Official Series Description


Lab Data Summary

Aggregate lab data for the DIABLO soil series. This aggregation is based on all pedons with a current taxon name of DIABLO, and applied along 1-cm thick depth slices. Solid lines are the slice-wise median, bounded on either side by the interval defined by the slice-wise 5th and 95th percentiles. The median is the value that splits the data in half. Five percent of the data are less than the 5th percentile, and five percent of the data are greater than the 95th percentile. Values along the right hand side y-axis describe the proportion of pedon data that contribute to aggregate values at this depth. For example, a value of "90%" at 25cm means that 90% of the pedons correlated to DIABLO were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

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Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
1440A3096S1961CA097011Diablo5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2852783,-122.6063919
1440A3097S1961CA097012Diablo5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2811127,-122.5908356
1593P066193CA079001Diablo8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3443056,-120.7421389
1593P066293CA079001ADiablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3443056,-120.7421389
1593P066393CA079001BDiablo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3443056,-120.7421389
1593P066493CA079001CDiablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3443056,-120.7421389
1593P066593CA079001DDiablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3443056,-120.7421389
1593P066693CA079002Diablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3295556,-120.697
1593P066793CA079002ADiablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3295556,-120.697
1593P066893CA079002BDiablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3295556,-120.697
1593P066993CA079002CDiablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3295556,-120.697
1593P067093CA079002DDiablo6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.3295556,-120.697
1540A3094S1958CA001001DIABLO5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7244453,-121.8183365
1540A3095S1958CA001002DIABLO5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7491684,-121.8177795
1540A3098S1965CA053010Diablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1622238,-120.9300003
1513N4945S2012CA079002Diablo7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.36761,-120.82006
n/a40A3089S1955CA079002DIABLO3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DIABLO soil series. Monthly precipitation (PPT) and potential evapotranspiration (PET) have been estimated from the 50th percentile of gridded values (PRISM 1981-2010) overlapping with the extent of SSURGO map units containing each series as a major component. Monthly PET values were estimated using the method of Thornthwaite (1948). These (and other) climatic parameters are calculated with each SSURGO refresh and provided by the fetchOSD function of the soilDB package. Representative water storage values (“AWC” in the figures) were derived from SSURGO by taking the 50th percentile of profile-total water storage (sum[awc_r * horizon thickness]) for each soil series. Note that this representation of “water storage” is based on the average ability of most plants to extract soil water between 15 bar (“permanent wilting point”) and 1/3 bar (“field capacity”) matric potential. Soil moisture state can be roughly interpreted as “dry” when storage is depleted, “moist” when storage is between 0mm and AWC, and “wet” when there is a surplus. Clearly there are a lot of assumptions baked into this kind of monthly water balance. This is still a work in progress.

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Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the DIABLO series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

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Select annual climate data summaries for the DIABLO series and siblings. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the DIABLO series and siblings. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. Proportions can be interpreted as an aggregate representation of geomorphic membership. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Small Shannon entropy values suggest relatively consistent geomorphic association, while larger values suggest lack thereof. Source: SSURGO component records .

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Competing Series

Soil series competing with DIABLO share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

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Select annual climate data summaries for the DIABLO series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

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Geomorphic description summaries for the DIABLO series and competing. Series are sorted according to hierarchical clustering of proportions and relative hydrologic position within an idealized landform (e.g. top to bottom). Proportions can be interpreted as an aggregate representation of geomorphic membership. Most soil series (SSURGO components) are associated with a hillslope position and one or more landform-specific positions: hills, mountain slopes, terraces, and/or flats. The values printed to the left (number of component records) and right (Shannon entropy) of stacked bars can be used to judge the reliability of trends. Shannon entropy values close to 0 represent soil series with relatively consistent geomorphic association, while values close to 1 suggest lack thereof. Source: SSURGO component records .

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Soil series sharing subgroup-level classification with DIABLO, arranged according to family differentiae. Hovering over a series name will print full classification and a small sketch from the OSD. Source: snapshot of SC database .

Block Diagrams

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. CA-2012-05-08-17 | Alameda Area - March 1966

    The relationship of geologic formations, landforms, and soil series in the Alameda Area (Soil Survey of Alameda Area, California; March, 1966).

Map Units

Map units containing DIABLO as a major component. Limited to 250 records.

