Official Series Description


Lab Data Summary

Aggregate lab data for the CORMANT soil series. This aggregation is based on all pedons with a current taxon name of CORMANT, 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 CORMANT 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
56UMN1199S1970MN0691199Cormant1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7431412,-96.5666962
56UMN1517S1972MN0691517Cormant2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.8172112,-96.5651474
56UMN2678S1978MN1132678Cormant3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0754509,-96.2764969
88UMN1195S1970MN0771195Cormant3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.726429,-94.9338989

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CORMANT 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 CORMANT 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 CORMANT 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 CORMANT 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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Click the image to view it full size.

Competing Series

Soil series competing with CORMANT 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 CORMANT 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 CORMANT 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 CORMANT, 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. MN-2010-09-10-07 | Roseau County -

    Pattern of soils and underlying material in the Redby-Hiwood-Cormant association (Soil Survey of Roseau County, Minnesota).

  2. WI-2012-03-23-33 | Shawano County - October 1982

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

  3. 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 CORMANT 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
Cormant loamy fine sand, stratified substratum7343261432962gjjjmn00119961:20000
Cormant loamy fine sand, 0 to 2 percent slopes117319043975912x14qmn00719911:24000
Cormant-Redby complex, 0 to 2 percent slopes1206146826036602qkjxmn00719911:24000
Urban land-Cormant complex1086176397589fbqgmn00719911:24000
Cormant loamy fine sand, 0 to 2 percent slopes117299430264782x14qmn02919931:20000
Cormant loamy fine sand, dense till, 0 to 2 percent slopesI97A188102798845307d5mn06920071:12000
Cormant and Rosewood soils, very poorly drained, 0 to 1 percent slopesI100A11582279884221by0mn06920071:12000
Cormant loamy fine sand, 0 to 2 percent slopes117358063988582x14qmn07719891:24000
Cormant loamy fine sand, 0 to 2 percent slopes11719013571022x14qmn08919941:20000
Cormant loamy fine sand, dense till, 0 to 2 percent slopesI97A92798976307d5mn08919941:20000
Cormant loamy sand, 0 to 1 percent slopesI573A527990042mbk2mn08919941:20000
Cormant loamy fine sand, 0 to 2 percent slopes117150423947852x14qmn13519991:24000
Cormant-Redby complex, 0 to 2 percent slopes120614926394794f7t9mn13519991:24000
Cormant loamy fine sand, dense till, 0 to 2 percent slopesI97A12732799860307d5mn13519991:24000
Redby-Cormant complex, 0 to 3 percent slopesB250A96229437962dv55mn62520151:24000
Leafriver-Cormant-Markey complex, 0 to 1 percent slopesB247A56129437932dv52mn62520151:24000
Cormant-Leafriver complex, 0 to 1 percent slopesB249A23729437952dv54mn62520151:24000
Cormant loamy sand, 0 to 1 percent slopesI573A424726430062mbk2nd06719721:20000
Deford and Cormant soils, 0 to 2 percent slopesDeCo1908531190472xxj0wi07519871:20000
Deford and Cormant soils, 0 to 2 percent slopesDeCo1709231190522xxj0wi08319851:15840
Deford and Cormant soils, 0 to 2 percent slopesDeCo233731190562xxj0wi11519811:15840

Map of Series Extent

Approximate geographic distribution of the CORMANT 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 .