Official Series Description


Lab Data Summary

Aggregate lab data for the BUNKUM soil series. This aggregation is based on all pedons with a current taxon name of BUNKUM, 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 BUNKUM 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
114B94P0273S1993IL163015Bunkum6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4117203,-90.0048141
114B13N0527S2012IL083001Bunkum6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.103725,-90.3471611

Water Balance

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

Soil series sharing subgroup-level classification with BUNKUM, 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 BUNKUM 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
Bunkum silt loam, 5 to 10 percent slopes, eroded515C21417023786262tbs3il00119971:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C31038423786272tbs5il00119971:12000
Bunkum silt loam, 10 to 18 percent slopes, eroded515D2524123786282kv4yil00119971:12000
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D3308623786292kv4zil00119971:12000
Bunkum silt loam, 2 to 5 percent slopes, eroded515B282523786252kv4vil00119971:12000
Bunkum-Atlas silt loams, 5 to 10 percent slopes, eroded897C250002617378sc4il02119991:12000
Bunkum-Atlas silty clay loams, 5 to 10 percent slopes, severely eroded897C31572617388sc5il02119991:12000
Bunkum silt loam, 5 to 10 percent slopes, eroded515C22525422482tbs3il06119681:15840
Bunkum-Atlas silt loams, 10 to 18 percent slopes, eroded897D2325422592qxs2il06119681:15840
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D37115408612tbrxil07720061:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C32515408602tbs5il07720061:12000
Bunkum silt loam, 5 to 10 percent slopes, eroded515C238997284512tbs3il08320021:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C322957284532tbs5il08320021:12000
Bunkum silt loam, 2 to 5 percent slopes, eroded515B21677728450sg0dil08320021:12000
Bunkum-Atlas silt loams, 5 to 10 percent slopes, eroded897C21728452sg0gil08320021:12000
Bunkum-Atlas silt loams, 5 to 10 percent slopes, eroded897C2114431992406pb3il11719991:12000
Bunkum-Atlas silt loams, 10 to 18 percent slopes, eroded897D259291992426pb5il11719991:12000
Bunkum-Atlas silty clay loams, 5 to 10 percent slopes, severely eroded897C38971992416pb4il11719991:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C371992322tbs5il11719991:12000
Bunkum-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded897D371991536p79il11719991:12000
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D351992332tbrxil11719991:12000
Bunkum silty clay loam, 2 to 5 percent slopes, severely eroded515B311992516pbgil11719991:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C377211989702tbs5il11920011:12000
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D323901989692tbrxil11920011:12000
Bunkum silty clay loam, 2 to 5 percent slopes, severely eroded515B321831989716p1fil11920011:12000
Bunkum-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded897D38761989756p1kil11920011:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C3128641840972tbs5il13319981:12000
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D3113171840982tbrxil13319981:12000
Bunkum-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded897D3245718415665mjil13319981:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B2128618415265mdil13319981:12000
Bunkum-Coulterville silty clay loams, 5 to 10 percent slopes, severely eroded884C3128218415365mfil13319981:12000
Bunkum-Atlas silt loams, 5 to 10 percent slopes, eroded897C2534717215341vsdcil13520071:12000
Bunkum silt loam, 5 to 10 percent slopes, eroded515C2368717215212tbs3il13520071:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C364917215232tbs5il13520071:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C34914592602tbs5il14520051:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B21614592571kzgtil14520051:12000
Bunkum silt loam, 5 to 10 percent slopes, eroded515C215202010752tbs3il14920011:12000
Bunkum silt loam, 10 to 18 percent slopes, eroded515D25862010776r7cil14920011:12000
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D34812010806r7gil14920011:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C33052010736r77il14920011:12000
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D3127302004932tbrxil15720011:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C3114162004962tbs5il15720011:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B284892005376qnyil15720011:12000
Bunkum silt loam, 5 to 10 percent slopes, eroded515C273352004976qmnil15720011:12000
Bunkum-Coulterville silty clay loams, 5 to 10 percent slopes, severely eroded884C325792005366qnxil15720011:12000
Bunkum-Coulterville silty clay loams, 10 to 18 percent slopes, severely eroded884D323232005356qnwil15720011:12000
Bunkum silt loam, 10 to 18 percent slopes515D2196600715n52xil15720011:12000
Bunkum silt loam, 10 to 18 percent slopes, eroded515D29322004946qmkil15720011:12000
Bunkum-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded897D34032005326qnsil15720011:12000
Bunkum-Coulterville silty clay loams, 5 to 10 percent slopes, severely eroded884C31198818317364ltil16319971:12000
Bunkum-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded897D3703618317864lzil16319971:12000
Bunkum silty clay loam, 10 to 18 percent slopes, severely eroded515D342191830732tbrxil16319971:12000
Bunkum silty clay loam, 5 to 10 percent slopes, severely eroded515C316581830722tbs5il16319971:12000
Bunkum silt loam, 5 to 10 percent slopes, eroded515C236118307164hjil16319971:12000
Bunkum-Coulterville silt loams, 2 to 5 percent slopes, eroded884B27815425071ns39il18920061:12000

Map of Series Extent

Approximate geographic distribution of the BUNKUM 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 .