Official Series Description


Lab Data Summary

Aggregate lab data for the BIELENBERG soil series. This aggregation is based on all pedons with a current taxon name of BIELENBERG, 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 BIELENBERG 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
43B92P107192MT043015Bielenberg5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.4752769,-112.1188889
4491P094691MT093007Bielenberg5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9958344,-112.7219467

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BIELENBERG 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 BIELENBERG 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 BIELENBERG 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 BIELENBERG 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 flats position figure.

Competing Series

Soil series competing with BIELENBERG 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 BIELENBERG 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 BIELENBERG 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 BIELENBERG, 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 BIELENBERG 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
Bielenberg-Catgulch, very stony-Breeton complex, 15 to 45 percent slopes454E511515550556t9mt62219971:24000
Bielenberg-Catgulch, very stony complex, 4 to 15 percent slopes454D214815550456t8mt62219971:24000
Catgulch, very stony-Bielenberg-Rock outcrop complex, 15 to 45 percent slopes654E53115563456ygmt62219971:24000
Bielenberg-Burtoner, very stony-Catgulch, bouldery, complex, 8 to 25 percent slopes1461D298115062251qsmt62719981:24000
Clancy-Bielenberg-Connieo complex, 4 to 15 percent slopes1835D246515073351vcmt62719981:24000
Clancy-Bielenberg-Connieo complex, 15 to 35 percent slopes1837E209415073551vfmt62719981:24000
Clancy, very stony-Crampton, bouldery-Bielenberg, very stony, complex, 15 to 45 percent slopes1287E134415058151pgmt62719981:24000
Clancy, bouldery-Bielenberg, stony-Catgulch, bouldery, complex, 15 to 45 percent slopes1836E120915073451vdmt62719981:24000
Clancy-Bielenberg-Breeton complex, 15 to 35 percent slopes1830E92215072851v6mt62719981:24000
Crackerville-Bielenberg-Catgulch, bouldery, complex, 20 to 35 percent slopes1283E90515057751pbmt62719981:24000
Crackerville-Bielenberg-Catgulch, bouldery, complex, 8 to 20 percent slopes1282D89215057651p9mt62719981:24000
Kellygulch, bouldery-Rock outcrop-Bielenberg complex, 35 to 70 percent slopes1821F86615072351v1mt62719981:24000
Crackerville-Bielenberg-Catgulch, bouldery, complex, 15 to 35 percent slopes, warm1286E45415058051pfmt62719981:24000
Sawicki-Bielenberg, very stony-Tolbert, very stony, complex, 15 to 45 percent slopes1656E42115066651s6mt62719981:24000
Clancy-Clancy, very stony-Bielenberg complex, 4 to 15 percent slopes1838D14215073651vgmt62719981:24000
Bielenberg-Catgulch, very stony-Breeton complex, 15 to 45 percent slopes1731621465474xhbmt63619831:24000
Catgulch, very stony-Bielenberg-Rock outcrop complex, 15 to 45 percent slopes181571465594xhqmt63619831:24000

Map of Series Extent

Approximate geographic distribution of the BIELENBERG 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 .