Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
102AUMN3101S1979MN067103 (3101)Wadenill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.284832,-95.0313873
103UMN2895S1978MN067141(2895)Wadenill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.313488,-94.7948227
103UMN3330S1980MN067107(3330)Wadenill2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0879898,-94.802063
103UMN4646S1992MN0934646Wadenill3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.2108917,-94.6456451

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the WADENILL series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the WADENILL series and siblings. 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 WADENILL 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 .

Click the image to view it full size.

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.

Competing Series

Soil series competing with WADENILL share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the WADENILL 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 WADENILL 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 .

Click the image to view it full size.

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 WADENILL, 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 WADENILL 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
Wadenill-Sunburg complex, 2 to 6 percent slopesL337B2991625366322n7zxmn06719831:20000
Sunburg-Wadenill complex, 6 to 12 percent slopes, moderately erodedL356C21451325366432n7zymn06719831:20000
Wadenill-Sunburg-Hawick complex, 2 to 6 percent slopesL340B368925366342n802mn06719831:20000
Sunburg-Wadenill complex, 12 to 18 percent slopes, moderately erodedL356D2316125366442n7zzmn06719831:20000
Sunburg-Wadenill-Hawick complex, 6 to 12 percent slopes, moderately erodedL315C2270425108362n803mn06719831:20000
Sunburg-Wadenill-Hawick complex, 6 to 12 percent slopes833C1365398724fcx2mn06719831:20000
Sunburg-Wadenill-Hawick complex, 18 to 35 percent slopesL315E96825108382n804mn06719831:20000
Sunburg-Wadenill-Hawick complex, 18 to 35 percent slopes833E769398726fcx4mn06719831:20000
Sunburg-Wadenill-Hawick complex, 12 to 18 percent slopes833D748398725fcx3mn06719831:20000
Sunburg-Wadenill-Hawick complex, 12 to 18 percent slopes, moderately erodedL315D267925108372n80fmn06719831:20000
Wadenill-Sunburg-Hawick complex, 2 to 6 percent slopes833B286398723fcx1mn06719831:20000
Wadenill loam, 2 to 6 percent slopesL353B791425366852n7zsmn09319961:20000
Wadenill-Sunburg complex, 2 to 6 percent slopesL337B502025366672n7zxmn09319961:20000
Sunburg-Wadenill complex, 6 to 12 percent slopes, moderately erodedL356C2373625366782n7zymn09319961:20000
Sunburg-Wadenill complex, 12 to 18 percent slopes, moderately erodedL356D278425366792n7zzmn09319961:20000
Wadenill-Sunburg-Hawick complex, 2 to 6 percent slopesL340B57525366692n802mn09319961:20000
Sunburg-Wadenill complex, 6 to 12 percent slopes, eroded805C2379436424gn46mn09319961:20000
Wadenill-Sunburg complex, 2 to 6 percent slopes1391B311436233gmy1mn09319961:20000
Sunburg-Wadenill-Hawick complex, 6 to 12 percent slopes, moderately erodedL315C226025366532n803mn09319961:20000
Wadenill loam, 2 to 6 percent slopes612B208436407gn3nmn09319961:20000
Sunburg-Wadenill complex, 12 to 18 percent slopes, eroded805D242436425gn47mn09319961:20000
Sunburg-Wadenill-Hawick complex, 12 to 18 percent slopes, moderately erodedL315D23325366542n80fmn09319961:20000
Wadenill-Sunburg complex, 2 to 6 percent slopesL337B6325367062n7zxmn14519801:15840
Sunburg-Wadenill complex, 12 to 18 percent slopes, moderately erodedL356D24425367152n7zzmn14519801:15840
Sunburg-Wadenill complex, 6 to 12 percent slopes, moderately erodedL356C21325367142n7zymn14519801:15840

Map of Series Extent

Approximate geographic distribution of the WADENILL 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 .