Official Series Description


Lab Data Summary

Aggregate lab data for the DENBY soil series. This aggregation is based on all pedons with a current taxon name of DENBY, 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 DENBY 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
6482P082982SD103012Denby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.8222237,-102.1999969
6482P083082SD103015Denby6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7208328,-102.0425034
6410N0718S2009SD103002Denby8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9742611,-102.2228389

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DENBY 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 DENBY 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 DENBY 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 DENBY 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with DENBY 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 DENBY 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 DENBY 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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Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

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 DENBY, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. SD-2012-03-15-13 | Custer and Pennington Counties, Prairie Parts - May 1996

    Pattern of soils, topography, and underlying material in the Cedarpass-Denby-Interior and the Orella-Fairburn-Badland associations (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

Map Units

Map units containing DENBY 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
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesIrB1492025809142t34xsd60620111:24000
Cedarpass-Denby complex, 0 to 3 percent slopesCfA1243125808832t34msd60620111:24000
Denby silty clay, 0 to 3 percent slopesDmA282625808932t34hsd60620111:24000
Whitewater-Denby silty clays, 1 to 6 percent slopesU802B825829422qqtqsd60620111:24000
Badland-Denby-Interior complex, 0 to 90 percent slopesBa5783233336462zj55sd61019651:20000
Denby silty clay, 0 to 3 percent slopesCy1167229255222t34hsd61019651:20000
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesIv935825826302t34xsd61120111:24000
Cedarpass-Denby complex, 0 to 3 percent slopesCfA702225810092t34msd61120111:24000
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesU335B614623751202t34xsd61220111:20000
Cedarpass-Denby complex, 0 to 3 percent slopesU120A397423754452t34msd61220111:20000
Whitewater-Denby silty clays, 1 to 6 percent slopesU802B325825474312qqtqsd61220111:20000
Denby silty clay, 0 to 3 percent slopesU165A220923751102t34hsd61220111:20000
Badland-Denby-Interior complex, 0 to 90 percent slopesBa4751133336472zj55sd61320111:24000
Denby silty clay, 0 to 3 percent slopesCy2755625826892t34hsd61320111:24000
Whitewater-Denby silty clays, 1 to 6 percent slopesU802B70025828592qqtqsd61320111:24000
Cedarpass-Denby complex, 0 to 3 percent slopesU120A51425828142t34msd61320111:24000
Interior, occasionally flooded-Cedarpass-Denby complex, 0 to 6 percent slopesU335B26525828242t34xsd61320111:24000

Map of Series Extent

Approximate geographic distribution of the DENBY 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 .