Official Series Description


Lab Data Summary

Aggregate lab data for the WIMPER soil series. This aggregation is based on all pedons with a current taxon name of WIMPER, 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 WIMPER 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 WIMPER 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 WIMPER 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 WIMPER 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 WIMPER 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 flats position figure.

Competing Series

Soil series competing with WIMPER 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 WIMPER 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 WIMPER 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 flats position figure.

Soil series sharing subgroup-level classification with WIMPER, 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 WIMPER 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
Wimper loam, 2 to 8 percent slopes423C31476124ylpmt60919711:24000
Wimper-Winspect complex, 4 to 8 percent slopes129C18115456555tzmt61620031:24000
Wimper-Winspect complex, 15 to 35 percent slopes129E14215456655v0mt61620031:24000
Wimper-Rock outcrop-Castner complex 15 to 50 percent slopes902F44324098912lwpfmt61719581:20000
Wimper cobbly silt loam, 4 to 15 percent slopes95D25124098772lwnzmt61719581:20000
Wimper gravelly silt loam, 15 to 30 percent slopes90E11224098862lwp8mt61719581:20000
Wimper-Castner complex, 8 to 30 percent slopes901E1524098892lwpcmt61719581:20000
Wimper-Rock outcrop-Castner complex 15 to 50 percent slopes902F395614524831krf9mt61820081:24000
Finleypoint-Haskillpass-Wimper complex, 8 to 30 percent slopes541E1678613445nlbkmt61820081:24000
Wimper cobbly silt loam, 4 to 15 percent slopes95D102116535381shmymt61820081:24000
Wimper gravelly silt loam, 15 to 30 percent slopes90E89014524861krfdmt61820081:24000
Finleypoint-Wimper complex, 4 to 15 percent slopes543D286805745w1fsmt61820081:24000
Castner-Wimper-Rock outcrop complex, 15 to 50 percent slopes761F27818828912169fmt61820081:24000
Wimper-Castner complex, 8 to 30 percent slopes901E25914524851krfcmt61820081:24000
Wimper-Finleypoint-Haskillpass complex, 8 to 30 percent slopes491E226802742vy9xmt61820081:24000
Wimper-Finleypoint-Haskillpass complex, 2 to 8 percent slopes491C118802859vyfpmt61820081:24000
Wimper-Rock outcrop-Castner complex 15 to 50 percent slopes902F74224099592lwrmmt61919881:24000
Castner-Wimper-Rock outcrop complex, 15 to 50 percent slopes761F16324099552lwrhmt61919881:24000
Wimper-Winspect complex, 15 to 35 percent slopes129E13871441914v1bmt62119971:24000
Wimper-Winspect cobbly loams, 15 to 35 percent slopes229E3761442784v44mt62119971:24000
Wimper-Winspect complex, 8 to 15 percent slopes129D1951441904v19mt62119971:24000
Wimper-Winspect complex, 35 to 60 percent slopes129F581441924v1cmt62119971:24000
Wimper loam, 2 to 4 percent slopes29B551443214v5jmt62119971:24000
Wimper gravelly loam, 15 to 35 percent slopes29E481443244v5mmt62119971:24000
Wimper loam, 4 to 8 percent slopes29C361443224v5kmt62119971:24000
Wimper loam, 8 to 15 percent slopes29D281443234v5lmt62119971:24000
Shawmut, very stony-Meagher, stony-Wimper complex, 4 to 15 percent slopes705D70124870752ph07mt62420211:24000
Beenom, stony-Wimper-Whitlash, very stony, complex, 4 to 15 percent slopes311D731151025524smt62719981:24000
Wimper-Whitlash association, 35 to 60 percent slopes426F609151080526kmt62719981:24000
Wimper-Wimper, stony, complex, 15 to 45 percent slopes424E605151078526hmt62719981:24000
Beenom, stony-Wimper-Whitlash, very stony, complex, 15 to 45 percent slopes311F551151026524tmt62719981:24000
