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Update inst/extdata/ JSON files
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SoilKnowledgeBot committed Jul 22, 2024
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95 changes: 59 additions & 36 deletions inst/extdata/OSD/V/VENTRIS.json
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"SERIES": "VENTRIS",
"STATUS": "Established Series",
"BYREV": "Rev. LAQ",
"REVDATE": "10/2003",
"REVDATE": "07/2024",
"STATES": "AR",
"OVERVIEW": "The Ventris series consists of moderately deep, moderately well drained soils with very slow permeability. They formed in\nresidual material weathered from dolomite, limestone, or\ncalcareous shales. These soils are on uplands in the Ozark\nHighland. Slopes range from 3 to 40 percent.",
"OVERVIEW": "The Ventris series consists of moderately deep, moderately well drained soils with very slow permeability. They formed in residual material weathered from dolomite, limestone, or calcareous shales. These soils are on uplands in the Ozark Highland. Slopes range from 3 to 40 percent.",
"TAXONOMIC CLASS": {
"section": "TAXONOMIC CLASS",
"content": "TAXONOMIC CLASS: Very-fine, mixed, active, mesic Albaquic Hapludalfs"
},
"TYPICAL PEDON": {
"section": "TYPICAL PEDON",
"content": "TYPICAL PEDON: Ventris very cherty silt loam, 1 to 3 percent\nslopes in woodland.\n(Colors are for moist soil unless otherwise\nstated.)\nA1--0 to 2 inches; very dark grayish brown (10YR 3/2) cherty silt loam; moderate medium granular structure; friable; many fine roots; 15 percent fragments of chert; neutral; abrupt smooth boundary. (1 to 6 inches thick)\nA2--2 to 5 inches; brown (10YR 5/3) cherty silt loam; weak\nfine subangular blocky structure; friable; many fine roots; approximately 15 percent fragments of chert; slightly acid; abrupt smooth boundary. (0 to 5 inches thick)\nB21t--5 to 16 inches; yellowish brown (10YR 5/4) clay; common medium distinct light brownish gray (10YR 6/2) and reddish brown\n(5YR 4/4) mottles; moderate medium angular blocky structure; very firm; few fine roots; common fine pores; thin continuous clay\nfilms on faces of peds and in pores; slightly acid; gradual smooth boundary. (6 to 15 inches thick)\nB22t--16 to 32 inches; yellowish brown (10YR 5/6) clay;\ncommon medium distinct gray (10YR 6/1) mottles; moderate fine\nangular blocky structure; very firm; few fine roots; few fine\ntubular pores; thin continuous clay films on faces of peds and in pores; 15 percent fragments of limestone; common slickensides; neutral; abrupt wavy boundary. (12 to 18 inches thick)\nCr--32 to 34 inches; yellowish brown (10YR 5/8) highly\nfractured weathered dolomite.\nR--34+ inches; hard level bedded dolomite bedrock."
"content": "TYPICAL PEDON: Ventris very cherty silt loam, 1 to 3 percent slopes in woodland. (Colors are for moist soil unless otherwise stated.)\nA1--0 to 5 centimeters (0 to 2 inches); very dark grayish brown (10YR 3/2) cherty silt loam; moderate medium granular structure; friable; many fine roots; 15 percent fragments of chert; neutral; abrupt smooth boundary. (3 to 15 centimeters thick)\nA2--5 to 13 centimeters (2 to 5 inches); brown (10YR 5/3) cherty silt loam; weak fine subangular blocky structure; friable; many fine roots; approximately 15 percent fragments of chert; slightly acid; abrupt smooth boundary. (0 to 13 centimeters thick)\n2Bt1--13 to 41 centimeters (5 to 16 inches); yellowish brown (10YR 5/4) clay; common medium distinct light brownish gray (10YR 6/2) and reddish brown (5YR 4/4) mottles; moderate medium angular blocky structure; very firm; few fine roots; common fine pores; thin continuous clay films on faces of peds and in pores; slightly acid; gradual smooth boundary. (15 to 38 centimeters thick)\n2Bt2--41 to 81 centimeters (16 to 32 inches); yellowish brown (10YR 5/6) clay; common medium distinct gray (10YR 6/1) mottles; moderate fine angular blocky structure; very firm; few fine roots; few fine tubular pores; thin continuous clay films on faces of peds and in pores; 15 percent fragments of limestone; common slickensides; neutral; abrupt wavy boundary. (30 to 46 centimeters thick)\nCr--81 to 86 centimeters (32 to 34 inches); yellowish brown (10YR 5/8) highly fractured weathered dolostone.\nR--86 centimeters (34 inches); hard level bedded dolostone bedrock."
