Official Series Description


Lab Data Summary

Aggregate lab data for the DEXTER soil series. This aggregation is based on all pedons with a current taxon name of DEXTER, 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 DEXTER 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
131AM92143021992MO143002Dexter4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.607193,-89.5463028
131A40A4387S1958AR147001Dexter6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.1713905,-91.2330551
13489P063389LA037093Dexter7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.8199997,-90.957222
13440A1345S1963LA083004DEXTER4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3491669,-91.7827759
13440A1344S1963LA083005DEXTER7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.3161125,-91.8697205

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DEXTER 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 DEXTER 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 DEXTER 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 DEXTER 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 hills figure.

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 DEXTER 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 DEXTER series and competing. 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 DEXTER 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 .

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

Soil series sharing subgroup-level classification with DEXTER, 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-2012-04-27-03 | Franklin Parish - August 1981

    Soils, parent material, and landscape position from east to west in the parish (Soil Survey of Franklin Parish, Louisiana; August 1981).

  3. MS-2012-04-27-03 | Sunflower County - February 1959

    East-west cross section, 2 miles south of Doddsville, showing relation of soils to topography (Soil Survey of Sunflower County, Mississippi; February 1959).

  4. MS-2012-04-27-10 | Bolivar County - December 1958

    Soil associations in Bolivar County: 1. Alluvial soils; 2. Commerce-Robinsonville-Crevasse; 3. Forestdale-Dundee-Bosket; 4. Brittain-Pearson-Dexter; 5. Dowling-Alligator-Sharkey (Soil Survey of Bolivar County, Mississippi; December 1958).

Map Units

Map units containing DEXTER 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
Dexter silt loam, gently undulating2313718564055lxybar02119751:20000
Dexter silt loam, undulatingDeU6989565800lzrmar06719711:20000
Dexter silt loam, 0 to 1 percent slopesDe3313565799lzrlar06719711:20000
Dexter very fine sandy loam, 1 to 3 percent slopesDrB1702577021mcflla03320071:24000
Dexter silt loam, 1 to 3 percent slopesDx81216052581qwdjla03719921:24000
Dexter silt loamDh690217110931vfjkla04119791:24000
Dexter-Foley complex, gently undulatingDk418517110941vfjlla04119791:24000
Dexter very fine sandy loam, 1 to 3 percent slopesDx1647569740m3vqla06319871:24000
Dexter silt loam, 3 to 5 percent slopesDx933569786m3x6la06719811:24000
Dexter silt loam, 1 to 3 percent slopesDe1612917147691vkc4la08319881:24000
Dexter silt loam, 3 to 5 percent slopesDf250917147701vkc5la08319881:24000
Dexter silt loam, 0 to 1 percent slopesDd222217147681vkc3la08319881:24000
Dexter very fine sandy loam, 1 to 5 percent slopesDx125717216321vshjla09119911:24000
Dexter silt loam, 1 to 3 percent slopes41514570379m4jbla12319751:24000
Dexter silt loam, 0 to 3 percent slopes (dubbs)Da1505567482m1hwms01119561:20000
Dexter silt loam, 3 to 7 percent slopes (dubbs)Db452567483m1hxms01119561:20000
Dexter silt loam, 0 to 3 percent slopes (dubbs)Da435568456m2j9ms13319561:20000
Bosket silt loam (Dexter)Bs1379566769m0rwtn04519631:15840
Dexter clay loam, 8 to 12 percent slopes, severely erodedDcD3841327547bzv1tn07119611:15840
Dexter clay loam, 5 to 8 percent slopes, severely erodedDcC3719327546bzv0tn07119611:15840
Dexter loam, 5 to 8 percent slopes, erodedDeC2422327549bzv3tn07119611:15840
Dexter loam, 8 to 12 percent slopesDeD347327550bzv4tn07119611:15840
Dexter loam, 2 to 5 percent slopes, erodedDeB2260327548bzv2tn07119611:15840
Dexter clay loam, 2 to 5 percent slopes, severely erodedDcB3188327545bztztn07119611:15840
Dexter fine sandy loam, eroded gently sloping phaseDd734327705c004tn07719551:20000
Dexter silt loam, eroded gently sloping phaseDg693327708c007tn07719551:20000
Dexter fine sandy clay loam, severely eroded sloping phaseDb553327703c002tn07719551:20000
Dexter silty clay loam, severely eroded sloping phaseDl437327711c00btn07719551:20000
Dexter silt loam, sloping phaseDh180327709c008tn07719551:20000
Dexter fine sandy clay loam, severely eroded sloping phaseDc145327704c003tn07719551:20000
Dexter fine sandy clay loam, severely eroded gently sloping phaseDa141327702c001tn07719551:20000
Dexter silty clay loam, severely eroded sloping phaseDm112327720c00mtn07719551:20000
Dexter fine sandy loam, eroded sloping phaseDe103327706c005tn07719551:20000
Dexter silt loam, eroded gently sloping phaseDk73327710c009tn07719551:20000
Dexter fine sandy loam, eroded sloping phaseDf32327707c006tn07719551:20000

Map of Series Extent

Approximate geographic distribution of the DEXTER 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 .