Official Series Description


Lab Data Summary

Aggregate lab data for the KOBASE soil series. This aggregation is based on all pedons with a current taxon name of KOBASE, 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 KOBASE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KOBASE 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 KOBASE 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 KOBASE 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 KOBASE 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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There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with KOBASE 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 KOBASE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the KOBASE 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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There are insufficient data to create the 3D mountains figure.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with KOBASE, 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

No block diagrams are available.

Map Units

Map units containing KOBASE 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
Kobase silty clay loam, moist, 3 to 8 percent slopes4812381496999jp57co68519791:24000
Kobase silty clay loam, moist, 0 to 3 percent slopes473233496998jp56co68519791:24000
Kobase silty clay loam, moist, 8 to 15 percent slopes492482497000jp58co68519791:24000
Kobase silty clay loam, warm, 2 to 8 percent slopes78C68993432382wby4mt01119921:24000
Kobase silty clay loam, 0 to 2 percent slopes78A1262343237cj55mt01119921:24000
Kobase silty clay loam, warm, 2 to 8 percent slopes53C217553435302wby4mt01719951:24000
Kobase silty clay loam, 0 to 2 percent slopes53A12958343529cjglmt01719951:24000
Kobase-Gerdrum silty clay loams, 2 to 8 percent slopes532C11162343524cjgfmt01719951:24000
Kobase silty clay loam, 2 to 15 percent slopes, gullied531D6620343523cjgdmt01719951:24000
Kobase silty clay loam, 8 to 15 percent slopes53D3269343531cjgnmt01719951:24000
Delpoint-Kobase-Yawdim complex, 4 to 15 percent slopes388D1108343426cjc8mt01719951:24000
Kobase-Cabbart-Yawdim complex, 8 to 25 percent slopes944E818343766cjq7mt01719951:24000
Abor-Delpoint-Kobase complex, 4 to 15 percent slopes958D2823437982zzrmmt01719951:24000
Yawdim-Cabbart-Kobase complex, 15 to 70 percent slopes956F188343794cjr4mt01719951:24000
Gerdrum-Kobase silty clay loams, 2 to 8 percent slopes941C159343760cjq1mt01719951:24000
Kobase silty clay loam, warm, 2 to 8 percent slopes78C18243422872wby4mt02519911:24000
Kobase silty clay loam, 2 to 8 percent slopes141118683423702wby5mt02719791:24000
Yamacall-Rock outcrop, soft-Kobase association, 8 to 70 percent slopes1002F81670342609chhxmt03320021:24000
Kobase silty clay loam, 0 to 4 percent slopes66B45645342679chl5mt03320021:24000
Kobase silty clay loam, warm, 2 to 8 percent slopes66C239153426802wby4mt03320021:24000
Kobase-Sonnett, thin surface, silty clay loams, 2 to 8 percent slopes661C21989342678chl4mt03320021:24000
Kobase silty clay loam, 8 to 15 percent slopes66D1049342681chl7mt03320021:24000
Gerdrum-Kobase silty clay loams, 0 to 2 percent slopes554A928342783chpjmt03320021:24000
Gerdrum-Kobase silty clay loams, 2 to 8 percent slopes554C846342784chpkmt03320021:24000
Yawdim-Cabbart-Kobase complex, 15 to 70 percent slopes991F630342796chpymt03320021:24000
Kobase clay loam, 0 to 2 percent slopes32A5133343906cjvrmt04119941:24000
Kobase clay loam, calcareous, 0 to 2 percent slopes321A1987343905cjvqmt04119941:24000
Kobase silty clay loam, 0 to 4 percent slopes32B20886344181ck4mmt05119921:24000
Ethridge-Kobase complex, 0 to 4 percent slopes385B11949344195ck52mt05119921:24000
Kobase silty clay loam, calcareous, 0 to 4 percent321B11000344176ck4gmt05119921:24000
Marias-Kobase complex, 0 to 4 percent slopes471B4656344211ck5lmt05119921:24000
Kobase silty clay loam, 4 to 8 percent slopes32C1299344182ck4nmt05119921:24000
Kobase silty clay loam, calcareous, 4 to 8 percent321C527344177ck4hmt05119921:24000
Kobase silty clay loam, 2 to 8 percent slopes40B115073445832wby5mt06519961:24000
Kobase-Zatoville silty clay loams, 1 to 8 percent slopes38A7262344577cgk0mt06519961:24000
Kobase silty clay loam, calcareous surface, 1 to 8 percent slopes40C4240344584cgk5mt06519961:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B4236344478cghrmt06519961:24000
Kobase-Megonot silty clay loams, calcareous, 1 to 8 percent slopes140C559344479cghsmt06519961:24000
Abor-Delpoint-Kobase complex, 4 to 15 percent slopes243303448342zzrmmt07919861:24000
Kobase silty clay loam, warm, 2 to 8 percent slopes7430243450052wby4mt07919861:24000
Kobase silty clay loam, 0 to 2 percent slopes731979345001cl02mt07919861:24000
Kobar-Gerdrum silty clay loams, 2 to 8 percent slopes751290345008cl09mt07919861:24000
