Official Series Description


Lab Data Summary

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

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

Competing Series

Soil series competing with SULPHURA 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 SULPHURA 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 SULPHURA 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 SULPHURA, 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. KY-2012-01-26-08 | Allen County - September 1989

    Relationship of soils to topography and underlying material in the Trimblel-Bedford-Mountview general soil map unit (Soil Survey of Allen County, Kentucky; September 1989).

  2. TN-2010-11-02-07 | Dickson County -

    The relationship of soils and landscape in the Hawthorne-Sulphura-Sengtown and Wolftever-Beason-Melvin general soil map units (Soil Survey of Dickson County, Tennessee).

  3. TN-2010-11-02-14 | Lewis County - 2006

    Typical pattern of soils and parent material in the Biffle-Ironcity general soil map unit (Soil Survey of Lewis County, Tennessee; 2006).

  4. TN-2010-11-02-31 | Perry County - 2006

    Relationship of soils, parent material, and topography in the Paden-Ellisville-Woodmont general soil map unit (Soil Survey of Perry County, Tennessee; 2006).

  5. TN-2012-03-16-02 | Cheatham County - 2002

    Relationship of soils to topography and the underlying material in the Beason-Wolftever-Melvin-Arrington and Hawthorne-Sulphura-Sengtown general soil map units (Soil Survey of Cheatham County, TN; 2002).

  6. TN-2012-03-16-05 | Dickson County - 2002

    The relationship of soils, landscape, and parent material in the Hawthorne-Sulphura-Sengtown and the Wolftever-Beason-Melvin general soil map units (Soil Survey of Dickson County, TN; 2002).

  7. TN-2012-03-19-34 | Wayne County - 2000

    Typical pattern of soils and parent material in the Biffle-Sulphura-Ironcity general soil map unit (Soil Survey of Wayne County, TN; 2000).

  8. TN-2012-03-19-37 | Wayne County - 2000

    Typical pattern of soils and parent material in the Braxton-Talbott-Rock outcrop general soil map unit (Soil Survey of Wayne County, TN; 2000).

  9. TN-2012-03-19-38 | Williamson County - August 1964

    Major and minor soils and underlying parent materials in the Mountview-Baxter-Bodine association (Soil Survey of Williamson County, TN; 1964).

  10. TN-2012-03-19-39 | Williamson County - August 1964

    Major and minor soils and underlying parent materials in the Sulphura-Dellrose-Bodine association (Soil Survey of Williamson County, TN; 1964).

Map Units

Map units containing SULPHURA 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
Sulphura-Trimble complex, 20 to 50 percent slopesStE1545548769lf17ky00319861:20000
Hawthorne-Sulphura association, 20 to 60 percent slopesHsF673815270152v5c6tn02119911:24000
Bodine-Sulphura complex, 20 to 50 percent slopesBsE46618523409kkn5tn03719771:15840
Hawthorne-Sulphura association, 20 to 60 percent slopesHsF374755271082v5c6tn04319931:24000
Dandridge-Needmore complex, 12 to 35 percent slopes (Sulphura)DaF7341327544bztytn07119611:15840
Dandridge-Needmore complex, 8 to 12 percent slopes (Sulphura)DaD515327543bztxtn07119611:15840
Hawthorne-Sulphura association, 20 to 60 percent slopesHsF101135274672v5c6tn08119971:24000
Sulphura cherty silt loam, steep phaseSe2056527685kq33tn09919551:20000
RocklandRb1488527680kq2ytn09919551:20000
Sulphura cherty silt loam, eroded steep phaseSf914527686kq34tn09919551:20000
Sulphura cherty silt loam, eroded moderately steep phaseSd568527684kq32tn09919551:20000
Biffle-Sulphura-Rock outcrop association, very steepBOF79143530847ktd3tn10119991:24000
Sulphura channery silt loam, 25 to 55 percent slopesSuF84415277232v5cmtn11119921:24000
Biffle, Hawthorne, and Sulphura soils, very steep, rockyBSF64445560604ltc0tn13520001:24000
Sulphura channery silt loam, 25 to 55 percent slopesSpF3955606512v5cmtn13520001:24000
Sulphura-Rock outcrop complex, 30 to 75 percent slopesSuF60560652ltdktn13520001:24000
Sulphura channery silt loam, 25 to 55 percent slopesSUF404995283812v5cmtn16519931:20000
Sulphura channery silt loam, 10 to 25 percent slopesSuD80515283882v5cltn16519931:20000
Sulphura channery silt loam, 25 to 55 percent slopesSUF19535300392v5cmtn16919931:24000
Sulphura channery silt loam, 20 to 60 percent slopesSuF19910328049c0c7tn18119961:24000
Sulphura-Rock outcrop complex, 30 to 75 percent slopesSxF11345328050c0c8tn18119961:24000
Sulphura channery silt loam, 25 to 55 percent slopesSuE72125235872v5cmtn18719611:15840
Sulphura cherty silt loam, 20 to 50 percent slopes, severely erodedSuE3872523588kktytn18719611:15840
Sulphura channery silt loam, 10 to 25 percent slopesSuD2585235862v5cltn18719611:15840

Map of Series Extent

Approximate geographic distribution of the SULPHURA 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 .