Official Series Description


Lab Data Summary

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

There are insufficient data to create the 3D mountains figure.

There are insufficient data to create the 3D terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with WINIFRED, 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 WINIFRED 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
Winifred clay, 4 to 25 percent slopes49D9308500930jt81co66619741:31680
Winifred clay, 25 to 65 percent slopes49E3423500931jt82co66619741:31680
Winifred silty clay loam, 4 to 15 percent slopes128D1421342077cgyrmt02519911:24000
Winifred-Windham-Eltsac complex, 15 to 45 percent slopes27554396342518chdzmt02719791:24000
Roy-Winifred complex, 8 to 45 percent slopes19524972342429chb3mt02719791:24000
Bitton-Winifred-Castner complex, 15 to 60 percent slopes2422972342479chcqmt02719791:24000
Doney-Winifred-Wayden complex, 15 to 45 percent slopes7019626342573chgrmt02719791:24000
Winifred-Judith clay loams, 8 to 15 percent slopes27316079342516chdxmt02719791:24000
Winifred-Judith clay loams, 4 to 8 percent slopes27213067342515chdwmt02719791:24000
Winifred clay loam, 2 to 8 percent slopes27011729342513chdtmt02719791:24000
Winifred-Castner-Norbert complex, 8 to 45 percent slopes2719483342514chdvmt02719791:24000
Gerber-Winifred clay loams, 2 to 8 percent slopes1108008342336ch73mt02719791:24000
Linwell-Winifred clay loams, 4 to 8 percent slopes1534807342383ch8mmt02719791:24000
Winifred-Linwell clay loams, 8 to 15 percent slopes2744529342517chdymt02719791:24000
Alder-Winifred clay loams, 15 to 45 percent slopes163331342390ch8vmt02719791:24000
Amor-Winifred complex, 8 to 15 percent slopes211409342446chbnmt02719791:24000
Bitton-Winifred-Castner complex, 15 to 60 percent slopes295F530344560ckjvmt06519961:24000
Winifred-Utica complexWn399511474634yfwmt60219631:20000
Winifred clay loam, 4 to 8 percent slopesWc233451474574yfpmt60219631:20000
Winifred-Judith clay loamsWk72981474614yftmt60219631:20000
Winifred clay loam, 8 to 15 percent slopesWd72531474584yfqmt60219631:20000
Winifred clay loam, 0 to 4 percent slopesWb61261474564yfnmt60219631:20000
Winifred cobbly clay loam, 2 to 8 percent slopesWf34121474594yfrmt60219631:20000
Winifred cobbly clay loam, 8 to 15 percent slopesWh29691474604yfsmt60219631:20000
Winifred-Rhoades clay loamsWm28241474624yfvmt60219631:20000
Winifred-Yawdim clay loams, 15 to 50 percent slopes2196236341889cgrpmt61319751:24000
Winifred clay loam, 2 to 8 percent slopes2173752341887cgrmmt61319751:24000
Winifred clay loam, 8 to 15 percent slopes2182507341888cgrnmt61319751:24000
Linwell-Winifred clay loams, 15 to 45 percent slopes623F9701346863cmy4mt61519921:24000
Wayden-Amherst-Winifred complex, 8 to 45 percent slopes432E362149997512mmt63920001:24000
Winifred clay loam, 2 to 8 percent slopes254C33314981650wsmt63920001:24000
Cabba-Winifred clay loams, 2 to 8 percent slopes181C26714971550sjmt63920001:24000
Farnuf-Winifred complex, 2 to 8 percent slopes193C5214973450t4mt63920001:24000
Cabba-Winifred clay loams, 8 to 15 percent slopes181D4014971650skmt63920001:24000
Kiev-Winifred-Vanda complex, 0 to 15 percent slopes784C12256348798cpykmt65719901:24000
Linwell-Winifred clay loams, 2 to 15 percent slopes179C3447348402cpjsmt65719901:24000
Winifred-Wayden-Cabba complex, 2 to 15 percent slopes285C2664348535cpp2mt65719901:24000
Wayden-Cabba-Winifred complex, 15 to 45 percent slopes187F1931348411cpk2mt65719901:24000
Bitton-Winifred-Castner complex, 15 to 60 percent slopes295F145015316621ndtgmt66620081:24000
Winifred-Castner-Norbert complex, 8 to 45 percent slopes471E100515316821ndv3mt66620081:24000
Winifred-Windham-Eltsac complex, 15 to 45 percent slopes475E13015316831ndv4mt66620081:24000

Map of Series Extent

Approximate geographic distribution of the WINIFRED 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 .