Official Series Description


Lab Data Summary

Aggregate lab data for the BENGAL soil series. This aggregation is based on all pedons with a current taxon name of BENGAL, 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 BENGAL 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 BENGAL 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 BENGAL 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 BENGAL 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 BENGAL 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 terrace figure.

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

Competing Series

Soil series competing with BENGAL 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 BENGAL 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 BENGAL 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with BENGAL, 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 BENGAL 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
Yanush-Avant-Bengal complex, 35 to 60 percent slopes57G27798577501mcy2ar09719971:24000
Bengal-Bismarck-Yanush complex, 15 to 35 percent slopes, extremely stony6F229055774722y1mtar09719971:24000
Bengal-Bismarck-Yanush complex, 8 to 15 percent slopes5D92205774762y1mrar09719971:24000
Yanush-Avant-Bengal complex, 15 to 35 percent slopes57F6759577515mcyjar09719971:24000
Bengal-Bismarck-Bigfork complex, 35 to 60 percent slopes, extremely stony4G67465774702y1msar09719971:24000
Bengal-Bismarck-Yanush complex, 15 to 35 percent slopes, extremely stony6265815428692y1mtar10920051:20000
Bengal-Bismarck-Yanush complex, 8 to 15 percent slopes544415428722y1mrar10920051:20000
Bengal-Bismarck-Bigfork complex, 35 to 60 percent slopes, extremely stony736515428682y1msar10920051:20000
Yanush-Avant-Bengal complex, 35 to 60 percent slopes9835415428931nshrar10920051:20000
Yanush-Avant-Bengal complex, 15 to 35 percent slopes9710915429061nsj5ar10920051:20000
Bengal-Bismarck-Yanush complex, 15 to 35 percent slopes4F251885708472y1mkar11319911:20000
Bismarck-Bengal-Bigfork complex, 35 to 60 percent slopes, rubbly9G186575708452y1mlar11319911:20000
Bengal-Bismarck-Yanush complex, 8 to 15 percent slopes4D58025708512y1mrar11319911:20000
Bengal-Carnasaw-Clebit complex, 15 to 35 percent slopes, extremely stonyNG4021036524953811qfz4ar14919851:20000
Bengal-Carnasaw-Clebit complex, 35 to 60 percent slopes, rubblyNG20113524953831qfz8ar14919851:20000
Carnasaw-Bengal-Clebit complex, 15 to 30 percent slopesEhE61905571680m5w9ok06119721:24000
Carnasaw-Bengal-Clebit complex, 3 to 15 percent slopesEhD32873571679m5w8ok06119721:24000
Carnasaw and Bengal soils, 30 to 45 percent slopesEkF5595571681m5wbok06119721:24000
Bengal-Denman association, 8 to 20 percent slopes233423571488m5p3ok07719801:24000
Bengal-Clebit complex, 3 to 8 percent slopes16478571477m5nrok07719801:24000
Bengal-Clebit association, 3 to 15 percent258163571402m5lbok07919811:24000
Bengal-Octavia-Tuskahoma complex, 4 to 20 percent slopes435773571424m5m1ok07919811:24000
Bengal-Pirum-Clebit complex, 5 to 15 percent slopes533978571435m5mdok07919811:24000
Sherless-Bengal complex, 3 to 15 percent slopes6424380571451m5mxok07919811:24000
Bengal stony fine sandy loam, 15 to 35 percent slopes114425571391m5kzok07919811:24000
Bengal-Octavia complex, 15 to 40 percent slopes312918571413m5lpok07919811:24000
Bengal-Clebit-Clearview complex, 5 to 30 percent slopesEhE302854571544m5qxok12119661:24000
Bengal-Clebit-Rock outcrop complex, 30 to 60 percent slopesEhF60773571545m5qyok12119661:24000

Map of Series Extent

Approximate geographic distribution of the BENGAL 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 .