Map Unit Name Symbol Map Unit Area (ac) Map Unit Key National Map Unit Symbol Soil Survey Area Publication Date Map Scale
Diablo clay, 15 to 30 percent slopes, MLRA 15DdE163054557882w60pca01319731:24000
Diablo clay, 30 to 50 percent slopes, MLRA 15DdF151454557892w637ca01319731:24000
Diablo clay, 5 to 25 percent slopes, MLRA 15DdD29754557872w63gca01319731:24000
Cut and fill land-Diablo complex, 9 to 30 percent slopesCmE1250455782h98nca01319731:24000
Diablo clay, 30 to 45 percent slopes, erodedDbE2aa3843727x9z0ca01319731:24000
Diablo clay, 7 to 15 percent slopesDbCaa1843725x9yyca01319731:24000
Linne-Diablo complex, 15 to 30 percent slopesLbE6025455634h93wca05319721:24000
San Benito-Diablo complex, 30 to 50 percent slopes, MLRA 15SdF45204557152wv88ca05319721:24000
Diablo clay, 15 to 30 percent slopes, MLRA 15DbE39604555842w60pca05319721:24000
Santa Ynez fine sandy loam, 9 to 15 percent slopesShD3410455723h96rca05319721:24000
Diablo clay, 5 to 25 percent slopes, MLRA 15DbD33504555832w63gca05319721:24000
Linne-Diablo complex, 9 to 15 percent slopesLbD28754556332x52rca05319721:24000
Diablo clay, 30 to 50 percent slopes, MLRA 15DbF26104555852w637ca05319721:24000
Diablo clay, 15 to 30 percent slopes128830458952hdkxca05519741:24000
Diablo clay, 30 to 50 percent slopes, MLRA 151296954589532w637ca05519741:24000
Diablo clay, 9 to 15 percent slopes, MLRA 151275454589512w63dca05519741:24000
Diablo clay, 5 to 9 percent slopes, MLRA 151264254589502w63cca05519741:24000
Altamont-Diablo clays, 9 to 30 percent slopesAmE2so2816079wd64ca05519741:24000
Diablo clay, 30 to 50 percent slopes, eroded, MLRA 15DaF2194924561862w639ca06919651:20000
Diablo clay, 15 to 30 percent slopes, eroded, MLRA 15DaE2138574561852w60rca06919651:20000
Diablo clay, 9 to 15 percent slopes, MLRA 15DaD32624561842w63dca06919651:20000
Diablo clay, 50 to 75 percent slopes, severely erodedDaG32222456187h9pqca06919651:20000
Diablo-Linne complex, 15 to 30 percent slopes, erodedDlE21544456189h9psca06919651:20000
Diablo-Linne complex, 9 to 15 percent slopesDlD1227456188h9prca06919651:20000
Diablo-Linne complex, 30 to 50 percent slopes, erodedDlF2613456190h9ptca06919651:20000
Diablo clay, 15 to 30 percent slopes, MLRA 1512711514559032w60pca08719761:24000
Diablo clay, 5 to 25 percent slopes, MLRA 151263744559022w63gca08719761:24000
Diablo-Ayar clays, 9 to 30 percent slopes, erodedDaE220574456077h9l5ca09519691:24000
Altamont-Diablo clays, 2 to 9 percent slopesAmC8384456055h9kgca09519691:24000
Diablo-Ayar clays, 2 to 9 percent slopesDaC7485456076h9l4ca09519691:24000
Altamont-Diablo clays, 9 to 30 percent slopesAmE22725456056h9khca09519691:24000
Diablo clay, 15 to 30 percent slopes, MLRA 15DbE50604597072w60pca09719681:20000
Diablo clay, 9 to 15 percent slopes, MLRA 15DbD36344597062w63dca09719681:20000
Diablo clay, 2 to 9 percent slopesDbC3487459705hfc6ca09719681:20000
Diablo clay, 15 to 30 percent slopes, eroded, MLRA 15DbE224904597082w60rca09719681:20000
Diablo clay, 30 to 50 percent slopes, MLRA 15DbF8504597092w637ca09719681:20000
Diablo clay, 30 to 50 percent slopes, eroded, MLRA 15DbF22834597102w639ca09719681:20000
Diablo clay, 30 to 50 percent slopes, MLRA 15129n77655072w637ca11319681:20000
Diablo clay, 30 to 50 percent slopes, MLRA 15DdFcc8017092w637ca60919631:20000
Diablo clay, 9 to 15 percent slopesDdDcc801707vx7jca60919631:20000
Diablo clay, 9 to 15 percent slopes113aw801687vx6wca60919631:20000
Diablo clay, 30 to 45 percent slopes, erodedDbE27836456576hb38ca60919631:20000
Diablo clay, 15 to 30 percent slopes, MLRA 15DbD55654565752w60pca60919631:20000
Diablo clay, moderately deep, 45to 60 percent slopes, erodedDmF22983456577hb39ca60919631:20000
Diablo clay, very deep, 3 to 15 percent slopesDvC2462456578hb3bca60919631:20000
Diablo clay, very deep, 30 to 45 percent slopes, erodedDvE21648456580hb3dca60919631:20000
Diablo clay, very deep, 15 to 30 percent slopes, erodedDvD21588456579hb3cca60919631:20000
Diablo clay, very deep, 45 to 60 percent slopes, erodedDvF2383456581hb3fca60919631:20000
Diablo clay, 7 to 15 percent slopesDbC141456574hb36ca60919631:20000
