Official Series Description


Lab Data Summary

Aggregate lab data for the WINNSBORO soil series. This aggregation is based on all pedons with a current taxon name of WINNSBORO, 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 WINNSBORO 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 WINNSBORO 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 WINNSBORO 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 WINNSBORO 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 WINNSBORO 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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Click the image to view it full size.

Competing Series

Soil series competing with WINNSBORO 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 WINNSBORO 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 WINNSBORO 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.

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 WINNSBORO, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. NC-2012-02-07-14 | Gaston County - May 1989

    The relationship of soils, landscape, and geology in the Gaston-Winnsboro-Cecil map unit (Soil Survey of Gaston County, North Carolina; May 1989).

  2. NC-2012-02-07-28 | Lincoln County - January 1995

    Relationship of soils and parent material in the Gaston-Pacolet-Cecil general soil map unit (Soil Survey of Lincoln County, North Carolina; January 1995).

Map Units

Map units containing WINNSBORO 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
Wynott-Winnsboro complex, 6 to 15 percent slopes, very stonyWyD2470189575221mp9al03720061:24000
Wynott-Winnsboro complex, 6 to 15 percent slopes, very stonyWnD161014764611lkcsal12320051:24000
Wynott-Wilkes-Winnsboro complex, 15 to 30 percent slopes, stonyWyE1401018616135ylga03520031:24000
Wynott-Wilkes-Winnsboro complex, 6 to 15 percent slopes, stonyWyD901018615135ykga03520031:24000
Wynott-Wilkes-Winnsboro complex, 6 to 15 percent slopesWnD711022005742cvw8ga20720071:24000
Wynott-Wilkes-Winnsboro complex, 15 to 30 percent slopesWnE378022005752cvw9ga20720071:24000
Wynott-Winnsboro-Mecklenburg complex, 6 to 15 percent slopes, very stonyWoD37522005762cvwbga20720071:24000
Wynott-Winnsboro-Sedgefield complex, 2 to 6 percent slopes, very stonyWsB8522005772cvwcga20720071:24000
Winnsboro-Wynott complex, 15 to 30 percent slopes, very stonyWmE1522005732cvw7ga20720071:24000
Wynott-Wilkes-Winnsboro complex, 15 to 25 percent slopesWyE204526390972rj4sga63920121:24000
Winnsboro-Wilkes complex, 2 to 8 percent slopesWwB12181126303s67nc06919971:24000
Winnsboro-Wilkes complex, 8 to 15 percent slopesWwD8971126313s68nc06919971:24000
Winnsboro-Wilkes complex, 15 to 30 percent slopesWwE3141126323s69nc06919971:24000
Winnsboro loam, 2 to 8 percent slopesWnB25201126683s7gnc07119851:24000
Winnsboro loam, 8 to 15 percent slopesWnD9211126693s7hnc07119851:24000
Winnsboro fine sandy loam, 2 to 8 percent slopesWnB4621136513t85nc10919891:24000
Wynott-Winnsboro-Rowan complex, 15 to 25 percent slopesWyD45224251722mdlcnc10919891:24000
Wynott-Winnsboro-Rowan complex, 8 to 15 percent slopesWyC42824251712mdlbnc10919891:24000
Winnsboro sandy loam, 6 to 10 percent slopesWnC119101322134fkysc02319771:20000
Winnsboro sandy loam, 2 to 6 percent slopesWnB82551322124fkxsc02319771:20000
Winnsboro sandy loam, 10 to 25 percent slopesWnE71801322144fkzsc02319771:20000
Winnsboro fine sandy loam, 2 to 6 percent slopesWnB33091298944c54sc03719781:20000
Winnsboro fine sandy loam, 6 to 10 percent slopesWnC14141298954c55sc03719781:20000
Winnsboro fine sandy loam, 10 to 15 percent slopesWnD7841298964c56sc03719781:20000
Winnsboro sandy loam, 6 to 10 percent slopesWnC212701299394c6lsc03919771:20000
Winnsboro sandy loam, 2 to 6 percent slopesWnB133451299384c6ksc03919771:20000
Winnsboro sandy loam, 10 to 25 percent slopesWnE94001299404c6msc03919771:20000
Winnsboro loam, 2 to 6 percent slopesWnB423943752lcjxsc05719671:20000
Wynott-Winnsboro complex, 6 to 10 percent slopes, moderately erodedWyC213664639554pghssc07120051:24000
Wynott-Winnsboro complex, 2 to 6 percent slopes, moderately erodedWyB27281639553pghrsc07120051:24000
Winnsboro sandy loam, 2 to 6 percent slopesWnB4335639547pghksc07120051:24000
Winnsboro sandy clay loam, 7 to 15 percent slopes, moderately eroded23C2302714595511kzs9sc07120051:24000
Winnsboro sandy clay loam, 15 to 25 percent slopes, moderately eroded23D2202814595501kzs8sc07120051:24000
Winnsboro sandy loam, 2 to 7 percent slopes22B67414595451kzs3sc07120051:24000
Winnsboro sandy clay loam, 2 to 7 percent slopes, moderately eroded23B253614595521kzsbsc07120051:24000
Winnsboro sandy loam, 7 to 15 percent slopes22C39914595531kzscsc07120051:24000
Winnsboro sandy clay loam, 15 to 25 percent slopes, severely eroded24D31914595491kzs7sc07120051:24000
Efland silt loam, 2 to 6 percent slopesEfB81401311734dhdsc08119601:20000
Efland silt loam, 6 to 10 percent slopesEfC18351311744dhfsc08119601:20000
Wynott-Winnsboro complex, 6 to 10 percent slopes, moderately erodedWyC21467125138792lq56sc09120131:15840
Wynott-Winnsboro complex, 2 to 6 percent slopes, moderately erodedWyB2754325138782lq53sc09120131:15840
Wynott-Winnsboro complex, 10 to 15 percent slopes, moderately erodedWyD2543425138802lq58sc09120131:15840
Winnsboro loam, 6 to 10 percent slopesWnC8601302464cjhsc61019851:20000
Winnsboro loam, 2 to 6 percent slopesWnB7761302454cjgsc61019851:20000
Winnsboro sandy loam, 2 to 7 percent slopes22B80591181283yxlva00719941:24000
Winnsboro sandy loam, 7 to 15 percent slopes22C58771181293yxmva00719941:24000

Map of Series Extent

Approximate geographic distribution of the WINNSBORO 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 .