Official Series Description


Lab Data Summary

Aggregate lab data for the DALEVILLE soil series. This aggregation is based on all pedons with a current taxon name of DALEVILLE, 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 DALEVILLE 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 DALEVILLE 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 DALEVILLE 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 DALEVILLE 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 DALEVILLE 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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Competing Series

Soil series competing with DALEVILLE 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 DALEVILLE 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 DALEVILLE 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 DALEVILLE, 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

No block diagrams are available.

Map Units

Map units containing DALEVILLE 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
Daleville-Quitman complex, 0 to 2 percent slopesDaA4260114754417j3kal02520041:24000
Daleville silt loam, pondedDaA518329772c24tal06520031:24000
Daleville and Smithton soils, 0 to 1 percent slopes, occasionally floodedDSA638329950202x5r3al09720181:24000
Smithton, Daleville and Bethera soils, occasionally ponded, 0 to 2 percent slopesSDA232529950762x5rfal09720181:24000
Daleville loam, frequently ponded, 0 to 2 percent slopesDaA180629950672x5r6al09720181:24000
Smithton, Daleville and Bethera soils, occasionally ponded, 0 to 2 percent slopesSNA2453726421322x5rfal12920131:24000
Daleville and Smithton soils, 0 to 1 percent slopes, occasionally floodedDSA470926420742x5r3al12920131:24000
Leaf silt loam (daleville)Lf1063332146c4mdms03119621:15840
Daleville silt loam, 0 to 1 percent slopes135588332555c51lms05919971:24000
Daleville loam, frequently ponded, 0 to 2 percent slopes1414813325562x5r6ms05919971:24000
Daleville-Jena association, 0 to 2 percent slopes, frequently floodedDJ57083327522tjlgms06919911:20000
Daleville sandy loam, 0 to 2 percent slopes, frequently floodedDa858332753301jfms06919911:20000
Daleville-Jena association, 0 to 2 percent slopes, frequently floodedDJ127143328792tjlgms07519801:20000
Daleville loam, 0 to 2 percent slopes, occasionally floodedDa9250332880301k3ms07519801:20000
Columbus-Daleville associationCD12434568216m28kms08919811:20000
Myatt very fine sandy loam (daleville) (0 to 2 percent slopes)Md1405333331c5vmms10119571:20000
Daleville silt loamDa110001297954c1ysc03519851:20000
Daleville variant loamDv16071315134dvcsc08919851:20000
Myatt loamMy6171382884mwxsc69019671:24000
Daleville silt loam, 0 to 2 percent slopes9A4935694811rb08va10119951:15840
Bethera and Daleville soils3123811964740hlva11919821:15840

Map of Series Extent

Approximate geographic distribution of the DALEVILLE 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 .