Official Series Description


Lab Data Summary

Aggregate lab data for the DEERFORD soil series. This aggregation is based on all pedons with a current taxon name of DEERFORD, 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 DEERFORD 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
133AS92AL-023-192AL023001-pgmDeerford3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.185,-88.2052778
13497P04531997LA033002Deerford7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.4156952,-91.117775
13489P004988LA063002Deerford8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.4541664,-90.7455521

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DEERFORD 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 DEERFORD 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 DEERFORD 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 DEERFORD 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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Competing Series

Soil series competing with DEERFORD 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 DEERFORD 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 DEERFORD 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 DEERFORD, 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. LA-2012-02-01-03 | Richland Parish - September 1993

    Relationship of soils, landscape, and parent material in Richland Parish (Soil Survey of Richland Parish, Louisiana; September 1993).

  2. LA-2012-04-27-06 | Ascension Parish - August 1976

    Relationship of the soil associations to elevation and parent material, shown by a cross section from Donaldsonville to Port Vincent (Soil Survey of Ascension Parish, Louisiana; August 1976).

Map Units

Map units containing DEERFORD 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
McCrory-Deerford complex, 0 to 2 percent slopes, occasionally floodedMdA9880328608c0y8al02319981:24000
McCrory-Deerford complex, 0 to 2 percent slopes, occasionally floodedMdA1770600077n4fbal02520041:24000
Deerford-Verdun complex, 0 to 1 percent slopesDv872510146292wk4pla00519721:24000
Deerford-Patoutville complexDp37151014628131syla00519721:24000
Foley-Deerford complexFo29621014633131t3la00519721:24000
Deerford silt loamDa183817119271vgdgla00919811:24000
Deerford-Verdun complex, 0 to 1 percent slopesDaA249056083012wk4pla03320071:24000
Deerford silt loam, 0 to 2 percent slopesDe197616052571qwdhla03719921:24000
Deerford silt loamDf785417110921vfjjla04119791:24000
Deerford silt loamDa462116001611qq33la05919861:24000
Deerford silt loam, occasionally floodedDb375016001621qq34la05919861:24000
Deerford-Verdun complex, 0 to 1 percent slopesDv181675697392wk4pla06319871:24000
Deerford silt loamDa295917147671vkc2la08319881:24000
Deerford silt loam19139570375m4j6la12319751:24000
Calloway and Deerford soils, 0 to 2 percent slopes43A574331776c47gms00719971:24000
Bonn-Deerford associationBD2696567899m1ybms04919761:20000
Deerford-Bonn complex, 0 to 2 percent slopesDa2077567954m203ms05119971:20000
Deerford siltDe7102568076m241ms06319761:20000
McCrory-Deerford complex, 0 to 2 percent slopes, occasionally floodedMdA129224034322lnz2ms15320081:24000
Deerford complexDe756334646c771ms16119751:20000

Map of Series Extent

Approximate geographic distribution of the DEERFORD 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 .