Official Series Description


Lab Data Summary

Aggregate lab data for the SCONSIN soil series. This aggregation is based on all pedons with a current taxon name of SCONSIN, 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 SCONSIN 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
90A89P029188WI119001Sconsin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2827797,-90.5766678
90A89P0521S1988WI119001ASconsin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2827797,-90.5766678
90A93P0377S1992WI113004Sconsin6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.8244438,-91.3472214

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with SCONSIN, 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 SCONSIN 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
Sconsin silt loam, 1 to 6 percent slopes648B1434492652tp00wi01320041:12000
Sconsin silt loam, 1 to 6 percent slopesScB158024316512tp00wi06919931:20000
Freeon-Sconsin silt loams, 2 to 6 percent slopesFsB7530431619gh46wi06919931:20000
Sconsin silt loam, 1 to 6 percent slopes648B547015988092tp00wi09920061:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B4026627366p1tmwi09920061:12000
Chequamegon, very stony-Sconsin complex, 2 to 6 percent slopes1345B149915987611qnmywi09920061:12000
Crystal Lake-Freeon, very stony-Sconsin complex, 2 to 6 percent slopes863B556627581p21kwi09920061:12000
Sconsin silt loam, 1 to 6 percent slopes648B71236251002tp00wi10720061:12000
Sconsin-Maincreek complex, 0 to 3 percent slopes950A2413727219sdqpwi10720061:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B1946625174nzjxwi10720061:12000
Chequamegon, very stony-Sconsin complex, 2 to 6 percent slopes1345B45913852961hhhzwi10720061:12000
Pence-Sconsin-Tawas complex, 0 to 25 percent slopes746D138757625tfcjwi10720061:12000
Sconsin silt loam, 1 to 6 percent slopes648B227466258802tp00wi11320061:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B5869625844p07jwi11320061:12000
Chequamegon, very stony-Sconsin complex, 2 to 6 percent slopes1345B151716699591t1qnwi11320061:12000
Crystal Lake-Freeon, very stony-Sconsin complex, 2 to 6 percent slopes863B4204581189mhs1wi11920021:12000
Freeon, very stony-Sconsin complex, 2 to 6 percent slopes345B2890435139glsrwi11920021:12000
Sconsin silt loam, 1 to 6 percent slopes648B26424352052tp00wi11920021:12000
Sconsin silt loam, 1 to 6 percent slopes648B13584490372tp00wi12920021:12000

Map of Series Extent

Approximate geographic distribution of the SCONSIN 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 .