Kobase silty clay loam, calcareous, 0 to 4 percent slopes321B7817345125cl42mt10119921:24000
Kobase silty clay loam, 0 to 4 percent slopes32B4994345128cl45mt10119921:24000
Kobase silty clay loam, calcareous, 4 to 8 percent slopes321C3741345126cl43mt10119921:24000
Kobase silty clay loam, 4 to 8 percent slopes32C1618345129cl46mt10119921:24000
Ethridge-Kobase silty clay loams, 0 to 4 percent slopes385B30558346745cmtbmt61519921:24000
Kobase silty clay loam, 0 to 4 percent slopes32B16676346691cmrlmt61519921:24000
Marias-Kobase complex, 0 to 4 percent slopes471B14309346790cmvsmt61519921:24000
Kobase silty clay loam, 4 to 8 percent slopes32C58763040357cmrmmt61519921:24000
Megonot-Kobase-Delpoint complex, 2 to 8 percent slopes142C2512346601cmnpmt61519921:24000
Kobase silty clay loam, 2 to 8 percent slopes032C13853466922wby5mt61519921:24000
Kobase silty clay loam, 8 to 15 percent slopes32D1333346693cmrnmt61519921:24000
Kobase-Megonot complex, calcareous, 0 to 8 percent slopes140C3524347251cnbnmt62420211:24000
Zatoville-Kobase complex, 2 to 8 percent slopes234C3156347382cngwmt62420211:24000
Kobase clay loam, 2 to 8 percent slopes150C2201347266cnc4mt62420211:24000
Zatoville-Kobase complex, 2 to 8 percent slopes, fan475C128619143392280wmt62420211:24000
Kobase-Megonot complex, calcareous, 0 to 8 percent slopes, fan474C110619126322267tmt62420211:24000
Kobase clay loam, calcareous surface, 0 to 4 percent slopes471C96519124092260mmt62420211:24000
Kobase-Harlake, rarely flooded-Lostriver, rarely flooded complex, 0 to 4 percent slopes807B49923844742l17jmt62420211:24000
Kobase clay loam, 2 to 8 percent slopes, fan472C3621912710226bbmt62420211:24000
Kobase-Megonot complex, 0 to 8 percent slopes473C23119126312267smt62420211:24000
Kobase-Zatoville silty clay loams, 1 to 8 percent slopes38A642513972cgk0mt62420211:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B332513995cghrmt62420211:24000
Kobase silty clay loam, 2 to 8 percent slopes40B131768462wby5mt62420211:24000
Kobase silty clay loam, calcareous surface, 1 to 8 percent slopes40C12513975cgk5mt62420211:24000
Kobase silty clay, 0 to 2 percent slopes130A4921476954ypcmt63019911:24000
Cabbart-Megonot-Kobase clay loams, 2 to 15 percent slopes138D657514965050qfmt63920001:24000
Kobase clay loam, 2 to 8 percent slopes150C524414967350r5mt63920001:24000
Kobase-Rentsac-Megonot complex, 4 to 25 percent slopes363E10481499215105mt63920001:24000
Kobase clay loam, 8 to 15 percent slopes150D42914967450r6mt63920001:24000
Kobase silty clay loam, 0 to 4 percent slopes32B14528347673cns8mt64119941:24000
Kobase-Megonot silty clay loams, 2 to 8 percent slopes322C1882347671cns6mt64119941:24000
Kobase silty clay, 0 to 2 percent slopes320A1450347669cns4mt64119941:24000
Kobase-Marvan-Weingart complex, 0 to 4 percent slopes323B904347672cns7mt64119941:24000
Megonot-Kobase silty clay loams, 8 to 15 percent slopes96D741347821cny1mt64119941:24000
Kobase silty clay loam, warm, 2 to 8 percent slopes110300663479322wby4mt64919851:24000
Gerdrum-Kobar silty clay loams, 2 to 8 percent slopes919957348127cp7xmt64919851:24000
Yawdim-Cabbart-Kobar complex, 15 to 70 percent slopes2126390348045cp58mt64919851:24000
Gerdrum-Kobar silty clay loams, 0 to 2 percent slopes901456348126cp7wmt64919851:24000
Kobase silty clay loam, 2 to 8 percent slopes40B13717125832wby5mt65519751:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B7517125631vh1zmt65519751:24000
Kobase-Gullied land complex, 2 to 8 percent slopes640B2217179631vnp5mt65519751:24000
Cabbart-Megonot-Kobase clay loams, 2 to 15 percent slopes138D20361416d42lmt65519751:24000
Kobase-Marias complex, 0 to 4 percent slopes240B19002348483cpmdmt65719901:24000
Kobase silty clay loam, 0 to 4 percent slopes40B13866348635cps9mt65719901:24000
Kobase-Ethridge clay loams, 4 to 8 percent slopes541C9862348714cpvvmt65719901:24000
Megonot-Kobase-Yawdim complex, 8 to 15 percent slopes570D6381348724cpw5mt65719901:24000
Kobase silty clay loam, 4 to 8 percent slopes40C3370348636cpsbmt65719901:24000
Kobase silty clay loam, 2 to 8 percent slopes40B125243416862wby5mt66620081:24000
Kobase-Zatoville silty clay loams, 1 to 8 percent slopes38A12077341682cgk0mt66620081:24000
Kobase-Megonot silty clay loams, 1 to 8 percent slopes140B7633341643cghrmt66620081:24000
Kobase silty clay loam, calcareous surface, 1 to 8 percent slopes40C4751341687cgk5mt66620081:24000
Kobase-Megonot silty clay loams, calcareous, 1 to 8 percent slopes140C2849341644cghsmt66620081:24000
Kobase-Gullied land complex, 2 to 8 percent slopes640B32517175701vn8hmt66620081:24000
Cabbart-Megonot-Kobase complex, 2 to 15 percent slopes138D215385691nn08mt66620081:24000
Kobase-Rentsac-Megonot complex, 4 to 25 percent slopes363E86620223ntd6mt6691:24000

Map of Series Extent

Approximate geographic distribution of the KOBASE 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 .