Official Series Description


Lab Data Summary

Aggregate lab data for the DECROSS soil series. This aggregation is based on all pedons with a current taxon name of DECROSS, 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 DECROSS 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
43B40A3107S1966WY019002Decross2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9336128,-107.0497208
43B40A3135S1967WY019005Decross7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.9375,-107.0538864

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DECROSS 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 DECROSS 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 DECROSS 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 DECROSS 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 DECROSS 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 DECROSS 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 DECROSS 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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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 DECROSS, 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 DECROSS 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
Decross loam, 1 to 15 percent slopes192444498449jqp0co63319811:24000
Greyback-Rooset association, hillyGRD572202391225y1hid75819981:24000
Greyback-Rooset association, steepGRE369202391325y1jid75819981:24000
Daisypeak, very bouldery-Decross-Monumentpeak, very stony families, complex, 4 to 25 percent slopes1262E2530397092r6y8mt61319751:24000
Daisypeak, very bouldery-Decross-Monumentpeak, very stony families, complex, 4 to 25 percent slopes1262E221526044772r6y8mt6321:24000
Tophat-Woodhurst, cobbly-Decross, complex, 2 to 20 percent slopes5434E5348741479swkpmt6691:24000
Decross-Auzqui, very stony-Youga complex, 8 to 35 percent slopes217669123761952krmgwy0411:24000
Woosley-Decross association76133711521245397wy04319761:24000
Decross-Woosley associationDE16384350840cs2fwy61919711:24000
Amsden-Decross associationAM2026350807cs1cwy61919711:24000
Woosley-Decross association761470816483wdm5wy61919711:24000
Decross-Woosley association, sloping16937816600wdqywy61919711:24000
Greyback-Rooset association, hillyGRD692715269853wrwy62319711:20000
Greyback-Rooset association, steepGRE656315269953wswy62319711:20000
Buckskin-Decross association, hillyBDD501515269053whwy62319711:20000
Buckskin-Decross association, undulatingBDC394715268953wgwy62319711:20000
Decross-Woosley association, sloping1691791502257jvmvwy62519851:24000
Sedimentary Sideslopes, Aspen-Big Sagebrush Complex363115642554694530wwy6351:24000
Woosley-Decross-Starman complex, 2 to 20 percent slopes22125148637780pdnkwy6471:24000
Fornor-Decross complex, 1 to 30 percent slopes149D220215792459bbwy65620081:24000
Woosley-Decross-Starman association, 2 to 20 percent slopes221D122815793859bswy65620081:24000
Sedimentary Sideslopes, Subalpine Fir-Big Sagebrush-Aspen Complex364996951518745315wy66219981:24000
Sedimentary Sideslopes, Aspen-Big Sagebrush Complex36312983151865530wwy66219981:24000
Foothill Sideslopes, Big Sagebrush-Aspen-Subalpine fir Complex66211383151898531ywy66219981:24000
Mountain Front Moraines, Subalpine Fir-Aspen-Big Sagebrush Complex43431106151919532mwy66219981:24000
Fornor-Decross complex, hilly14918530503014jwf8wy71319861:24000
Woosley-Decross-Starman association, rolling2218098503100jwj1wy71319861:24000
Monaberg family-Beavet-Decross complex, 2 to 8 percent slopes650129253002xyfmwy7231:24000
Wilhelm, extremely stony-Badwater-Decross complex, 8 to 35 percent slopes651129251292wdj8wy7231:24000

Map of Series Extent

Approximate geographic distribution of the DECROSS 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 .