Official Series Description


Lab Data Summary

Aggregate lab data for the COMBS soil series. This aggregation is based on all pedons with a current taxon name of COMBS, 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 COMBS 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
120B93P0757S1993IN123012Combs6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9338875,-86.5077744
12298KY-111-00398KY111041Combs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1025,-85.8986111
12577KY-193-00677KY193 Combs-OSDCombs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3322792,-83.3565445
n/a81KY-189-00181KY-189-001Combs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98KY-111-00498KY-111-004Combs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98KY-111-00598KY-111-005Combs4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the COMBS 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 COMBS 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 COMBS 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 COMBS 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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Click the image to view it full size.

Click the image to view it full size.

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Competing Series

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

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the COMBS 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

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

Soil series sharing subgroup-level classification with COMBS, 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. KY-2012-02-01-37 | Pike County - June 1990

    Along the Levisa and Russell Forks of the Big Sandy River, the soils in the valleys are in the Nelse-Shelbiana-Udorthents general soil map unit and those on the mountains are in the Marrowbone-Fedscreek-Kimper-Dekalb map unit (Soil Survey of Pike County, Kentucky; June 1990).

Map Units

Map units containing COMBS 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
Combs loam, 0 to 2 percent slopes, frequently flooded, brief durationCndAH282535713kzg2in12319971:12000
Combs fine sandy loam, frequently flooded, brief durationCo26117182471vnzbin14719661:15840
Combs fine sandy loam, occasionally floodedCo20415330101ng6yky11120051:12000
Urban land-Haplic Udarents-Combs complex, 0 to 6 percent slopes, rarely floodedUacB8915364561nkt3ky11120051:12000
Combs silt loam, 0 to 4 percent slopes, occasionally floodeduComB37827382542ncv5ky19519861:24000
Huntington-Combs complex, 0 to 2 percent slopes, frequently floodedHm624915927531qgd4ky60219721:12000
Combs silt loam, 0 to 4 percent slopes, occasionally floodeduComB73127382672ncv5ky63319791:24000
Combs fine sandy loam, 0 to 3 percent slopes, occasionally floodedCoA74624011032lljymd00120091:12000
Combs silt loam, 0 to 3 percent slopesCnA2699534949kynfmd02120011:12000
Combs fine sandy loam, 0 to 3 percent slopesCmA361534795kyhgmd02120011:12000
Combs fine sandy loamCo1136534215kxwrmd04319981:12000
Combs silt loamCp1087534221kxwymd04319981:12000
Combs loam, rarely floodedCm177524770km22tn60620011:24000
Combs loam, rarely floodedCo1176529683ks5ktn60820011:24000
Combs loam, 0 to 3 percent slopes, frequently flooded9A14731367264l8jva00920041:24000
Combs fine sandy loam, 0 to 3 percent slopes, occasionally flooded10A1486517130kc3mva13919951:20000
Combs loam, 0 to 2 percent slopes, occasionally flooded8A1318520414kgjkva16119901:24000
Combs fine sandy loamCs899516225kb5fwv00319971:24000
Combs fine sandy loamCs115917109121vfbqwv0371:24000
Combs fine sandy loamCz1384555668ln6swv06520031:24000
Combs-Potomac complex, 0 to 3 percent slopes, very stony, occasionally floodedCpA29324851132pdyywv62220101:12000
Combs fine sandy loam, 0 to 3 percent slopes, occasionally floodedCoA19824851122pdyxwv62220101:12000
Combs fine sandy loam, 0 to 3 percent slopes, occasionally floodedCoA21224977552pdyxwv62320101:12000

Map of Series Extent

Approximate geographic distribution of the COMBS 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 .