Official Series Description


Lab Data Summary

Aggregate lab data for the TOWNSHIP soil series. This aggregation is based on all pedons with a current taxon name of TOWNSHIP, 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 TOWNSHIP 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
43A96P00261995ID035009Township7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.585556,-115.7841644
43A99P054799ID035004Township7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7641678,-115.8386078

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the TOWNSHIP 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 TOWNSHIP 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 TOWNSHIP 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 TOWNSHIP 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with TOWNSHIP 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 TOWNSHIP 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 TOWNSHIP 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 TOWNSHIP, 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 TOWNSHIP 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
Township-Rettig complex, 35 to 75 percent slopesTn122956447892x1zdid05720131:24000
Township, cool-Township, cool, moist complex, 35 to 65 percent slopesTn51733645302pnh6id05720131:24000
Township-Grandad, dry complex, 20 to 50 percent slopesTg21623645292pngwid05720131:24000
Rettig-Township complex, 35 to 60 percent slopesTr2j12142501993v2yfid05720131:24000
Township-Rock outcrop-Township, cool complex, 10 to 25 percent slopesTn7297697415rdq8id05720131:24000
Township, cool-Township, cool, moist complex, 35 to 65 percent slopesTn54112663027pnh6id60819941:24000
Township-Rock outcrop-Township, cool complex, 10 to 25 percent slopesTn7262663028rdq8id60819941:24000
Humic Udivitrands-Township-Typic Haplocryands families, complex, weakly weathered mica schist geology, mid to high elevation broadly convex mountain slopes, south aspect, fern glades2lgr62229367812lgr6id60819941:24000
Township-Humic Udivitrands families, complex, weakly weathered mica schist geology, dissected stream breaklands, north aspects2lgs5429368022lgs5id60819941:24000
Township-Rettig complex, 35 to 75 percent slopes234201597773962x1zdid61220031:24000
Rettig-Township complex, 35 to 60 percent slopes19810911777400v2yfid61220031:24000
Township-Rettig-Nakarna complex, 35 to 65 percent slopes2354501777398v2ycid61220031:24000
Rettig-Township-Stepoff complex, 35 to 70 percent slopes1992392777397v2ybid61220031:24000
Township-Rettig complex, 15 to 35 percent slopes2331148777399v2ydid61220031:24000
Township-Humic Udivitrands-Typic Haplocryands families, complex, weakly weathered mica schist geology, mid to high elevation broadly convex mountain slopes, south aspect, fern glades2lgr75628508992lgr7id61220031:24000
Township-Humic Udivitrands families, complex, weakly weathered mica schist geology, dissected stream breaklands, north aspects780524723974832lgs5id6701:24000
Township family, weakly weathered mica schist geology, mountain slopes, south aspects770325523974772lgrzid6701:24000
Typic Vitrixerands-Township families, complex, weakly weathered mica schist geology, dissected stream breaklands, south aspects779281823974822lgs4id6701:24000
Rock outcrop-Township family-Typic Fulvicryands family, complex, steep breaklands and avalanche chutes, weakly weathered mica schist, timber-brush-fern glade mosaic, north aspects715255523974392lgqrid6701:24000
Typic Vitrixerands-Township-Hugus families, complex, moderately weathered mica schist geology, dissected breaklands, south aspects782194223974852lgs7id6701:24000
Township-Humic Udivitrands-Typic Haplocryands families, complex, weakly weathered mica schist geology, mid to high elevation broadly convex mountain slopes, south aspect, fern glades751170623974542lgr7id6701:24000
Township-Humic Udivitrands-Typic Haplocryands families, complex, weakly weathered mica schist geology, mid to high elevation broadly convex mountain slopes, north aspect, fern glades75282023974562lgr9id6701:24000
Humic Udivitrands-Township-Typic Haplocryands families, complex, weakly weathered mica schist geology, mid to high elevation broadly convex mountain slopes, south aspect, fern glades75074023974532lgr6id6701:24000
Typic Vitrixerands family-Rock outcrop-Township family, complex, weakly weathered mica schist geology, mountain slopes, south aspects, dry77129723974782lgs0id6701:24000
Typic Vitrixerands-Township families, complex, weakly weathered mica schist geology, stream breaklands, south aspects7837923974862lgs8id6701:24000

Map of Series Extent

Approximate geographic distribution of the TOWNSHIP 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 .