Official Series Description


Lab Data Summary

Aggregate lab data for the DOWNSVILLE soil series. This aggregation is based on all pedons with a current taxon name of DOWNSVILLE, 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 DOWNSVILLE 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
14705N0628S2005WV037005Downsville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2352778,-77.8213889
14705N0629S2005WV037006Downsville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4936111,-77.7736111

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DOWNSVILLE 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 DOWNSVILLE 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 DOWNSVILLE 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 DOWNSVILLE 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 flats position figure.

Competing Series

Soil series competing with DOWNSVILLE 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 DOWNSVILLE 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 DOWNSVILLE 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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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 DOWNSVILLE, 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 DOWNSVILLE 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
Downsville silt loam, 3 to 8 percent slopesDvB76324011292llksmd00120091:12000
Downsville silt loam, 8 to 15 percent slopesDvC44724011302llktmd00120091:12000
Downsville silt loam, 0 to 3 percent slopesDvA29224011282llkrmd00120091:12000
Downsville-Urban land complex, 8 to 15 percent slopesDwC14824010202llg8md00120091:12000
Downsville-Urban land complex, 0 to 8 percent slopeDwB12324010192llg7md00120091:12000
Downsville gravelly loam, 8 to 15 percent slopesDoC554534799kyhlmd02120011:12000
Downsville gravelly loam, 3 to 8 percent slopesDoB319534802kyhpmd02120011:12000
Downsville gravelly loam, 3 to 8 percent slopesDoB3107534273kxymmd04319981:12000
Downsville gravelly loam, 8 to 15 percent slopesDoC3087534274kxynmd04319981:12000
Downsville gravelly loam, 15 to 25 percent slopesDoD1422534275kxypmd04319981:12000
Downsville gravelly loam, 25 to 45 percent slopesDoE142534276kxyqmd04319981:12000
Downsville gravelly loam, 0 to 3 percent slopesDoA31534272kxylmd04319981:12000
Downsville gravelly loam, 3 to 8 percent slopesDoB721545103l96zpa05519991:24000
Downsville gravelly loam, 8 to 25 percent slopesDoD93545104l970pa05519991:24000
Downsville gravelly loam, 3 to 8 percent slopesDsB1526516231kb5mwv00319971:24000
Downsville gravelly loam, 8 to 15 percent slopesDsC1164516232kb5nwv00319971:24000
Downsville gravelly loam, 15 to 25 percent slopesDsD184516233kb5pwv00319971:24000
Downsville gravelly loam, 8 to 15 percent slopesDsC159117102481vdn9wv0371:24000
Downsville gravelly loam, 15 to 25 percent slopesDsD116117102491vdnbwv0371:24000
Downsville gravelly loam, 3 to 8 percent slopesDsB59417102471vdn8wv0371:24000
Downsville gravelly loam, 25 to 35 percent slopesDsE17617102501vdncwv0371:24000
Downsville gravelly loam, 8 to 15 percent slopesDsC206555683ln78wv06520031:24000
Downsville gravelly loam, 3 to 8 percent slopesDsB183555682ln77wv06520031:24000

Map of Series Extent

Approximate geographic distribution of the DOWNSVILLE 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 .