Official Series Description


Lab Data Summary

Aggregate lab data for the CARVILLE soil series. This aggregation is based on all pedons with a current taxon name of CARVILLE, 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 CARVILLE 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
131A01N0364S2000LA095002Carville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.0767231,-90.4743729
131A02N0335S2002LA095003Carville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.0686798,-90.4638977

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CARVILLE 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 CARVILLE 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 CARVILLE 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 CARVILLE 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 CARVILLE 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 CARVILLE 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 CARVILLE 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 CARVILLE, 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 CARVILLE 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
Carville and Cancienne soils, gently undulating, frequently floodedCNA817194769523cqwla03320071:24000
Fausse-Carville associationFC16508824181wnmhla04519731:24000
Carville and Schriever soils, undulating, frequently floodedCN36511014380131jyla04519731:24000
Hydraquents, Carville, and Glenwild soils, undulating, floodedGW2657824206wnn9la04519731:24000
Carville soils, undulating, frequently floodedCe5431014381131jzla04519731:24000
Carville silt loam, undulatingCd148114513491kq7qla04719751:24000
Cancienne and Carville soils, undulating, frequently floodedCg125914513661kq88la04719751:24000
Carville soils, undulating, frequently floodedCF97014513651kq87la04719751:24000
Cancienne and Carville soils, frequently floodedCR514134511jft6la05119811:24000
Carville, Cancienne, and Schriever soils, frequently floodedCV1344515986551qnjjla07519881:24000
Carville silt loam, 0 to 1 percent slopesCt68915986582w9wzla07519881:24000
Cancienne and Carville soils, frequently floodedCR8324375466dlptla08919841:24000
Carville silt loam, 0 to 1 percent slopesCvA430914157952w9wzla09320071:24000
Carville and Cancienne soils, gently undulating, frequently floodedCT221914157941jj7sla09320071:24000
Cancienne and Carville soils, gently undulating, frequently floodedCT6944576993mcdpla09520041:24000
Carville silt loam, 0 to 1 percent slopesCvA65495792642w9wzla09520041:24000
Carville-Barbary associationCH17860824141wnl6la09919741:24000
Carville soils, undulating, frequently floodedCR692714516841kqljla09919741:24000
Hydraquents, Carville, and Glenwild soils, undulating, floodedGW3519824168wnm2la09919741:24000
Carville and Schriever soils, undulating, frequently floodedCN122414526671krm7la09919741:24000
Hydraquents, Carville, and Glenwild soils, undulating, floodedHYA13773740598svn8la10119991:24000
Carville and Hydraquents soils, undulating, floodedCvA12096378493dpvgla10119991:24000

Map of Series Extent

Approximate geographic distribution of the CARVILLE 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 .