Official Series Description


Lab Data Summary

Aggregate lab data for the WORSHAM soil series. This aggregation is based on all pedons with a current taxon name of WORSHAM, 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 WORSHAM 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
n/a40A4058S1965NC167001WORSHAM6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WORSHAM 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 WORSHAM 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 WORSHAM 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 WORSHAM 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 WORSHAM 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 WORSHAM 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 WORSHAM 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 WORSHAM, 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-2010-09-28-07 | Rutherford County - 1997

    Typical relationship of soils, landform position, and parent material in the Cecil-Pacolet general soil map unit (Soil Survey of Rutherford County, North Carolina; 1997).

Map Units

Map units containing WORSHAM 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
Worsham sandy loamWb70412277543rhal01719571:20000
Worsham sandy loamWf25329309c1nwal05119481:20000
Worsham sandy loam, 2 to 6 percent slopesWoB12512429245bfga08919791:15840
Worsham sandy loam, very gently sloping phaseWcB29512438645fgga11719571:20000
Worsham sandy loam, level phaseWcA26512438545ffga11719571:20000
Worsham sandy loam, eroded very gently sloping phaseWcB225012438745fhga11719571:20000
Worsham sandy loam, severely eroded sloping phaseWcD319012438845fjga11719571:20000
Worsham sandy loam, 2 to 6 percent slopesWkB1690639986pgyqga13519661:15840
Worsham sandy loam, 0 to 2 percent slopesWkA410639985pgypga13519661:15840
Worsham coarse sandy loam, 2 to 6 percent slopesWoB18012475345t9ga19919601:15840
Worsham sandy loam, 2 to 6 percent slopesWkB2051249954623ga25519621:15840
Worsham soils, 2 to 6 percent slopesWmB3251250594645ga29719621:15840
Worsham silt loamWsl88012546746kbga61819661:15840
Worsham fine sandy loamWks580531379kty8ga62219671:20000
Worsham sandy loam, 2 to 6 percent slopesWkB37012550846lnga62319651:15840
Worsham sandy loamWo260012559346pdga62819771:20000
Worsham loam, 0 to 3 percent slopesWoA6071145753v6znc00719991:24000
Helena-Worsham complex 1 to 6 percent slopesHeB20611170683xtdnc04520001:24000
Worsham loam, 0 to 2 percent slopesWoA13251126703s7jnc07119851:24000
Worsham fine sandy loam, 0 to 2 percent slopesWoA14971136523t86nc10919891:24000
Worsham loam, 0 to 2 percent slopesWoA21641109293qfcnc12719841:24000
Helena-Worsham complex, 1 to 6 percent slopesHeB15971176293ydhnc16119971:24000
Worsham loam, 0 to 2 percentWoA9451176963ygnnc18119771:20000
Worsham loam, 1 to 4 percent slopesWoB8741300804cc4sc04719731:20000
Worsham fine sandy loamWo8821303494cmtsc05719671:20000
Chewacla and Worsham soilsCw28001303634cn8sc05919701:20000
Worsham loam, 1 to 4 percent slopesWoB4921307304d13sc06519731:20000
Worsham loam, 0 to 2 percent slopesWoA365639548pghlsc07120051:24000
Chewacla and Worsham soilsCw711314694dsysc08719701:20000
Worsham silt loam, 2 to 8 percent slopes31B126324207662m807va02520071:24000
Worsham soilsWo22401188043zmdva03719701:15840
Worsham soils, fragipan variantWr3931188053zmfva03719701:15840
Worsham fine sandy loam, 0 to 4 percent slopes6B55771189303zrgva04119741:15840
Creedmoor-Worsham sandy loams, 6 to 12 percent percent slopes202C2821188643zpbva04119741:15840
Creedmoor-Worsham sandy loams, 2 to 6 percent slopes202B191188633zp9va04119741:15840
Worsham loam, 0 to 4 percent slopes45B141515874581q8wbva04920051:24000
Worsham loamWr18524540472ncmtva06120061:12000
Worsham silt loamWf284412184842slva06519501:15840
Worsham sandy loamWe147012184742skva06519501:15840
Worsham fine sandy loam785320119184400nva08519761:15840
Worsham fine sandy loam, 2 to 7 percent slopesWoB7822119436408sva10919721:15840
Worsham loam, 0 to 4 percent slopes24B2076119466409rva11119791:20000
Worsham loam, 2 to 7 percent slopesWmB1238517067kc1lva11319671:15840
Worsham fine sandy loam, 1 to 6 percent slopesWoB1051911962740gyva11719901:24000
Helena-Worsham complex, 6 to 12 percent slopesHbC611011957540f8va11719901:24000
Worsham sandy loamWk633812193842whva13519561:20000
Worsham silt loamWl15112193942wjva13519561:20000
Worsham silt loam, 2 to 8 percent slopes931B624531602nbq6va13519561:20000
Worsham sandy loamWo5787120306415vva14719501:20000
Worsham loamWr68524535902nc52va15319851:15840
Worsham silt loamWo2048517479kcgwva15719581:20000
Worsham stony silt loamWs347517480kcgxva15719581:20000
Worsham loamWr276812058741gxva17919701:15840
Worsham soils, 0 to 4 percent slopesWoB587112079241pjva63119731:15840
Worsham silt loam, 2 to 8 percent slopes931B324818882p9lxva65319911:24000
Worsham-Urban land complex, 0 to 4 percent slopes47A261401264pt6va76020041:24000

Map of Series Extent

Approximate geographic distribution of the WORSHAM 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 .