},
"TYPE LOCATION": {
"section": "TYPE LOCATION",
"content": "TYPE LOCATION: Baxter County, Arkansas; about 1 mile east of Mountain Home on Buzzard Roost Road and 1400 feet south. SE1/4SW1/4NW1/4 sec. 2, T. 19 N., R. 13 W."
"content": "TYPE LOCATION: Baxter County, Arkansas; about 1 mile east of Mountain Home on Buzzard Roost Road and 1,400 feet south. SE1/4 SW1/4 NW1/4 section 2, T. 19 N., R. 13 W."
},
"RANGE IN CHARACTERISTICS": {
"section": "RANGE IN CHARACTERISTICS",
"content": "RANGE IN CHARACTERISTICS: The solum thickness and depth to\nbedrock ranges from 24 to 40 inches.\nThe A1 horizon has hue of 10YR, value of 2 or 3, and chroma of 2,\nor value of 3, and chroma of 3. The A2 horizon has hue of 10YR, value of 4 or 5, and chroma of 2, 3, or 4. The A horizon is silt loam, silty clay loam or with cherty, very cherty or stony\ntextural modifiers. The reaction ranges from medium acid to\nneutral.\nThe B21t horizon has hue of 10YR or 2.5Y, value of 5, and chroma\nof 4 or 6, or value of 4, and chroma of 4. The reaction ranges\nfrom medium acid to neutral. Mottles are in shades of gray,\nbrown, or red. The B22t horizon has hue of 7.5YR, 10YR, or 2.5Y, value of 5, and chroma of 4 or 6 and mottled with hue of 10YR,\nvalue of 4, 6, or 7, and chroma of 1 or 2, or is mottled in shades\nof gray, brown, and red with no dominant color. The reaction\nranges from slightly acid to mildly alkaline. The B3 horizon,\nwhere present, has similar color and texture as the B22t horizon. The B horizon is clay or cherty clay with 0 to 20 percent\nfragments of chert, limestone, or shale.\nThe Cr horizon is highly fractured weathered dolomite, limestone,\nor shale of light gray to yellowish brown colors.\nThe underlying bedrock (R) is hard level bedded dolomite limetone\nor shale."
"content": "RANGE IN CHARACTERISTICS:\nSolum thickness and depth to bedrock: 61 to 102 centimeters\nA1 horizon\nHue: 10YR\nValue: 2 or 3\nChroma: 2 or 3\nTexture: silt loam, silty clay loam or with gravelly or very gravelly or stony analogues\nReaction: medium acid to neutral\nA2 horizon\nHue: 10YR\nValue: 4 or 5\nChroma: 2 to 4\nTexture: silt loam, silty clay loam or with gravelly or very gravelly or stony analogues\nReaction: medium acid to neutral\n2Bt1 horizon\nHue: 10YR or 2.5Y\nValue: 4 or 5\nChroma: 4 or 6\nTexture: clay or gravelly clay\nRock fragment content: 0 to 20 percent chert, limestone, or shale\nReaction: medium acid to neutral\nMottles: shades of gray, brown, or red\n2Bt2 horizon\nHue: 7.5YR, 10YR, or 2.5Y\nValue: 5\nChroma: 4 or 6\nTexture: clay or gravelly clay\nRock fragment content: 0 to 20 percent chert, limestone, or shale\nMottles: hue of 10YR, value of 4, 6, or 7, and chroma of 1 or 2, or is mottled in shades of gray, brown, and red with no dominant color\nReaction: slightly acid to mildly alkaline\nBC horizon (where present)\nHue: 7.5YR, 10YR, or 2.5Y\nValue: 5\nChroma: 4 or 6\nTexture: clay or gravelly clay\nRock fragment content: 0 to 20 percent chert, limestone, or shale\nMottles: hue of 10YR, value of 4, 6, or 7, and chroma of 1 or 2, or is mottled in shades of gray, brown, and red with no dominant color\nReaction: slightly acid to mildly alkaline\nCr horizon\nNote: highly fractured weathered dolostone, limestone, or shale of light gray to yellowish brown colors.\nR horizon\nNote: hard level bedded dolostone limestone or shale."
