Official Series Description


Lab Data Summary

Aggregate lab data for the WINTERGREEN soil series. This aggregation is based on all pedons with a current taxon name of WINTERGREEN, 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 WINTERGREEN 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 WINTERGREEN 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 WINTERGREEN 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 WINTERGREEN 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 WINTERGREEN 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 WINTERGREEN 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 WINTERGREEN series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the WINTERGREEN 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.

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 WINTERGREEN, 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 WINTERGREEN 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
Wintergreen loam, 2 to 7 percent slopes46B52411367844lbdva00920041:24000
Wintergreen loam, 7 to 15 percent slopes46C50321367864lbgva00920041:24000
Wintergreen clay loam, 7 to 15 percent slopes, severely eroded45C34151367824lbbva00920041:24000
Wintergreen clay loam, 2 to 7 percent slopes, severely eroded45B15831367814lb9va00920041:24000
Wintergreen clay loam, 15 to 25 percent slopes, severely eroded45D7031367834lbcva00920041:24000
Wintergreen loam, 7 to 15 percent slopes, very stony47C6821367874lbhva00920041:24000
Wintergreen loam, 15 to 25 percent slopes46D5071367884lbjva00920041:24000
Wintergreen loam, 15 to 25 percent slopes, very stony47D2991367894lbkva00920041:24000
Wintergreen loam, 2 to 7 percent slopes, very stony47B2081367854lbfva00920041:24000
Wintergreen fine sandy loam, 2 to 7 percent slopes33B37071359762xx71va01919851:24000
Wintergreen fine sandy loam, 7 to 15 percent slopes33C26551359772xx73va01919851:24000
Wintergreen fine sandy loam, 15 to 25 percent slopes33D2551359782xx72va01919851:24000
Wintergreen clay loam, 2 to 7 percent slopes, severely eroded45B3124224794742p731va02920101:24000
Wintergreen clay loam, 7 to 15 percent slopes, severely eroded45C394524794762p733va02920101:24000
Yadkin and Wintergreen loams, 2 to 15 percent slopesHtC7985192312yztsva03519651:15840
Yadkin and Wintergreen fine sandy loams, 2 to 15 percent slopesHvC4275192352yztxva03519651:15840
Yadkin and Wintergreen loams, 15 to 25 percent slopesHtD3685192322yzttva03519651:15840
Yadkin and Wintergreen cobbly fine sandy loams, 7 to 15 percent slopesHuC2675192332yztvva03519651:15840
Yadkin and Wintergreen cobbly fine sandy loams, 15 to 25 percent slopesHuD2065192342yztwva03519651:15840
Yadkin and Wintergreen loams, 2 to 7 percent slopesHtB2065192302yztrva03519651:15840
Wintergreen loam, 2 to 7 percent slopes44B39415874571q8w9va04920051:24000
Wintergreen loam, 8 to 15 percent slopes39C6702582050mjntva06720041:24000
Thurmont-Wintergreen complex, 8 to 15 percent slopes36C2278582042mjnkva06720041:24000
Wintergreen loam, 2 to 8 percent slopes39B2101582049mjnsva06720041:24000
Wintergreen loam, 15 to 25 percent slopes39D1661582051mjnvva06720041:24000
Thurmont-Wintergreen complex, 2 to 8 percent slopes36B248582041mjnjva06720041:24000
Thurmont-Urban land-Wintergreen complex, 8 to 15 percent slopes35C218582040mjnhva06720041:24000
Thurmont-Wintergreen complex, 15 to 25 percent slopes36D172582043mjnlva06720041:24000
Wintergreen loam, 7 to 15 percent slopes52C44761371334lpnva12519921:24000
Wintergreen loam, 2 to 7 percent slopes52B42081371324lpmva12519921:24000
Wintergreen clay loam, 7 to 15 percent slopes, severely eroded53C26131371364lprva12519921:24000
Wintergreen loam, 15 to 25 percent slopes52D11081371344lppva12519921:24000
Wintergreen clay loam, 2 to 7 percent slopes, severely eroded53B10521371354lpqva12519921:24000
Wintergreen clay loam, 15 to 25 percent slopes, severely eroded53D10161371374lpsva12519921:24000
Wintergreen loam, 7 to 15 percent slopes, very stony54C1671371394lpvva12519921:24000
Wintergreen loam, 8 to 15 percent slopes77C22125148892qddzva16320101:24000
Wintergreen loam, 15 to 35 percent slopes, very stony78E19925148922qdf2va16320101:24000
Wintergreen loam, 15 to 25 percent slopes77D13725148902qdf0va16320101:24000
Wintergreen loam, 25 to 35 percent slopes77E8025148912qdf1va16320101:24000
Wintergreen loam, 2 to 7 percent slopes60B4023738032kp49va51520081:24000
Wintergreen loam, 7 to 15 percent slopes60C423738042kp4bva51520081:24000
Wintergreen loam, 8 to 15 percent slopes97C2325252762qm2cva6061:24000
Wintergreen loam, 15 to 25 percent slopes97D1925252772qm2dva6061:24000
Wintergreen loam, 15 to 35 percent slopes, very stony41E2631740962z3g1va8501:24000

Map of Series Extent

Approximate geographic distribution of the WINTERGREEN 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 .