Wimper loam, 15 to 35 percent slopes423E247151076526fmt62719981:24000
Wimper-Wimper, stony, complex, 4 to 15 percent slopes424D215151077526gmt62719981:24000
Wimper loam, 8 to 15 percent slopes423D211151075526dmt62719981:24000
Wimper gravelly loam, 8 to 35 percent slopes, stony425E121151079526jmt62719981:24000
Wimper loam, 2 to 8 percent slopes423C114151074526cmt62719981:24000
Wimper gravelly loam, 8 to 35 percent slopes, stony, moist1356E5615060051q2mt62719981:24000
Wimper-Wimper, stony, complex, 15 to 35 percent slopes, warm1355E2315059951q1mt62719981:24000
Wimper-Wimper, stony, complex, 4 to 15 percent slopes, warm1355D1915059851q0mt62719981:24000
Castner-Wimper-Rock outcrop complex, 15 to 50 percent slopes761F11624099142lwq5mt62919911:20000
Whitecow-Wimper loams, 8 to 15 percent slopes220D27424380352mtz9mt63819851:24000
Wimper very gravelly loam, 15 to 35 percent slopes189E26824380312mtz5mt63819851:24000
Hilger-Wimper-Azaar complex, 4 to 15 percent slopes219D26424380342mtz8mt63819851:24000
Farnuf-Bitterroot-Subwell complex, 15 to 40 percent slopes104E14024226052m9xkmt63819851:24000
Meagher-Subwell complex, 8 to 15 percent slopes101D5424226032m9xhmt63819851:24000
Burnt Fork-Subwell complex, 8 to 15 percent slopes201D4724226312m9ydmt63819851:24000
Subwell-Burnt Fork complex, 8 to 15 percent slopes100D1924226022m9xgmt63819851:24000
Subwell-Burnt Fork complex, 4 to 8 percent slopes100C1724226012m9xfmt63819851:24000
Farnuf-Bitterroot-Wimper complex, 15 to 40 percent slopes104E370215852559yqmt64520131:12000
Burnt Fork-Wimper-Fairway complex, 1 to 35 percent slopes201E310213895661hmyqmt64520131:12000
Farnuf-Wimper-Whitlash, rubbly complex, 15 to 45 percent slopes540F2901633728p8fvmt64520131:12000
Quast-Wimper complex, 15 to 35 percent slopes550E2114633733p8g0mt64520131:12000
Wimper-Burnt Fork complex, 4 to 8 percent slopes100C187015851659yfmt64520131:12000
Farnuf-Wimper complex, 8 to 15 percent slopes540D14681585835b0lmt64520131:12000
Wimper-Quast complex, 8 to 15 percent slopes550D12491585795b0gmt64520131:12000
Wimper sandy loam, 0 to 4 percent slopes105B1157633470p85jmt64520131:12000
Losttrail-Wimper complex, 0 to 4 percent slopes102B1101633468p85gmt64520131:12000
Losttrail-Wimper complex, 4 to 8 percent slopes102C89615851059y7mt64520131:12000
Wimper gravelly loam, 0 to 4 percent slopes103B877633469p85hmt64520131:12000
Meagher-Wimper complex, 8 to 15 percent slopes101D69615851259y9mt64520131:12000
Wimper-Losttrail complex, 4 to 8 percent slopes103C62515850859y5mt64520131:12000
Burnt Fork-Wimper complex, 8 to 15 percent slopes201D6011586455b2lmt64520131:12000
Wimper-Burnt Fork complex, 8 to 15 percent slopes100D52515851559ydmt64520131:12000
Wimper-Farnuf complex, 2 to 8 percent slopes540C5001585845b0mmt64520131:12000
Meagher-Wimper complex, wet, 4 to 15 percent slopes125D423633587p899mt64520131:12000
Wimper-Quast complex, 2 to 8 percent slopes550C3621585805b0hmt64520131:12000
Meagher-Wimper complex, wet, 15 to 25 percent slopes125E21815853459z0mt64520131:12000
Shawmut, very stony-Wimper, extremely bouldery-Gnojek, bouldery complex, 4 to 35 percent slopes3511E3585695978rc6xmt6691:24000
Corbly, extremely stony-Wimper, extremely stony - Shawmut, very stony complex, 8 to 35 percent slopes3510E287415648657tymt6691:24000
Martinsdale-Wimper, extremely stony-Turner complex, 0 to 8 percent slopes3518C1644697276rdksmt6691:24000
Wimper-Meagher-Windham extremely bouldery complex, 8 to 45 percent slopes5635E1416699331rgq2mt6691:24000
Winspect-Corpening-Wimper complex, 4 to 40 percent slopes441031709752z206wy6291:24000

Map of Series Extent

Approximate geographic distribution of the WIMPER 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 .