},
"COMPETING SERIES": {
"section": "COMPETING SERIES",
"content": "COMPETING SERIES: Ventris is the only series in this family.\nSeries with common limits in definition are Cadeville, Homa, Invershiel, Marion, Orange, and Wister series. Cadeville, Invershiel, Orange, and Wister soils have less than 60 percent\nclay in the control section and are thermic. Homa soils are\nsimilar in texture but are thermic. Marion soils have less than\n60 percent clay in the control section."
"content": "COMPETING SERIES: Ventris is the only series in this family. Series with common limits in definition are Cadeville, Homa, Invershiel, Marion, Orange, and Wister series. Cadeville, Invershiel, Orange, and Wister soils have less than 60 percent clay in the control section and are thermic. Homa soils are similar in texture but are thermic. Marion soils have less than 60 percent clay in the control section."
},
"GEOGRAPHIC SETTING": {
"section": "GEOGRAPHIC SETTING",
"content": "GEOGRAPHIC SETTING: Ventris soils are on broad gently sloping uplands, side slopes, and on foot slopes of hills and mountains. Slopes range from 3 to 40 percent. They formed in residual\nmaterial weathered from dolomite, limestones, and calcareous\nshales of the Ozarks Highlands."
"content": "GEOGRAPHIC SETTING: Ventris soils are on broad gently sloping uplands, side slopes, and on foot slopes of hills and mountains. Slopes range from 3 to 40 percent. They formed in residual material weathered from dolomite, limestones, and calcareous shales of the Ozarks Highlands."
},
"GEOGRAPHICALLY ASSOCIATED SOILS": {
"section": "GEOGRAPHICALLY ASSOCIATED SOILS",
"content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are Arkana, Captina, Clarksville, Doniphan, Gassville, and Moko series. Arkana soils\nhave thicker mollic surface layers, dominant B horizon colors of\n5YR and on similar landscapes and steeper side slopes. Captina\nsoils have a fine-silty control section, a fragipan, and are\nadjacent similar landscapes. Doniphan soils are deeper than 40 inches to bedrock, have redder B horizons, low base saturation in\nthe lower solum and on similar landscapes. Gassville soils have redder B horizons, low base saturation in the lower solum and\nmostly on steeper side slopes. Moko soils are shallow to bedrock, have a loamy-skeletal control section, and on similar landscapes."
"content": "GEOGRAPHICALLY ASSOCIATED SOILS: These are Arkana, Captina, Clarksville, Doniphan, Gassville, and Moko series. Arkana soils have thicker mollic surface layers, dominant B horizon colors of 5YR and on similar landscapes and steeper side slopes. Captina soils have a fine-silty control section, a fragipan, and are adjacent similar landscapes. Doniphan soils are deeper than 10 centimeters to bedrock, have redder B horizons, low base saturation in the lower solum and on similar landscapes. Gassville soils have redder B horizons, low base saturation in the lower solum and mostly on steeper side slopes. Moko soils are shallow to bedrock, have a loamy-skeletal control section, and on similar landscapes."
