Official Series Description


Lab Data Summary

Aggregate lab data for the SEVERN soil series. This aggregation is based on all pedons with a current taxon name of SEVERN, 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 SEVERN were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the SEVERN 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 SEVERN 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 SEVERN 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 SEVERN 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 hills figure.

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 SEVERN 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 SEVERN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the SEVERN 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with SEVERN, 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. TX-2010-11-03-04 | Fannin County - 2001

    Typical landscape pattern and major soils along the Red River (Soil Survey of Fannin County, Texas; 2001).

Map Units

Map units containing SEVERN 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
Severn silt loamSn4370566394m0csar13119711:20000
Severn silt loam, 0 to 3 percent slopes, gently undulating, rarely flooded72433025649502tgljar67019811:20000
Severn silt loam, 0 to 1 percent slopes, rarely flooded71117275649492tglhar67019811:20000
Severn silt loam, occasionally flooded734513564951lyw7ar67019811:20000
Severn very fine sandy loam, 1 to 3 percent slopes, gently undulating, occasionally floodedSkB600615922452v9rdla01520051:24000
Severn very fine sandy loam, frequently floodedSNA422015922461qfvsla01520051:24000
Severn silt loam, 0 to 1 percent slopes, rarely floodedSgA388215922432tglhla01520051:24000
Severn silt loam, 0 to 3 percent slopes, gently undulating, rarely floodedSgB349715922442tgljla01520051:24000
Severn very fine sandy loam, 0 to 1 percent slopes, rarely floodedSvA929528057402v9rcla01720131:24000
Severn very fine sandy loam, 1 to 3 percent slopes, rarely floodedSvB575828057412ssxzla01720131:24000
Severn very fine sandy loam, 0 to 3 percent slopes, gently undulating, frequently floodedSxA467028057432tgllla01720131:24000
Severn very fine sandy loam, 1 to 3 percent slopes, gently undulating, occasionally floodedSwA257228057422v9rdla01720131:24000
Severn very fine sandy loam, occasionally floodedSe7689190312721wc6la06919831:24000
Severn very fine sandy loam, 0 to 3 percent slopes, gently undulating, frequently floodedSf451019031282tgllla06919831:24000
Severn very fine sandy loam, 0 to 3 percent slopes, gently undulating, frequently floodedSr650317206852tgllla08119731:24000
Severn very fine sandy loam, 1 to 3 percent slopes, gently undulating, occasionally floodedSn592917206842v9rdla08119731:24000
Severn very fine sandy loam, 0 to 1 percent slopes, rarely floodedSe135817206832v9rcla08119731:24000
Severn (udifluvents)Ud106917206871vrj1la08119731:24000
Severn very fine sandy loam, 0 to 3 percent slopes, gently undulating, frequently floodedSf3019038422tgllla12719911:24000
Severn fine sandy loam, 0 to 1 percent slopes, rarely flooded723122381857dtbzok01319741:24000
Severn very fine sandy loam, 0 to 1 percent slopes, rarely flooded4622315712382v9rcok02319771:24000
Severn very fine sandy loam, 0 to 1 percent slopes, rarely flooded63805571450m5mwok07919811:24000
Severn very fine sandy loam, 0 to 1 percent slopes, rarely floodedSg6565571182m5c7ok08919701:24000
Severn very fine sandy loam, 0 to 1 percent slopes, rarely flooded6271931064273kr4ok10119841:24000
Severn very fine sandy loam, 2 to 6 percent slopes, rarely flooded635461064283kr5ok10119841:24000
Severn very fine sandy loam, 0 to 1 percent slopes, occasionally floodedSevA4188384205dwsqok10719961:24000
Severn silt loam, 0 to 1 percent slopes, occasionally floodedSvnA2238384211dwsxok10719961:24000
Choska-Severn-Urban land complex, 0 to 1 percent slopes, rarely flooded8105891067413l28ok14319751:12000
Severn very fine sandy loam, 0 to 3 percent slopes, rarely flooded4962931067323l1zok14319751:12000
Severn very fine sandy loam, 0 to 1 percent slopes, rarely flooded38222755752842v9rctx03719781:20000
Severn silty clay loam395846575285m9mltx03719781:20000
Severn silt loam, 0 to 1 percent slopes, rarely floodedSe38973655472tglhtx14719891:24000
Severn very fine loam, 0 to 2 percent slopes425099393372f6bftx61419751:20000
Severn silty clay loam, 0 to 1 percent slopes, overwash433139393373f6bgtx61419751:20000
Severn-Kiomatia complex, 0 to 1 percent slopes, frequently flooded442468393374f6bhtx61419751:20000

Map of Series Extent

Approximate geographic distribution of the SEVERN 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 .