Official Series Description


Lab Data Summary

Aggregate lab data for the KEMPSVILLE soil series. This aggregation is based on all pedons with a current taxon name of KEMPSVILLE, 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 KEMPSVILLE 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
152AS23_0191990-FL045-S23_019Kempsville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.1949997,-85.1736145
n/a78P0313S1978VA159065Kempsville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KEMPSVILLE 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 KEMPSVILLE 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 KEMPSVILLE 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 KEMPSVILLE 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 KEMPSVILLE 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 KEMPSVILLE 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 KEMPSVILLE 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 mountains figure.

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

Soil series sharing subgroup-level classification with KEMPSVILLE, 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 KEMPSVILLE 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
Kempsville fine sandy loam, 5 to 10 percent slopes, severely erodedKeC3187412831749j8md03719751:20000
Kempsville fine sandy loam, 5 to 10 percent slopes, moderately erodedKeC2184512831649j7md03719751:20000
Kempsville fine sandy loam, 10 to 15 percent slopes, severely erodedKeD3103312831949jbmd03719751:20000
Kempsville fine sandy loam, 10 to 15 percent slopes, moderately erodedKeD265512831849j9md03719751:20000
Kempsville-Emporia complex, 2 to 6 percent slopes11B7446212103241y8va03319961:24000
Kempsville-Emporia-Remlik complex, 15 to 50 percent slopes10E6337412103441ybva03319961:24000
Slagle-Kempsville complex, 2 to 15 percent slopes21C4423512105841z3va03319961:24000
Kempsville-Emporia complex, 6 to 10 percent slopes11C2214112103341y9va03319961:24000
Kempsville-Emporia complex, 0 to 2 percent slopes11A375712103141y7va03319961:24000
Emporia-Kempsville complex, 2 to 6 percent slopes23B34691178433ymdva03619931:24000
Kempsville loamy sand, 2 to 6 percent slopes25B8141178463ymhva03619931:24000
Kempsville-Bourne complex, 2 to 6 percent slopes82B81151189353zrmva04119741:15840
Kempsville-Bourne complex, 6 to 12 percent slopes82C3191189363zrnva04119741:15840
Kempsville sandy loam, 2 to 6 percent slopes10B1254212147642dlva05719851:20000
Kempsville sandy loam, 0 to 2 percent slopes10A251312147542dkva05719851:20000
Kempsville sandy loam, 6 to 10 percent slopes10C79112147742dmva05719851:20000
Kempsville fine sandy loam, 2 to 6 percent slopes13B102761189453zryva07319781:15840
Kempsville fine sandy loam, 0 to 2 percent slopes13A6231189443zrxva07319781:15840
Kempsville-Bourne fine sandy loams, 2 to 7 percent slopes40B62701191183zyjva08519761:15840
Kempsville gravelly fine sandy loam, 2 to 7 percent slopes39B26501191133zycva08519761:15840
Kempsville-Remlik complex, 7 to 15 percent slopes69C243011916530nznva08519761:15840
Kempsville-Remlik complex, 15 to 25 percent slopes69D170011916630nzmva08519761:15840
Kempsville gravelly fine sandy loam, 7 to 15 percent slopes39C6401191143zydva08519761:15840
Kempsville-Bourne fine sandy loams, 0 to 2 percent slopes40A4901191173zyhva08519761:15840
Kempsville very fine sandy loam, clayey substratum, 0 to 2 percent slopesKgA7794119247402pva08719731:15840
Kempsville very fine sandy loam, clayey substratum, 2 to 6 percent slopesKgB2789119248402qva08719731:15840
Kempsville fine sandy loam, 2 to 6 percent slopesKeB1064119242402jva08719731:15840
Kempsville fine sandy loam, 0 to 2 percent slopesKeA637119241402hva08719731:15840
Kempsville fine sandy loam, flooded, 2 to 6 percent slopesKfB349119246402nva08719731:15840
