Official Series Description


Lab Data Summary

Aggregate lab data for the DEPUTY soil series. This aggregation is based on all pedons with a current taxon name of DEPUTY, 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 DEPUTY 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
114BJF76091976IN077009Deputy2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6932556,-85.5364222
114B90P029189IN143002Deputy6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6780548,-85.5849991
114B90P0527S1987IN143013DEPUTY5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7936096,-85.7469406
114B06N0336S2005IN079004Deputy7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9433327,-85.6147232

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DEPUTY 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 DEPUTY 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 DEPUTY 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 DEPUTY 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 DEPUTY 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 DEPUTY 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 DEPUTY 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.

Click the image to view it full size.

Soil series sharing subgroup-level classification with DEPUTY, 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 DEPUTY 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
Deputy-Trappist silt loams, 6 to 12 percent slopes, erodedDtvC228492011096r8din01920011:12000
Trappist-Deputy complex, 6 to 12 percent slopes, severely erodedTsaC3272418515966nwin01920011:12000
Deputy silt loam, 2 to 6 percent slopes, erodedDeB2146796464111csgin07719821:15840
Deputy silt loam, 6 to 12 percent slopes, erodedDeC283996464211cshin07719821:15840
Deputy silt loam, 6 to 12 percent slopes, severely erodedDeC326496464311csjin07719821:15840
Deputy-Trappist silty clay loams, 6 to 15 percent slopes, severely erodedDtzC3329616514501sfglin07920101:12000
Scottsburg-Deputy silt loams, 2 to 6 percent slopes, erodedScfB2262116514101sff9in07920101:12000
Deputy silt loam, 6 to 15 percent slopes, erodedDtwC2255416514491sfgkin07920101:12000
Blocher, soft black shale substratum-Jennings-Deputy silt loams, 6 to 12 percent slopes, erodedBlcC2196016133471r4tgin07920101:12000
Blocher, soft black shale substratum-Jennings-Deputy silt loams, 6 to 12 percent slopes, severely erodedBlcC3182216134391r4xfin07920101:12000
Urban land-Deputy-Scottsburg complex, 2 to 15 percent slopesUdaB110816132251r4pjin07920101:12000
Deputy silt loam, 2 to 6 percent slopes, erodedDddB216131656425kc9in14319951:12000
Deputy silt loam, 6 to 12 percent slopes, erodedDddC210881656435kcbin14319951:12000
Deputy silt loam, 6 to 12 percent slopes, severely erodedDddC35671656445kccin14319951:12000

Map of Series Extent

Approximate geographic distribution of the DEPUTY 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 .