Official Series Description


Lab Data Summary

Aggregate lab data for the WURTSMITH soil series. This aggregation is based on all pedons with a current taxon name of WURTSMITH, 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 WURTSMITH 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
91B95P0311S1994WI129010WURTSMITH6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.9000015,-91.7102814

Water Balance

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

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Click the image to view it full size.

Soil series sharing subgroup-level classification with WURTSMITH, 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 WURTSMITH 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
Wurtsmith-Meehan sands, 0 to 8 percent slopes305B26614554441kvhtmi00320071:24000
Wurtsmith-Deford complex, 0 to 6 percent slopes298B22614554331kvhgmi00320071:24000
Meehan-Tawas-Wurtsmith complex, 0 to 12 percent slopes438C37361918776fnlmi06919951:15840
Wurtsmith sand, 0 to 6 percent slopes383B22791918446fmjmi06919951:15840
Wurtsmith-Meehan sands, 0 to 6 percent slopes432B12001918706fncmi06919951:15840
Wurtsmith-Meehan-Urban land complex, 0 to 6 percent slopes446B11041918876fnxmi06919951:15840
Wurtsmith-Meehan-Deer Park sands, 0 to 18 percent slopes437D5901918756fnjmi06919951:15840
Wurtsmith-Tawas-Deford complex, 0 to 6 percent slopes86B584714570291kx4ymi15320071:24000
Wurtsmith-Duck-Rubicon complex, 0 to 15 percent slopes492D332714569501kx2dmi15320071:24000
Shuberts-Wurtsmith-Meehan complex, 0 to 6 percent slopes56B78814570041kx44mi15320071:24000
Wurtsmith-Meehan complex, 0 to 4 percent slopesB58B202726534312pg47mn00719911:24000
Wurtsmith-Meehan complex, 1 to 8 percent slopesD73B557625104142lvb9mn03520091:24000
Graycalm-Wurtsmith complex, 2 to 8 percent slopesD72B326025104132lvb6mn03520091:24000
Wurtsmith-Meehan-Beach complex, 1 to 8 percent slopesD74B167825104152ndr8mn03520091:24000
Wurtsmith loamy sand, map 22-30, 0 to 3 percent slopes14446076436549gn87mn05719981:24000
Wurtsmith-Grettum complex, 0 to 3 percent slopesC44A43116734891t5djmn06520061:12000
Wurtsmith-Meehan complex, lake beach, 1 to 3 percent slopesC121A89116764481t8gzmn09520061:12000
Wurtsmith-Grettum complex, 0 to 3 percent slopesC44A9216763901t8f3mn09520061:12000
Wurtsmith loamy sand, map 22-30, 0 to 3 percent slopes14444361394885f7x7mn13519991:24000
Wurtsmith-Friendship complex, 1 to 4 percent slopesA3B3482510828wm8ymn61320161:24000
Wurtsmith-Friendship complex, MLRA 93, 1 to 4 percent slopesF41B5324077222ltfgmn61320161:24000
Wurtsmith-Friendship complex, MLRA 93, 1 to 4 percent slopesF41B373186143420gz8mn61720071:24000
Wurtsmith-Meehan complex, 0 to 4 percent slopesB58B144186149620h18mn61720071:24000
Wurtsmith-Meehan complex, 0 to 4 percent slopesB58B2227194686123bvzmn61920091:24000
Wurtsmith-Friendship complex, 1 to 4 percent slopesA3B2273822893wm8ymn62120061:24000
Wurtsmith-Friendship complex, MLRA 93, 1 to 4 percent slopesF41B69515368011nl57mn62120061:24000
Wurtsmith-Meehan complex, 0 to 4 percent slopesB58B508823064wmggmn62120061:24000
Wurtsmith-Meehan complex, 0 to 4 percent slopesB58B1908329438572pg47mn62520151:24000
Wurtsmith-Friendship complex, mlra 93A, 1 to 4 percent slopesF41B41329438452pg12mn62520151:24000
Wurtsmith sand, beaches, 0 to 3 percent slopes598A20614445861kh6kwi00320061:12000
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes396B20879448340h1jlwi01320041:12000
Wurtsmith loamy sand, 0 to 3 percent slopes3126A4604448188h1cpwi01320041:12000
Wurtsmith sand, 0 to 3 percent slopes896A223656114q0qzwi01320041:12000
Wurtsmith sand, 0 to 3 percent slopes896A457781520v77bwi03120051:12000
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes396B423781213v6xfwi03120051:12000
Wurtsmith loamy sand, 0 to 3 percent slopes3126A224781101v6stwi03120051:12000
Wurtsmith sand, 0 to 3 percent slopesWuA4229395881f8ycwi07819981:12000
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes396B17824276862mh6gwi09519781:15840
Wurtsmith loamy sand, 0 to 3 percent slopes3126A3724276842mh6dwi09519781:15840
Wurtsmith loamy sand, 0 to 3 percent slopes3126A172114814891lqlzwi10720061:12000
Wurtsmith loamy sand, 0 to 3 percent slopes3126A58816699531t1qgwi11320061:12000
Wurtsmith loamy sand, 0 to 3 percent slopes3126A3638723601s8yzwi12920021:12000
Friendship-Wurtsmith-Grayling complex, 0 to 6 percent slopes396B216435507gm5mwi12920021:12000

Map of Series Extent

Approximate geographic distribution of the WURTSMITH 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 .