Kempsville fine sandy loam, 10 to 25 percent slopes, erodedKeD2314119244402lva08719731:15840
Kempsville fine sandy loam, flooded, 0 to 2 percent slopesKfA279119245402mva08719731:15840
Kempsville fine sandy loam, 2 to 10 percent slopes, erodedKeC2269119243402kva08719731:15840
Kempsville very fine sandy loam, clayey substratum, 6 to 10 percent slopes, erodedKgC2152119249402rva08719731:15840
Kempsville sandy loam, 2 to 6 percent slopes13B13054694676r9vxva10119951:15840
Kempsville sandy loam, 0 to 2 percent slopes13A357694674r9vvva10119951:15840
Kempsville loamy fine sand, thick surface, 0 to 2 percent slopesKtA238011948740bfva11519601:20000
Kempsville fine sandy loam, 0 to 2 percent slopesKeA102011948540bcva11519601:20000
Kempsville fine sandy loam, 2 to 5 percent slopesKeB21711948640bdva11519601:20000
Kempsville sandy loam, 2 to 6 percent slopes9B638811965740hxva11919821:15840
Kempsville sandy loam, 0 to 2 percent slopes9A62711965640hwva11919821:15840
Kempsville-Emporia complex, 2 to 6 percent slopes19B1053611966940j9va12719851:15840
Kempsville-Suffolk complex, 2 to 6 percent slopes20B227811967240jdva12719851:15840
Kempsville fine sandy loam, 2 to 6 percent slopes17B139611966740j7va12719851:15840
Kempsville-Emporia complex, 6 to 10 percent slopes19C74011967040jbva12719851:15840
Kempsville gravelly fine sandy loam, 2 to 6 percent slopes18B37611966840j8va12719851:15840
Kempsville fine sandy loam, nearly levelKeA371311974540lrva13319601:20000
Kempsville fine sandy loam, gently slopingKeB324211974640lsva13319601:20000
Kempsville fine sandy loam, gently sloping, erodedKeB275111974740ltva13319601:20000
Kempsville fine sandy loam, sloping, erodedKeC224611974840lvva13319601:20000
Kempsville fine sandy loam, sloping, severely erodedKeC312011974940lwva13319601:20000
Kempsville gravelly fine sandy loam, 2 to 7 percent slopes14B1081120181411tva14519841:15840
Kempsville fine sandy loam, gravelly substratum, 6 to 10 percent slopes, erodedKfC224624535712nc4gva15319851:15840
Kempsville fine sandy loam, gravelly substratum, 2 to 6 percent slopesKfB8824535702nc4fva15319851:15840
Kempsville sandy loam, 2 to 6 percent slopes6B32471203764183va15919801:20000
Kempsville loam723821203774184va15919801:20000
Kempsville gravelly sandy loam, 7 to 15 percent slopes25C28961204094195va17719801:15840
Kempsville gravelly sandy loam, 2 to 7 percent slopes25B4111204084194va17719801:15840
Kempsville gravelly sandy loam, 15 to 25 percent slopes25D2131204104196va17719801:15840
Kempsville fine sandy loam, gravelly substratum, 2 to 6 percent slopesKfB380812053141f3va17919701:15840
Kempsville fine sandy loam, gravelly substratum, 6 to 10 percent slopes, erodedKfC2213812053241f4va17919701:15840
Kempsville fine sandy loam, gravelly substratum, 10 to 18 percent slopes, erodedKfD2152512053341f5va17919701:15840
Kempsville fine sandy loam, 2 to 6 percent slopesKeB107012053041f2va17919701:15840
Kempsville fine sandy loam, 0 to 2 percent slopesKeA39012052941f1va17919701:15840
Kempsville fine sandy loam, 2 to 6 percent slopes18B141512251943h7va18119971:24000
Kempsville loam, 2 to 6 percent slopes7B1153812061941hyva19319801:20000
Kempsville loam, 0 to 2 percent slopes7A586912061841hxva19319801:20000
Kempsville gravelly sandy loam, 2 to 7 percent slopes25B22623764082krvbva63020081:12000
Kempsville gravelly sandy loam, 7 to 15 percent slopes25C6523764092krvcva63020081:12000
Kempsville-Emporia fine sandy loams, 2 to 6 percent slopes19B853212080941q2va69519811:15840
Kempsville fine sandy loam, 2 to 6 percent slopes18B205812080841q1va69519811:15840
Kempsville-Urban land complex, 2 to 6 percent slopes22B331400314pq4va76020041:24000
Kempsville-Bourne-Urban land complex, 2 to 6 percent slopes23B101399894pnsva76020041:24000

Map of Series Extent

Approximate geographic distribution of the KEMPSVILLE 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 .