Official Series Description


Lab Data Summary

Aggregate lab data for the SHEDD soil series. This aggregation is based on all pedons with a current taxon name of SHEDD, 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 SHEDD 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
1540A2966S1965CA053008SHEDD7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2075005,-120.9674988
1540A2965S1965CA053009SHEDD6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1786118,-120.9483337
17UCD541100354-CA-11-003SHEDD2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7955284,-122.3233643

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHEDD 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 SHEDD 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 SHEDD 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 SHEDD 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 SHEDD 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 SHEDD series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the SHEDD 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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 SHEDD, 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 SHEDD 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
Shedd-Altamont association, 10 to 30 percent slopesSgD1881458843hdgdca02119611:20000
Shedd silty clay loam, 15 to 30 percent slopes, MLRA 15SfD13734588412tyzpca02119611:20000
Altamont-Shedd association, 3 to 15 percent slopesAnC701458577hd5tca02119611:20000
Shedd silty clay loam, 3 to 15 percent slopesSfC462458840hdg9ca02119611:20000
Shedd-Altamont-Gullied land complex, 8 to 15 percent slopesShC96458844hdgfca02119611:20000
Shedd silty clay loam, 30 to 50 percent slopesSfE72458842hdgcca02119611:20000
Shedd silt loam, 30 to 75 percent slopes, severely erodedSmG346115455726h96vca05319721:24000
Shedd silty clay loam, 30 to 50 percent slopes, erodedSnF225880455729h96yca05319721:24000
Linne-Shedd silty clay loams, 50 to 75 percent slopes, erodedLcG215700455638h940ca05319721:24000
Linne-Shedd silty clay loams, 15 to 50 percent slopes, erodedLcF215110455637h93zca05319721:24000
Shedd silty clay loam, 15 to 30 percent slopes, MLRA 15SnE149504557282tyzpca05319721:24000
Linne-Shedd silty clay loams, 15 to 30 percent slopesLcE13030455635h93xca05319721:24000
Linne-Shedd silty clay loams, 30 to 50 percent slopesLcF9055455636h93yca05319721:24000
Shedd silty clay loam, 9 to 15 percent slopesSnD3710455727h96wca05319721:24000
Shedd loam, 30 to 50 percent slopes, severely erodedShF35254456283h9stca06919651:20000
Linne-Shedd complex, 30 to 50 percent slopes, erodedLsF25089456222h9qvca06919651:20000
Shedd loam, 30 to 50 percent slopes, erodedShF24566456282h9ssca06919651:20000
Shedd loam, 15 to 30 percent slopes, erodedShE21276456281h9srca06919651:20000
Shedd loam, 9 to 15 percent slopesShD1175456280h9sqca06919651:20000
Linne-Shedd complex, 15 to 30 percent slopes, erodedLsE2353456221h9qtca06919651:20000
Shedd silt loam, 30 to 45 percent slopes, erodedSdE21766456621hb4qca60919631:20000
Shedd silt loam, 45 to 75 percent slopes, severely erodedSdF31171456622hb4rca60919631:20000
Shedd silt loam, 15 to 30 percent slopes, erodedSdD2646456620hb4pca60919631:20000
Shedd silty clay loam, 30 to 75 percent slopes, severely erodedSrG322999457505hc27ca67219661:20000
Shedd silty clay loam, 45 to 75 percent slopesSrG13472457504hc26ca67219661:20000
Shedd silty clay loam, 30 to 45 percent slopesSrF5118457503hc25ca67219661:20000
Shedd silty clay loam, diatomaceous, 30 to 45 percent slopesSsF2763457507hc29ca67219661:20000
Shedd silty clay loam, 15 to 30 percent slopes, MLRA 15SrE19804575022tyzpca67219661:20000
Shedd silty clay loam, diatomaceous, 45 to 75 percent slopesSsG518457508hc2bca67219661:20000
Shedd silty clay loam, diatomaceous, 15 to 30 percent slopesSsE439457506hc28ca67219661:20000

Map of Series Extent

Approximate geographic distribution of the SHEDD 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 .