Diablo clay, very deep, 3 to 15 percent slopesDvCaa801696vx75ca61019751:24000
Diablo clay, 9 to 15 percent slopes, MLRA 1511311674566662w63dca61019751:24000
Diablo clay, 15 to 30 percent slopes, MLRA 151142754566672w60pca61019751:24000
Diablo clay, 30 to 50 percent slopes, MLRA 15115884566682w637ca61019751:24000
Diablo clay, 9 to 15 percent slopes, warm MAATDaD106524567942w63fca63819671:24000
Diablo clay, 2 to 9 percent slopesDaC9063456793hbb8ca63819671:24000
Diablo clay, 15 to 30 percent slopesDaE7796456795hbbbca63819671:24000
Diablo-Olivenhain complex, 9 to 30 percent slopesDoE5197456800hbbhca63819671:24000
Diablo-Urban land complex, 5 to 15 percent slopesDcD4567456798hbbfca63819671:24000
Diablo clay, 15 to 30 percent slopes, eroded, warm MAATDaE224974567962w60sca63819671:24000
Diablo clay, 30 to 50 percent slopes, warm MAAT, MLRA 20DaF24694567972w638ca63819671:24000
Diablo-Urban land complex, 15 to 50 percent slopesDcF1717456799hbbgca63819671:24000
Diablo clay, 15 to 30 percent slopes, MLRA 15310118318829212w60pca64120091:24000
Diablo-Urbanland complex, 9 to 15 percent slopes31273724259002mfbvca64120091:24000
Diablo-Urbanland complex, 15 to 30 percent slopes31351824259012mfbwca64120091:24000
Diablo clay, 30 to 50 percent slopes, MLRA 153116418829202w637ca64120091:24000
Diablo clay, 5 to 25 percent slopes, MLRA 154002624354662w63gca64120091:24000
Diablo clay, 9 to 15 percent slopesDaD206456983hbjdca64619671:24000
Diablo clay, 30 to 50 percent slopes, MLRA 15DaF1394569842w637ca64619671:24000
Diablo-Lodo complex, 15 to 50 percent slopes13318285457105hbnbca66419771:24000
Diablo and Cibo clays, 30 to 50 percent slopes13214320457104hbn9ca66419771:24000
Diablo and Cibo clays, 15 to 30 percent slopes13112990457103hbn8ca66419771:24000
Los Osos-Diablo complex, 30 to 50 percent slopes16512325457137hbpcca66419771:24000
Diablo and Cibo clays, 9 to 15 percent slopes1306960457102hbn7ca66419771:24000
Los Osos-Diablo complex, 15 to 30 percent slopes1646485457136hbpbca66419771:24000
Diablo clay, 5 to 9 percent slopes, MLRA 1512961504571012w63cca66419771:24000
Los Osos-Diablo complex, 9 to 15 percent slopes1634770457135hbp9ca66419771:24000
Los Osos-Diablo complex, 5 to 9 percent slopes1622355457134hbp8ca66419771:24000
Ayar and Diablo soils, 15 to 30 percent slopes1108525457213hbrtca66519771:24000
Ayar and Diablo soils, 9 to 15 percent slopes1095610457212hbrsca66519771:24000
Ayar and Diablo soils, 30 to 50 percent slopes1112530457214hbrvca66519771:24000
Linne-Diablo complex, 9 to 15 percent slopes1557904572582x52rca66519771:24000
Diablo silty clay, 30 to 45 percent slopesDaF4117457386hbydca67219661:20000
Diablo silty clay, 15 to 30 percent slopesDaE197633563752zwt7ca67219661:20000
San Benito-Diablo complex, 45 to 75 percent slopesSgG1247457489hc1qca67219661:20000
Diablo silty clay, 9 to 15 percent slopesDaD941457384hbybca67219661:20000
San Benito-Diablo complex, 30 to 45 percent slopesSgF915457488hc1pca67219661:20000
Diablo silty clay, 45 to 75 percent slopesDaG775457388hbygca67219661:20000
Diablo silty clay, 15 to 45 percent slopes, severely erodedDaF3302457387hbyfca67219661:20000
Diablo clay, 15 to 30 percent slopes, erodedDaE2171534228302zwttca67319741:24000
Diablo clay, 2 to 9 percent slopesDaC1293457589hc4yca67319741:24000
Diablo clay, 9 to 15 percent slopes, warm MAATDaD11334575902w63fca67319741:24000
Diablo clay, 30 to 50 percent slopes, longer FFSDaF27704575922w63bca67319741:24000
Diablo clay, 15 to 30 percent slopesDbE2188457692hc88ca67419681:24000
Diablo clay, 30 to 50 percent slopes, warm MAAT, MLRA 20DbF18274576932w638ca67419681:24000
Diablo clay, 9 to 15 percent slopes, warm MAATDbD13114576912w63fca67419681:24000
Diablo-Altamont-Henneke families association, 10 to 60 percent slopes515134465318hm68ca77219811:24000

Map of Series Extent

Approximate geographic distribution of the DIABLO soil series. To learn more about how this distribution was mapped, or to compare this soil series extent to others, use the Series Extent Explorer (SEE) application. Source: generalization of SSURGO geometry .