Official Series Description


Lab Data Summary

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

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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 BENDAHL 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 BENDAHL 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 BENDAHL 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.

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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.

Soil series sharing subgroup-level classification with BENDAHL, 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 BENDAHL 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
Beeskove-Bendahl-Foyslake families, complex, moderately steep mountain slopes30MC3874528090582tr4hmt60319891:24000
Beeskove, Bendahl and Foyslake families, steep mountain slopes64MC2972628091182tr6fmt60319891:24000
Bendahl-Foyslake families-Rock outcrop, stream breaklands60MC2005828091012tr5wmt60319891:24000
Bendahl and Foyslake families, steep mountain slopes64MD1799728091192tr6gmt60319891:24000
Stevie-Bendahl families-Rock outcrop complex, stream breaklands60MD1540528091022tr5xmt60319891:24000
Bendahl family, steep mountain slopes64MG234928091212tr6jmt60319891:24000
Beeskove-Bendahl-Foyslake families, complex, moderately steep mountain slopes30MC029953102tr4hmt63520061:24000
Beeskove, Bendahl and Foyslake families, steep mountain slopes64MC44729953622tr6fmt63819851:24000
Bendahl family, steep mountain slopes64MG20730449762tr6jmt63819851:24000
Bendahl-Foyslake families-Rock outcrop, stream breaklands60MC1229953532tr5wmt63819851:24000
Bendahl family, steep mountain slopes64MG1529953862tr6jmt64419951:24000
Bendahl gravelly ashy silt loam, 15 to 30 percent slopes98E221215642757s1mt65119971:24000
Beeskove-Bendahl-Foyslake families, complex, moderately steep mountain slopes30MC129029954102tr4hmt65119971:24000
Bendahl gravelly ashy silt loam, 30 to 50 percent slopes98F118215642957s3mt65119971:24000
Bendahl-Foyslake families-Rock outcrop, stream breaklands60MC50529954322tr5wmt65119971:24000
Beeskove, Bendahl and Foyslake families, steep mountain slopes64MC24929954402tr6fmt65119971:24000
Bendahl and Foyslake families, steep mountain slopes64MD1228483082tr6gmt65119971:24000

Map of Series Extent

Approximate geographic distribution of the BENDAHL 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 .