Official Series Description


Lab Data Summary

Aggregate lab data for the KIRKVILLE soil series. This aggregation is based on all pedons with a current taxon name of KIRKVILLE, 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 KIRKVILLE 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
133AS46_0121996-FL091-S46_012Kirkville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.6907082,-86.6195984

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the KIRKVILLE 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 KIRKVILLE 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 KIRKVILLE 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 KIRKVILLE 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 KIRKVILLE 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 KIRKVILLE 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 KIRKVILLE 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with KIRKVILLE, 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 KIRKVILLE 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
Kirkville loam12810330613c30yal09319761:20000
Kirkville sandy loam, 0 to 3 percent slopes, occasionally floodedKrB655324354282mr86al13320121:24000
Kirkville fine sandy loam, occasionally flooded3354833179256lymvar05919831:20000
Kirkville loam, occasionally flooded419323331771c479ms00719971:24000
Mantachie and Kirkville soilsMa1726331812c48mms00919721:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKr11693318082shs5ms00919721:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKk48193319282shs5ms01919821:20000
Kirkville fine sandy loam, frequently floodedKr330331929c4ddms01919821:20000
Mantachie, Bibb, and Iuka soils (kirkville, kinston, iuka)Mn31002332011c4h1ms02319631:15840
Mantachie soils, local alluviumMc6884332010c4h0ms02319631:15840
Mantachie fine sandy loam (kirkville)Ma4451332009c4gzms02319631:15840
Kirkville-Mantachie associationKR11745332462c4ylms05719751:20000
Jena-Kirkville associationJK10786332460c4yjms05719751:20000
Kirkville, Mantachie and Mooreville soilsKT9362332463c4ymms05719751:20000
Kirkville-Mantachie complexKk14894332629c53zms06119741:20000
Kirkville-Jena association, frequently floodedKR11860332628c53yms06119741:20000
Kirkville and Mantachie soils, frequently floodedKm12300332675c55gms06519721:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKr7123327622shs5ms06919911:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, frequently floodedKv589332763301jjms06919911:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally flooded1331743328122shs5ms07119791:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKa125863328852shs5ms07519801:20000
Kirkville-Bibb complex, 0 to 2 percent slopes, frequently floodedKb9431332886301k4ms07519801:20000
Kirkville-Bibb association, 0 to 2 percent slopes, frequently floodedKK8687332884301k5ms07519801:20000
Jena-Kirkville-Kinston complex, 0 to 5 percent slopes, frequently floodedJkB2024416035512tjlpms07920081:24000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKr24873329752shs5ms07920081:24000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKr154213332652shs5ms09919791:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKv21033338102shs5ms11719951:24000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally flooded7149303338792shs5ms12119841:20000
Jena-Kirkville-Kinston complex, 0 to 5 percent slopes, frequently floodedJkB836724264702tjlpms12320091:24000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKr224424264662mfy3ms12320091:24000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKr86473339622shs5ms12719931:20000
Kirkville fine sandy loam, 0 to 2 percent slopes, occasionally floodedKr112523340512shs5ms12919971:20000
Kirkville loamKr5736334232c6spms14119801:20000
Jena-Kirkville complex, occasionally floodedJk3674334597c75gms15919971:24000

Map of Series Extent

Approximate geographic distribution of the KIRKVILLE 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 .