Merge 41ae005 into 8238419

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",

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",

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",

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",