Official Series Description


Lab Data Summary

Aggregate lab data for the HANCEVILLE soil series. This aggregation is based on all pedons with a current taxon name of HANCEVILLE, 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 HANCEVILLE 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
12978P008277AL117001Hanceville4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.0050694,-86.5808528

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HANCEVILLE 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 HANCEVILLE 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 HANCEVILLE 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 HANCEVILLE 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 HANCEVILLE 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 HANCEVILLE 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 HANCEVILLE 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 HANCEVILLE, 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 HANCEVILLE 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
Hanceville loam, 2 to 6 percent slopesHcB755328370c0plal00919741:24000
Hanceville loam, 6 to 10 percent slopesHcC735328371c0pmal00919741:24000
Hanceville loam, 2 to 6 percent slopes, erodedHaB220153289012sr6val04319601:20000
Hanceville loam, 6 to 10 percent slopes, erodedHaC2337328902c17ral04319601:20000
Hanceville loam, 2 to 6 percent slopes, erodedHaB24553294632sr6val05719631:15840
Hanceville fine sandy loam, rolling phaseHno875522906kk3yal07119431:24000
Hanceville fine sandy loam, undulating phaseHnu750522907kk3zal07119431:24000
Hanceville fine sandy loam, eroded, rolling phaseHnn226522905kk3xal07119431:24000
Hanceville fine sandy loam, eroded, undulating phaseHne74522904kk3wal07119431:24000
Hanceville fine sandy loam, 8 to 15 percent slopes221260329920c29lal07319801:24000
Hanceville-Urban land complex, 2 to 8 percent slopes23560329921c29mal07319801:24000
Hanceville fine sandy loam, eroded, undulatingHb1244331081c3j1al10319491:15840
Hanceville fine sandy loam, eroded, rollingHa1179331080c3j0al10319491:15840
Hanceville loam, severely eroded, rollingHd793331083c3j3al10319491:15840
Hanceville fine sandy loam, undulatingHc389331082c3j2al10319491:15840
Hanceville loam, 6 to 15 percent slopesHvD470331442c3wpal11719821:24000
Hanceville loam, 6 to 15 percent slopesHcD1180562915lwrkga64820011:12000
Hanceville-Urban land complex, 2 to 15 percent slopesHnC505562939lwsbga64820011:12000
Hanceville loam, 2 to 6 percent slopesHcB475562912lwrgga64820011:12000
Hanceville loam, 15 to 30 percent slopesHcE265562916lwrlga64820011:12000
Hanceville loam, 25 to 40 percent slopesHcE938101786313559tn06519801:15840
Hanceville loam, 12 to 25 percent slopesHcD152101786213558tn06519801:15840

Map of Series Extent

Approximate geographic distribution of the HANCEVILLE 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 .