Official Series Description


Lab Data Summary

Aggregate lab data for the WADLEY soil series. This aggregation is based on all pedons with a current taxon name of WADLEY, 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 WADLEY 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
133AS71AL-025-871AL025008-pgmWadley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.6355609893799,-87.607780456543
133AS99AL-065-499AL065004-pgmWadley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.9772222,-87.4752778
138S12_0081979-FL023-S12_008Wadley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.026556,-82.5734787
138S12_0151980-FL023-S12_015Wadley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9786148,-82.5799179
138S63_0041985-FL125-S63_004Wadley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties29.9507141,-82.4970932
153AS02_0081988-FL003-S02_008Wadley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.3494034,-82.1284561

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WADLEY 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 WADLEY 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 WADLEY 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 WADLEY 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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Click the image to view it full size.

Competing Series

Soil series competing with WADLEY 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 WADLEY 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 WADLEY 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 WADLEY, 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-2012-04-24-02 | Clarke County - August 2006

    Generalized patterns of soils and geomorphology and landscape relationships in general soil map units 2—Iuka-Bibb-Harleston, 6—Lucedale-Bama-Smithdale, 8—Smithdale-Wadley-Boykin, 9—Smithdale-Flomaton-Wadley, 10—Prim-Suggsville-Brantley, and 11—Okeelala-Brantley-Smithdale. The area illustrated is along Bassett Creek in the northeastern part of Clarke County, Alabama (Soil Survey of Clarke County, Alabama; August 2006).

