Official Series Description


Lab Data Summary

Aggregate lab data for the SHAWANO soil series. This aggregation is based on all pedons with a current taxon name of SHAWANO, 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 SHAWANO 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
57UMN2858S1978MN137078 (2858)Shawano2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.6727295,-92.8412323
93AUMN2869S1978MN137076 (2869)Shawano2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.8697934,-92.3265972

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SHAWANO 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 SHAWANO 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 SHAWANO 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 SHAWANO 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 SHAWANO 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 SHAWANO 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 SHAWANO 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 SHAWANO, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. WI-2012-03-23-18 | Marinette County - February 1991

    Pattern of soils and parent material in the Wainola-Deford association (Soil Survey of Marinette County, WI; 1991).

  2. WI-2012-03-23-34 | Shawano County - October 1982

    Relationship of sols and substratum in the Shawano-Rousseau-Wainola general map unit (Soil Survey of Shawano County, WI; 1982).

Map Units

Map units containing SHAWANO 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
Lavell-Shawano complex, 1 to 6 percent slopesB36B682494012wmdhmn61320161:24000
Shawano loamy fine sand, 1 to 8 percent slopesF16B82494005wmf0mn61320161:24000
Lavell-Shawano complex, 1 to 6 percent slopesB36B1252186149920h1cmn61720071:24000
Shawano loamy fine sand, 1 to 8 percent slopesF16B679186146620h09mn61720071:24000
Shawano loamy fine sand, 6 to 18 percent slopesB40D284186150720h1mmn61720071:24000
Lavell-Shawano complex, 1 to 6 percent slopesB36B107624380862mv0ymn61920091:24000
Shawano loamy fine sand, 6 to 18 percent slopesB40D100194687723bwhmn61920091:24000
Lavell-Shawano complex, 1 to 6 percent slopesB36B1074823003wmdhmn62120061:24000
Shawano loamy fine sand, 6 to 18 percent slopesB40D468823005wmdkmn62120061:24000
Shawano loamy fine sand, 1 to 8 percent slopesF16B133823019wmf0mn62120061:24000
Shawano loamy fine sand, 2 to 6 percent slopesSfB6910426245g9jvwi00919701:20000
Shawano loamy fine sand, 6 to 12 percent slopesSfC1104426246g9jwwi00919701:20000
Shawano fine sand, hillySeD882426244g9jtwi00919701:20000
Shawano fine sand, rollingSeC765426243g9jswi00919701:20000
Shawano fine sand, 0 to 6 percent slopes557B6151448839h21pwi01320041:12000
Shawano fine sand, 6 to 12 percent slopes557C2753448963h25pwi01320041:12000
Shawano fine sand, 12 to 30 percent slopes557D1132448990h26kwi01320041:12000
Rousseau-Shawano fine sands, 2 to 12 percent slopesRpC581422269g5dlwi02919751:15840
Rousseau-Shawano fine sands, 12 to 35 percent slopesRpD298422270g5dmwi02919751:15840
Shawano loamy fine sand, 2 to 6 percent slopesSfB7133422448g5lcwi07519871:20000
Shawano loamy fine sand, 6 to 12 percent slopesSfC4293422449g5ldwi07519871:20000
Shawano loamy fine sand, 12 to 30 percent slopesSfD776422450g5lfwi07519871:20000
Shawano fine sand, 0 to 6 percent slopesSfB1180395863f8xswi07819981:12000
Shawano fine sand, 6 to 15 percent slopesSfC1071395865f8xvwi07819981:12000
Shawano fine sand, 15 to 35 percent slopesSfD448395864f8xtwi07819981:12000
Shawano fine sand, 2 to 6 percent slopesSfB12574422511g5ndwi08319851:15840
Shawano fine sand, 6 to 12 percent slopesSfC9748422512g5nfwi08319851:15840
Shawano fine sand, 12 to 30 percent slopesSfD3065422513g5ngwi08319851:15840
Shawano fine sand, rollingSeC3160422594g5r2wi08719751:15840
Shawano fine sand, hillySeD511422595g5r3wi08719751:15840
Shawano fine sand, 0 to 6 percent slopes557B357224277192mh7jwi09519781:15840
Shawano fine sand, 6 to 12 percent slopes557C210024277232mh7nwi09519781:15840
Shawano fine sand, 12 to 30 percent slopes557D139124277222mh7mwi09519781:15840
Braham-Shawano complex, 12 to 35 percent slopes3082E224870352pgyywi09519781:15840
Shawano loamy fine sand, 1 to 6 percent slopesSfB7267422631g5s8wi11519811:15840
Shawano loamy fine sand, 6 to 12 percent slopesSfC4409422632g5s9wi11519811:15840
Shawano loamy fine sand, 12 to 20 percent slopesSfD878422633g5sbwi11519811:15840
Shawano-Briggsville complex, 6 to 12 percent slopesSgC342422635g5sdwi11519811:15840
Shawano-Briggsville complex, 2 to 6 percent slopesSgB253422634g5scwi11519811:15840
Shawano loamy fine sand, 2 to 6 percent slopesSfB1858422749g5x2wi13519821:15840
Shawano loamy fine sand, 6 to 12 percent slopesSfC1633422750g5x3wi13519821:15840
Shawano loamy fine sand, 12 to 20 percent slopesSfD589422751g5x4wi13519821:15840

Map of Series Extent

Approximate geographic distribution of the SHAWANO 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 .