Official Series Description


Lab Data Summary

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

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 DEMOPOLIS 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 DEMOPOLIS 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 DEMOPOLIS 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 DEMOPOLIS, 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. AL-2010-02-25-01 | Wilcox County - March 1999

    Generalized patterns of soils, geomorphology, and landscape relationships in the Sucarnoochee-Congaree, Searcy-Freest, Demopolis-Watsonia, and Oktibbeha-Brantley general soil map units along Pine Barren Creek in the eastern part of Wilcox County (Soil Survey of Wilcox County, Alabama; 1999).

Map Units

Map units containing DEMOPOLIS 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
Demopolis-Watsonia complex, 2 to 8 percent slopesDwD104703284492wty7al01319961:20000
Demopolis-Brantley complex, 15 to 35 percent slopesDbF6450328448c0s3al01319961:20000
Demopolis silty clay loam, 3 to 12 percent slopes2311202329059c1dtal04719771:20000
Demopolis cobbly silty clay loam, 5 to 15 percent slopes241019329060c1dval04719771:20000
Demopolis-Sumter complex, 3 to 8 percent slopes, erodedDsD271663297572v5ltal06520031:24000
Demopolis-Sumter complex, 8 to 12 percent slopes, erodedDsE24232329758c24cal06520031:24000
Demopolis silty clay loam, 3 to 8 percent slopes, erodedDeD2882725104sbjgal06520031:24000
Sumter-Demopolis complex, 8 to 25 percent slopes, moderately erodedSpE2258025146492wwm6al08520111:24000
Demopolis-Brantley complex, 15 to 35 percent slopesDbF139225146522qdgcal08520111:24000
Demopolis-Watsonia complex, 2 to 8 percent slopesDwC120325146512wty7al08520111:24000
Demopolis silty clay loam, 3 to 8 percent slopes, erodedDeD214620330571c2zlal09119971:24000
Demopolis-Urban land complex, 0 to 8 percent slopesDuD1830330572c2zmal09119971:24000
Gullied land-Demopolis complex, 2 to 12 percent slopes, severely erodedGdE3240330576c2zral09119971:24000
Demopolis-Sumter complex, 3 to 8 percent slopes, erodedDsD246503312292v5ltal10519961:24000
Demopolis-Watsonia complex, 1 to 3 percent slopesDwB2700331230c3nval10519961:24000
Demopolis-Kipling complex, 3 to 20 percent slopes, moderately erodedDkE2731643314732tjlhal11919861:24000
Demopolis-Sumter complex, 1 to 3 percent slopesDsB13320331474c3xqal11919861:24000
Gullied land-Demopolis complex, 3 to 20 percent slopes, severely erodedGdE3685331476c3xsal11919861:24000
Demopolis-Watsonia complex, 2 to 8 percent slopesDwC139803316482wty7al13119971:24000
Sumter-Demopolis complex, 8 to 25 percent slopes, moderately erodedSpE2123203316762wwm6al13119971:24000
Demopolis channery silty clay loam, 3 to 12 percent slopes, severely eroded191863179350lymbar01919831:20000
Demopolis silty clay loam, gullied62204565681lzmsar05719761:20000
Demopolis silty clay, 3 to 12 percent slopes, severely erodedDeD33583565691lzn3ar06119701:24000
Demopolis silty clay loam, 3 to 20 percent slopes, eroded161487564888lyt6ar67019811:20000
Demopolis silty clay loam, 2 to 8 percent slopes, severely erodedDeC35655331881c4bvms01719691:20000
Demopolis-Kipling complex, 8 to 25 percent slopes, severely erodedDkE34552331882c4bwms01719691:20000
Gullied land-Demopolis complex, 8 to 25 percent slopesGdE3099331884c4byms01719691:20000
Chalk outcrop-Demopolis complex, 5 to 15 percent slopesCoD2208332084c4kdms02519741:20000
Sumter-Demopolis complex, 5 to 17 percent slopes, severely erodedSuE33786332798c59fms06919911:20000
Binnsville-Demopolis complex, 2 to 5 percent slopes, erodedBeB23406332750c57wms06919911:20000
Demopolis-Rock outcrop, chalk complex, 5 to 12 percent slopes, severely erodedDmD32525332754c580ms06919911:20000
Gullied land-Demopolis complex, 5 to 20 percent slopesGdE4711333009c5j7ms08119681:20000
Demopolis silty clay loam, 5 to 12 percent slopes, severely erodedDeD32125333007c5j5ms08119681:20000
Demopolis-Binnsville complex, 2 to 8 percent slopes, erodedDeC24142333065c5l1ms08719771:20000
Sumter-Demopolis-Chalk outcrop complex, 5 to 20 percent slopes, severely erodedSvD31595333105c5mbms08719771:20000
Demopolis-Binnsville complex, 2 to 8 percent slopes, erodedDeC26049333409c5y4ms10319831:20000
Sumter-Demopolis-Rock outcrop, chalk complex, 5 to 20 percent slopes, severely erodedSvE32081333458c5zqms10319831:20000

Map of Series Extent

Approximate geographic distribution of the DEMOPOLIS 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 .