 ++++++++++++++++++++++++++++++ 1 file changed, 244 insertions(+) create mode 100644 misc/parseOSD-migration/example.R diff --git a/misc/parseOSD-migration/example.R b/misc/parseOSD-migration/example.R new file mode 100644 index 0000000000..815962d2d3 --- /dev/null +++ b/misc/parseOSD-migration/example.R @@ -0,0 +1,244 @@ +library(stringi) +library(purrr) +library(httr) +library(rvest) +library(plyr) +library(aqp) + +source('local_functions.R') + + +# funky SSRO1-style OSDs, put drainage class up top +res <- testIt('ZYGORE') +res$`site-data` + +res <- testItLocal('ZYGORE') +res$`site-data` + + + +testIt('PAIA') + + +testIt('TINTERO') + + +# color moist and dry not correctly interpreted +testIt('KALAPA') + + +# old-style O horizons and formatting errors +# https://github.com/dylanbeaudette/parse-osd/issues/12 +testIt('KLAWASI') + +# +testIt('tiger creek') + +# TYPICAL PEDON section is mis-labeled +# https://casoilresource.lawr.ucdavis.edu/sde/?series=MEIKLE +testIt('MEIKLE') + +# O insteat of 0 in "1OYR 6/3" +# https://casoilresource.lawr.ucdavis.edu/sde/?series=ESPARTO +testIt('ESPARTO') + +# latest OSD from Kyle +# informed by his OSD synthesis via NASIS report / components +testIt('bordengulch') + +# missing typical pedon header +testIt('ARIEL') + +# no simple fix:" "O" instead of "0" in depths and colors +testIt('kuck') + +# works +testIt('downer') + +# missing "cm" +testIt('hammonton') + +# +testIt('drummer') + + +# brief narrative not parsed, extra white space after SERIES +testIt('ATOMIC') + +# brief narrative not parsed: fixed 2017-09-02 +testIt('amador') + +# typos related to OCR: fixed 2017-08-08 +testIt('rincon') + +# typos related to OCR: fixed 2017-08-08 +testIt('solano') + +# first horizon depths use inconsistent units specification: incorrect conversion applied +testIt('proper') + +# can't parse (N 3/) +testIt('demas') + +# horizons are multi-line records... REGEX can't parse +testIt('HELMER') + +# fixed B and N hues +testIt('SOUTHPOINT') + +# fixed: 5GY hues +testIt('figgs') + +# fixed +# multiple matches in type location +testIt('URLAND') + +# fixed +# multiple, exact matches for typical pedon +testIt('MANASTASH') +testIt('KEAA') + +# missing "TYPICAL PEDON" +testIt('ARIEL') +testIt('PACKSADDLE') + +# no white space, fixed +# "TYPICAL PEDON:" +testIt('dinuba') + +# "TYPICAL PEDON;" +testIt('NEISSENBERG') + +# funky white space +testIt('ODESSA') + +## multiple matches for typical pedon +testIt('CAJON') + +## no OSD.. +testIt('FUCHES') + +# white-space in front of section names: fixed +testIt('BRYMAN') + +# missing dry/moist flag +testIt('ADAMSTOWN') +extractSections(x) + + +testIt('Funkstown') + + +# section names have no spaces... +testIt('TUSKAHOMA') + + +# typos and ? +testIt('vance') + + +# extra "----" +testIt('Ravenrock') + + +# neutral hues +testIt('Yorkville') + + +# error in OSD, 'O' should be '0' +testIt('clear lake') + + +# error in OSD, 'O' should be '0' +testIt('iron mountain') + + +# errors in OSD: "A1, A3--0 to 19 inches;" +testIt('whitney') + + +# "l" and "O" used instead of "1" and "0" +# must fix OSD +testIt('SIRRETTA') + + +# can't parse this: (10YR 3/1 moist or dry) +testIt('salinas') + + +# error in O horizon narrative +testIt('CROQUIB') + + +# false-positives matched in RIC section +# -> fixed in post-processing SQL code +testIt('humeston') + + +# variation on type location +testIt('ANAN') + + +# multiple mention of "type location" +testIt('yutan') + + +# multiple mention of "type location" +testIt('filbert') + + +# "E and Bt1" +testIt('colonie') + + +# some problematic OSDs +testIt('pardee') + + +## TODO, still not correct as all colors are moist +testIt('canarsie') + + +testIt('capay') + + +testIt('academy') + + +testIt('newot') + + +testIt('flagspring') + + +# error in "TYPICAL PEDON" heading +testIt('ACKWATER') + + +testIt('CASA GRANDE') + + +# return NULL +# strange notation: A [A1]--0 to 10 cm (4 inches) +testIt('RAPSON') + + +testIt('KILFOIL') + + +# "TYPICAL PEDON-" +testIt('MENTZ') + + +# non-standard TYPE LOCATION heading +testIt('ALBUS') + + +# no OSD document +testIt('YALE') + + + + + +# parsing all of the series data could be done from the SC database...