Official Series Description


Lab Data Summary

Aggregate lab data for the CANCIENNE soil series. This aggregation is based on all pedons with a current taxon name of CANCIENNE, 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 CANCIENNE 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
131A02N033302LA093001Cancienne CmA TPCancienne7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.0601111,-90.6076472
131A97P045797LA005002Cancienne7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.1708056,-90.9853056

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CANCIENNE 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 CANCIENNE 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 CANCIENNE 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 CANCIENNE 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 hills figure.

There are insufficient data to create the 3D mountains figure.

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Competing Series

Soil series competing with CANCIENNE 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 CANCIENNE 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 CANCIENNE 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 CANCIENNE, 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 CANCIENNE 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
Cancienne silt loam, 0 to 1 percent slopesCmA4111014145002s8sqla00719761:24000
Cancienne silty clay loam, 0 to 1 percent slopesCnA1018914145012qr6xla00719761:24000
Cancienne silt loam, 0 to 1 percent slopesCmA67686097592s8sqla03320071:24000
Carville and Cancienne soils, gently undulating, frequently floodedCNA817194769523cqwla03320071:24000
Cancienne silt loam, 0 to 1 percent slopesCa1209514513462s8sqla04719751:24000
Cancienne silty clay loam, 0 to 1 percent slopesCb957714513472qr6xla04719751:24000
Cancienne silt loam, 0 to 1 percent slopesCm1017814134382s8sqla05119811:24000
Cancienne silty clay loam, 0 to 1 percent slopesCo528214134312qr6xla05119811:24000
Cancienne and Schriever soils, frequently floodedCS110214134321jfslla05119811:24000
Cancienne and Carville soils, frequently floodedCR514134511jft6la05119811:24000
Cancienne silt loam, 0 to 1 percent slopesCm380388085152s8sqla05719811:24000
Cancienne silty clay loam, 0 to 1 percent slopesCo225188085162qr6xla05719811:24000
Gramercy-Cancienne silty clay loams, 0 to 1 percent slopesGcA459808519w4b8la05719811:24000
Cancienne silty clay loam, 0 to 1 percent slopes, occasionally floodedCeA120808513w4b2la05719811:24000
Cancienne silt loam, 0 to 1 percent slopes, occasionally floodedCfA92808514w4b3la05719811:24000
Cancienne silt loam, 0 to 1 percent slopesCm48055698842s8sqla07119871:24000
Cancienne silty clay loam, 0 to 1 percent slopesCo23825698852qr6xla07119871:24000
Cancienne and Schriever soils, frequently floodedCS546569883m40bla07119871:24000
Carville, Cancienne, and Schriever soils, frequently floodedCV1344515986551qnjjla07519881:24000
Cancienne silty clay loam, 0 to 1 percent slopesCo766215986572qr6xla07519881:24000
Cancienne silt loam, 0 to 1 percent slopesCm344315986562s8sqla07519881:24000
Cancienne silt loam, 0 to 1 percent slopesCm33293753522s8sqla08719841:24000
Cancienne silty clay loam, 0 to 1 percent slopesCo33003753532qr6xla08719841:24000
Cancienne and Schriever soils, frequently floodedCS536375351dll3la08719841:24000
Cancienne silt loam, 0 to 1 percent slopesCc92153754672s8sqla08919841:24000
Cancienne and Carville soils, frequently floodedCR8324375466dlptla08919841:24000
Cancienne silty clay loam, 0 to 1 percent slopesCm75833754682qr6xla08919841:24000
Cancienne silty clay loam, frequently floodedCn4844375469dlpxla08919841:24000
Cancienne-Harahan-Allemands complex, drainedCo1481375470dlpyla08919841:24000
Cancienne silt loam, 0 to 1 percent slopesCmA1936214157922s8sqla09320071:24000
Cancienne silty clay loam, 0 to 1 percent slopesCnA692014157932qr6xla09320071:24000
Carville and Cancienne soils, gently undulating, frequently floodedCT221914157941jj7sla09320071:24000
Cancienne silt loam, 0 to 1 percent slopesCmA118635769702s8sqla09520041:24000
Cancienne and Carville soils, gently undulating, frequently floodedCT6944576993mcdpla09520041:24000
Cancienne silty clay loam, 0 to 1 percent slopesCnA19215769742qr6xla09520041:24000
Cancienne silty clay loam, 0 to 1 percent slopesCdA224163936892qr6xla10920011:24000
Cancienne silt loam, 0 to 1 percent slopesCbA126663936882s8sqla10920011:24000
Gramercy-Cancienne silty clay loams, 0 to 1 percent slopesGcA5926394449f7g5la10920011:24000
Cancienne silty clay loam, 0 to 1 percent slopes, occasionally floodedCeA4117393696f6nwla10920011:24000
Cancienne silt loam, 0 to 1 percent slopes, occasionally floodedCfA1311393695f6nvla10920011:24000

Map of Series Extent

Approximate geographic distribution of the CANCIENNE 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 .