Official Series Description


Lab Data Summary

Aggregate lab data for the DELRIDGE soil series. This aggregation is based on all pedons with a current taxon name of DELRIDGE, 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 DELRIDGE 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
5483P0029S1981SD093004DELRIDGE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.5833321,-102.3038864

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DELRIDGE 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 DELRIDGE 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 DELRIDGE 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 DELRIDGE 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 DELRIDGE 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 DELRIDGE 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 DELRIDGE 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 DELRIDGE, 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-2012-03-15-49 | Harding County - December 1988

    Pattern of soils and parent material in the Cabbart-Rock outcrop-Delridge association (Soil Survey of Harding County, SD; 1988).

  2. SD-2012-03-15-73 | Meade County, Northern Part - January 1986

    Pattern of soils and parent material in the Assinniboine-Blackhall-Twilight association (Soil Survey of Meade County, Northern Part, SD; 1986).

  3. SD-2012-03-15-74 | Meade County, Northern Part - January 1986

    Pattern of soils and parent material in the Cabbart-Delridge association (Soil Survey of Meade County, Northern Part, SD; 1986).

Map Units

Map units containing DELRIDGE 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
Cabbart-Delridge loams, 15 to 40 percent slopesCdE21629355728cy53sd06319841:24000
Delridge-Cabbart loams, 6 to 15 percent slopesDcC9352355734cy59sd06319841:24000
Delridge loam, 6 to 15 percent slopesDaD31165354310cwpcsd60019741:24000
Delridge-Cabbart loams, 6 to 15 percent slopesDeC82127355430cxvhsd60119831:24000
Eapa-Delridge loams, 2 to 6 percent slopesEdB19979355434cxvmsd60119831:24000
Tanna-Delridge complex, 2 to 6 percent slopesTdB16640355469cxwrsd60119831:24000
Eapa-Delridge loams, 6 to 9 percent slopesEdC12058355435cxvnsd60119831:24000
Tanna-Delridge complex, 6 to 9 percent slopesTdC5188355470cxwssd60119831:24000
Cabbart-Delridge loams, 6 to 30 percent slopesP060E24527681622qt26wy01119781:24000
Delridge-Badland complex, 20 to 50 percent slopes -- draft543792014802111lp8rwy0411:24000
Morset-Teeler-Delridge complex, 8 to 35 percent slopes216409323761962krmhwy0411:24000
Chinook-Delridge complex, 3 to 10 percent slopesP068C222327459612qt28wy04519841:24000
Cabbart-Delridge loams, 6 to 30 percent slopesP060E215927460142qt26wy04519841:24000
Chinook-Delridge complex, 10 to 30 percent slopesP068E70927459622qt29wy04519841:24000
Skelridge, very stony-Delridge-Yamacall complex, 10 to 50 percent slopes9772083715292131nb8gwy71920131:24000
Delridge-Badland complex, 20 to 50 percent slopes -- draft4054499624944771lp8rwy7231:24000
Delridge-Yamacall-Bronec complex, 2 to 25 percent slopes8205435026119642qsv9wy7231:24000

Map of Series Extent

Approximate geographic distribution of the DELRIDGE 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 .