},
"DRAINAGE AND PERMEABILITY": {
"section": "DRAINAGE AND PERMEABILITY",
"content": "DRAINAGE AND PERMEABILITY: Moderately well drained; medium to\nrapid runoff; very slow permeability."
"section": "DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY",
"content": "DRAINAGE AND SATURATED HYDRAULIC CONDUCTIVITY: Moderately well drained; medium to rapid runoff; moderately low saturated hydraulic conductivity class; very slow permeability class."
},
"USE AND VEGETATION": {
"section": "USE AND VEGETATION",
"content": "USE AND VEGETATION: Some areas are used for pasture and hay.\nMost areas are in forests of redcedar, blackjack oak, post oak,\nand elm the native vegetation."
"content": "USE AND VEGETATION: Some areas are used for pasture and hay. Most areas are in forests of redcedar, blackjack oak, post oak, and elm the native vegetation."
},
"DISTRIBUTION AND EXTENT": {
"section": "DISTRIBUTION AND EXTENT",
"content": "DISTRIBUTION AND EXTENT: Arkansas, Missouri, and possibly\nTennessee. The series is moderately extensive."
"content": "DISTRIBUTION AND EXTENT: Ozark Highland (MLRA 116A) of Arkansas and Missouri. The series is of moderate extent."
},
"REGIONAL OFFICE": {
"section": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE",
"content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Morgantown, West Virginia"
"content": "MLRA SOIL SURVEY REGIONAL OFFICE (MO) RESPONSIBLE: Salina, Kansas"
},
"ORIGIN": {
"section": "SERIES ESTABLISHED",
"content": "SERIES ESTABLISHED: Benton County, Arkansas; 1973."
},
"REMARKS": {
"section": "REMARKS",
"content": "REMARKS: The Ventris series would have been classified in the Red-Yellow Podzolic great soil group. These soils were mapped\nunder the field name of Colbert. Change in classification based\non University of Arkansas Soils Laboratory Data from Baxter\nCounty, Benton County, and Lawrence County, Arkansas."
"content": "REMARKS: Diagnostic horizons and features recognized in this pedon are:\nOchric epipedon--the zone from 0 to 13 centimeters (A horizons)\nArgillic horizon--the zone from 13 to 81 centimeters (Bt horizons)\nParalithic material--the zone from 81 to 86 centimeters (Cr horizon)\nLithic contact--dolostone at 86 centimeters\nThe Ventris series would have been classified in the Red-Yellow Podzolic great soil group. These soils were mapped under the field name of Colbert. Change in classification based on University of Arkansas Soils Laboratory Data from Baxter County, Benton County, and Lawrence County, Arkansas."
},
"ADDITIONAL DATA": {
"section": "ADDITIONAL DATA",
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"eff_class": "NA",
"distinctness": "abrupt",
"topography": "smooth",
"narrative": "A1--0 to 2 inches; very dark grayish brown (10YR 3/2) cherty silt loam; moderate medium granular structure; friable; many fine roots; 15 percent fragments of chert; neutral; abrupt smooth boundary. (1 to 6 inches thick)"
"narrative": "A1--0 to 5 centimeters (0 to 2 inches); very dark grayish brown (10YR 3/2) cherty silt loam; moderate medium granular structure; friable; many fine roots; 15 percent fragments of chert; neutral; abrupt smooth boundary. (3 to 15 centimeters thick)"
},
{
"name": "A2",
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"moist_value": 5,
"moist_chroma": 3,
"texture_class": "silt loam",
"structure": "NA",
"structure": "weak fine subangular blocky",
"dry_rupture": "NA",
"moist_rupture": "NA",
"moist_rupture": "friable",