Map Units

Map units containing WADLEY 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
Heidel-Wadley complex, 15 to 30 percent slopesHeE3321231162112z46zal00119721:20000
Heidel-Wadley complex, 5 to 15 percent slopesHeD1930131162122z470al00119721:20000
Heidel-Wadley complex, 2 to 8 percent slopesHeC642232720382zkvwal00119721:20000
Wadley loamy fine sand, 0 to 5 percent slopesEuB2957631217262x59mal00319611:20000
Wadley loamy fine sand, 5 to 8 percent slopesEuC74913281302x5qfal00319611:20000
Wadley-Heidel complex, 8 to 15 percent slopesEuD20023281312x5qdal00319611:20000
Wadley-Smithdale-Boykin complex, 5 to 20 percent slopesWdE564522471442ffbjal00720071:24000
Wadley-Boykin complex, 15 to 35 percent slopesWbF141522471412ffbfal00720071:24000
Wadley loamy fine sand, 1 to 5 percent slopesWaB2100328566c0wxal02319981:24000
Wadley-Smithdale complex, 15 to 35 percent slopesWsF657306000452wtz1al02520041:24000
Maubila-Wadley-Smithdale complex, 8 to 30 percent slopesMbF49630600074n4f7al02520041:24000
Flomaton-Smithdale-Wadley complex, 10 to 25 percent slopesFaE21580600099n4g1al02520041:24000
Wadley loamy sand, 1 to 5 percent slopesWaB2600600095n4fxal02520041:24000
Wadley-Smithdale-Boykin complex, 5 to 20 percent slopesWbD6242725102sbjdal06520031:24000
Wadley-Boykin complex, 15 to 35 percent slopesWbF487725098sbj8al06520031:24000
Wadley loamy sand, 0 to 5 percent slopesWaB166329770c24ral06520031:24000
Boykin-Wadley complex, 15 to 30 percent slopesBpE18950330562c2z9al09119971:24000
Wadley loamy fine sand, 5 to 15 percent slopesWdD10520330607c30ral09119971:24000
Wadley loamy fine sand, 0 to 5 percent slopesWaB4997129950292x59mal09720181:24000
Wadley-Heidel complex, 8 to 15 percent slopesWhD4713929950272x5qdal09720181:24000
Wadley-Heidel complex, 15 to 25 percent slopesWhE3946229950642x5r1al09720181:24000
Wadley-Heidel complex, 2 to 8 percent slopesWhC1614629950632x5r0al09720181:24000
Wadley loamy fine sand, 5 to 8 percent slopesWaC1541129950282x5qfal09720181:24000
Wadley-Urban land complex, 0 to 8 percent slopesWuC1524629950302x5qgal09720181:24000
Wadley-Urban land complex, 8 to 15 percent slopesWuD454229950312x5qhal09720181:24000
Wadley-Boykin-Smithdale complex, 15 to 35 percent slopesWbF429526421492rrx6al12920131:24000
Wadley-Boykin-Smithdale complex, 5 to 15 percent slopesWbD404326421482rrx5al12920131:24000
Wadley loamy fine sand, 0 to 5 percent slopesWaB136226421472x59mal12920131:24000
Penney-Wadley complex, 0 to 5 percent slopes16399514210861jprhfl02919981:24000
Wadley fine sand, 0 to 5 percent slopes135180321796bsvjfl04119891:20000
Wadley sand, 0 to 5 percent slopes181940114881317kfhfl04719951:24000
Wadley sand, 5 to 12 percent slopes17580114881217kfgfl04719951:24000
Wadley-Toinette-Smithdale association, 12 to 40 percent slopesEsF1985631217412z24jms02319631:15840
Wadley-Heidel complex, 8 to 15 percent slopesEsD27713319872x5qdms02319631:15840
Wadley loamy fine sand, 5 to 8 percent slopesEsC22903319862x5qfms02319631:15840
Wadley loamy fine sand, 0 to 5 percent slopesEsB58031217272x59mms02319631:15840
Wadley-Toinette-Smithdale association, 12 to 40 percent slopesEsF1119031217402z24jms03119621:15840
Wadley loamy fine sand, 5 to 8 percent slopesEsC4043321332x5qfms03119621:15840
Wadley loamy fine sand, 0 to 5 percent slopesEsB14031217282x59mms03119621:15840
Wadley-Heidel complex, 8 to 15 percent slopesEsD1343321342x5qdms03119621:15840
Wadley loamy fine sand, 5 to 8 percent slopesTrB2403322422x5qfms03519761:20000
Wadley loamy fine sand, 0 to 5 percent slopesEsB1530631217292x59mms03919671:20000
Wadley-Heidel complex, 8 to 15 percent slopesEsE74643322632x5qdms03919671:20000
Wadley loamy fine sand, 5 to 15 percent slopesEsD643331217232z3t2ms03919671:20000
Wadley-Boykin-Smithdale complex, 5 to 15 percent slopesWbD507126422532rs3yms04120121:24000
Wadley loamy fine sand, 0 to 5 percent slopesWaB329026422522x59mms04120121:24000
Wadley loamy fine sand, 5 to 15 percent slopesEuD100031217242z3t2ms04120121:24000
Wadley-Boykin-Smithdale complex, 15 to 35 percent slopesWbF27326422542rs3zms04120121:24000
Wadley loamy fine sand, 0 to 5 percent slopesEuB43831217302x59mms04519791:20000
Wadley and Poarch soils, 8 to 17 percent slopesEuE841031217222z3t3ms04719711:20000
Wadley loamy fine sand, 0 to 5 percent slopesEtB188231217312x59mms04719711:20000
Wadley loamy fine sand, 0 to 5 percent slopes841286631217322x59mms05919971:24000
Wadley loamy fine sand, 5 to 15 percent slopes17299131217252z3t2ms05919971:24000
Wadley-Heidel complex, 8 to 15 percent slopes189913325592x5qdms05919971:24000
Wadley loamy fine sand, 0 to 5 percent slopesEaB78731217332x59mms07519801:20000
Wadley loamy fine sand, 5 to 8 percent slopesTaB37213335682x5qfms10919801:20000
Wadley fine sand, 0 to 5 percent slopesWdC2577333628c656ms11119971:20000
Wadley fine sand, 5 to 15 percent slopesWdE1866333629c657ms11119971:20000
Wadley loamy fine sand, 5 to 8 percent slopes408823341352x5qfms13119971:24000
Wadley-Heidel complex, 8 to 15 percent slopes97823341662x5qdms13119971:24000
Wadley loamy fine sand, 0 to 5 percent slopes1037731217342x59mms13119971:24000
Wadley-Boykin-Smithdale complex, 5 to 15 percent slopesWsD620124034742lp0fms15320081:24000
Wadley fine sand, 0 to 5 percent slopesWaB85624034732lp0dms15320081:24000

Map of Series Extent

Approximate geographic distribution of the WADLEY 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 .