Official Series Description


Lab Data Summary

Aggregate lab data for the BENTEEN soil series. This aggregation is based on all pedons with a current taxon name of BENTEEN, 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 BENTEEN 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 BENTEEN 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 BENTEEN 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 BENTEEN 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 BENTEEN 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 BENTEEN 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 BENTEEN 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 BENTEEN 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 BENTEEN, 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 BENTEEN 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
Benteen-Rock outcrop complex, 3 to 18 percent slopes53700496487jnmqco62719801:24000
Benteen loam, 15 to 40 percent slopes6962497886jq2vco64919771:24000
Benteen loam, 6 to 15 percent slopes5668497875jq2hco64919771:24000
Wesdy family-Lithic Cryorthents-Benteen family, association, 30 to 75 percent slopes406-BR3129842415366id7131:24000
Benteen-Levengood-Maciver families, complex, moderately steep mountain slopes534C516202405325y61id75819981:24000
Bridger-Benteen-Philipsburg families, complex, landslide deposits704E173331487594zspmt60520071:24000
Maciver-Prudy-Benteen families, complex, moderately steep mountain slopes534E151291486474zp2mt60520071:24000
Benteen-Levengood-Maciver families, complex, moderately steep mountain slopes534C45951486454zp0mt60520071:24000
Groomer-Foolhen, rarely flooded-Benteen families, complex, alluvial-colluvial deposits614G26951487244zrkmt60520071:24000
Levengood-Benteen-Wetopa families, complex, valley bottoms646G105614931850cqmt60520071:24000
Benteen loam, rollingBp5809345886clxmmt60719701:24000
Benteen loam, hillyBr1168345887clxnmt60719701:24000
Levengood-Benteen-Wetopa families, complex, valley bottoms646G4259777250cqmt61220111:24000
Levengood-Benteen-Wetopa families, complex, valley bottoms3053117101621vdkjmt63619831:24000
Starley-Benteen families complex, 3 to 15 percent slopes562A331289030gx4ut6451:24000
Farlow-Zeesix, very stony-Benteen families complex, 5 to 40 percent slopes562331288930gx3ut6451:24000
Sponsor-Benteen, deep families, association, 10 to 70 percent slopes4458268152045536pwy66320121:24000
Wesdy family-Lithic Cryorthents-Benteen family, association, 30 to 75 percent slopes40664561520305366wy66320121:24000
Wesdy family-Lithic Cryorthents-Benteen family, association, 30 to 75 percent slopes40631697095366wy7231:24000
Sponsor-Benteen, deep families, association, 10 to 70 percent slopes4453169710536pwy7231:24000
Benteen-Fossilbutte complex, 1 to 4 percent slopes632829562342wr48wy7231:24000

Map of Series Extent

Approximate geographic distribution of the BENTEEN 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 .