"coherence": "NA",
"cf_class": "NA",
"pH": "NA",
"pH_class": "NA",
"pH_class": "slightly acid",
"eff_class": "NA",
"distinctness": "NA",
"topography": "NA",
"narrative": "A2--2 to 5 inches; brown (10YR 5/3) cherty silt loam; weak"
"distinctness": "abrupt",
"topography": "smooth",
"narrative": "A2--5 to 13 centimeters (2 to 5 inches); brown (10YR 5/3) cherty silt loam; weak fine subangular blocky structure; friable; many fine roots; approximately 15 percent fragments of chert; slightly acid; abrupt smooth boundary. (0 to 13 centimeters thick)"
},
{
"name": "B21t",
"name": "2Bt1",
"top": 13,
"bottom": 41,
"dry_hue": "NA",
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"moist_value": 5,
"moist_chroma": 4,
"texture_class": "clay",
"structure": "NA",
"structure": "moderate medium angular blocky",
"dry_rupture": "NA",
"moist_rupture": "NA",
"moist_rupture": "firm",
"coherence": "NA",
"cf_class": "NA",
"pH": "NA",
"pH_class": "NA",
"pH_class": "slightly acid",
"eff_class": "NA",
"distinctness": "NA",
"topography": "NA",
"narrative": "B21t--5 to 16 inches; yellowish brown (10YR 5/4) clay; common medium distinct light brownish gray (10YR 6/2) and reddish brown"
"distinctness": "gradual",
"topography": "smooth",
"narrative": "2Bt1--13 to 41 centimeters (5 to 16 inches); yellowish brown (10YR 5/4) clay; common medium distinct light brownish gray (10YR 6/2) and reddish brown (5YR 4/4) mottles; moderate medium angular blocky structure; very firm; few fine roots; common fine pores; thin continuous clay films on faces of peds and in pores; slightly acid; gradual smooth boundary. (15 to 38 centimeters thick)"
},
{
"name": "B22t",
"name": "2Bt2",
"top": 41,
"bottom": 81,
"dry_hue": "NA",
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"moist_value": 5,
"moist_chroma": 6,
"texture_class": "clay",
"structure": "NA",
"structure": "moderate fine angular blocky",
"dry_rupture": "NA",
"moist_rupture": "NA",
"moist_rupture": "firm",
"coherence": "NA",
"cf_class": "NA",
"pH": "NA",
"pH_class": "NA",
"pH_class": "neutral",
"eff_class": "NA",
"distinctness": "NA",
"topography": "NA",
"narrative": "B22t--16 to 32 inches; yellowish brown (10YR 5/6) clay;"
"distinctness": "abrupt",
"topography": "wavy",
"narrative": "2Bt2--41 to 81 centimeters (16 to 32 inches); yellowish brown (10YR 5/6) clay; common medium distinct gray (10YR 6/1) mottles; moderate fine angular blocky structure; very firm; few fine roots; few fine tubular pores; thin continuous clay films on faces of peds and in pores; 15 percent fragments of limestone; common slickensides; neutral; abrupt wavy boundary. (30 to 46 centimeters thick)"
},
{
"name": "Cr",
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"eff_class": "NA",
"distinctness": "NA",
"topography": "NA",
"narrative": "Cr--32 to 34 inches; yellowish brown (10YR 5/8) highly"
"narrative": "Cr--81 to 86 centimeters (32 to 34 inches); yellowish brown (10YR 5/8) highly fractured weathered dolostone."
},
{
"name": "R",
"top": 86,
"bottom": "NA",
"dry_hue": "NA",
"dry_value": "NA",
"dry_chroma": "NA",
"moist_hue": "NA",
"moist_value": "NA",
"moist_chroma": "NA",
"texture_class": "NA",
"structure": "NA",
"dry_rupture": "hard",
"moist_rupture": "NA",
"coherence": "NA",
"cf_class": "NA",
"pH": "NA",
"pH_class": "NA",
"eff_class": "NA",
"distinctness": "NA",
"topography": "NA",
"narrative": "R--86 centimeters (34 inches); hard level bedded dolostone bedrock."
}
]
]
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