Official Series Description


Lab Data Summary

Aggregate lab data for the SHADY soil series. This aggregation is based on all pedons with a current taxon name of SHADY, 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 SHADY 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
12891P043090TN019001Shady7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2770309,-82.2929077
n/a91P043190TN057004Shady7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHADY 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 SHADY 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 SHADY 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 SHADY 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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Competing Series

Soil series competing with SHADY 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 SHADY 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 SHADY 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 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 SHADY, 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 SHADY 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
Shady loam, 2 to 6 percent slopesShB248116118451r380ga01520131:12000
Shady loam, 0 to 2 percent slopes, occasionally floodedShA218916118441r37zga01520131:12000
Shady-Whitwell complex, 2 to 6 percent slopes, rarely floodedSeB2985202379325xxnga12920071:12000
Ketona-Shady complex, 2 to 6 percent slopesKsB1345202382925xytga12920071:12000
Shady fine sandy loam, 2 to 6 percent slopesSdB485202383925xz4ga12920071:12000
Sipsey-Shady complex, 2 to 6 percent slopesSpB135202381725xyfga12920071:12000
Shady loam, 2 to 6 percent slopesShB152511177trtfga22320101:12000
Shady loam, 0 to 2 percent slopes, occasionally floodedShA52511176trtdga22320101:12000
Shady loam, 2 to 6 percent slopesSdB224424803262p7zjga61920121:24000
Shady loam, 0 to 2 percent slopesSd88124803252p7zhga61920121:24000
Shady loam, occasionally floodedSk575188735921byktn00119781:15840
Shady loam, occasionally floodedSfA11825079482q78dtn01119511:20000
Shady loam, 1 to 4 percent slopes, rarely floodedShB2249526482knv9tn01920001:24000
Shady loam, 1 to 4 percent slopesShB693525036kmbntn05719961:24000
Shady-Whitwell complex, 0 to 3 percent slopes, rarely floodedSo1942632844p7jbtn09320051:12000
Shady loam, 2 to 5 percent slopesShB1784632842p7j8tn09320051:12000
Shady loam, 5 to 12 percent slopesShC158632843p7j9tn09320051:12000
Shady loam, 2 to 5 percent slopesShB472526140knh8tn10719991:24000
Shady loam, 5 to 12 percent slopesShC229526180knjktn10719991:24000
Shady-Altavista complex, 1 to 5 percent slopesSaB178815393601nntstn12119681:15840
Shady-Hamblen complex, 0 to 3 percent slopes, occasionally floodedSh129614218101jqhvtn12119681:15840
Shady-Altavista complex, 5 to 12 percent slopesSaC47415393941nnvwtn12119681:15840
Shady loam, 2 to 5 percent slopesShB729843334x9kbtn13320031:24000
Shady loam, 5 to 12 percent slopes, erodedShC2318843335x9kctn13320031:24000
Shady loam, 1 to 5 percent slopesShB1898530795ktbftn14320031:24000
Shady loam, 0 to 3 percent slopes, occasionally floodedSm1438728824sgdgtn14320031:24000
Cobstone-Shady-Urban land complex, 0 to 5 percent slopes, rarely floodedCDB1048728886sgggtn14320031:24000
Shady loam, occasionally floodedSd33071475614301gxtn14520051:24000
Shady-Swafford-Urban land complex, 2 to 5 percent slopesSfB96314756431ljjdtn14520051:24000
Shady loam, occasionally floodedSh1136524828km3ytn60620011:24000

Map of Series Extent

Approximate geographic distribution of the SHADY 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 .