Official Series Description


Lab Data Summary

Aggregate lab data for the BIENVILLE soil series. This aggregation is based on all pedons with a current taxon name of BIENVILLE, 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 BIENVILLE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BIENVILLE 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 BIENVILLE 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 BIENVILLE 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 BIENVILLE 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 BIENVILLE 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 BIENVILLE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the BIENVILLE 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.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with BIENVILLE, 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

Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.

  1. TX-2012-03-19-06 | Angelina County - February 1988

    Typical pattern of soils and underlying material in the Besner-Mollville-Bienville map unit (Soil Survey of Angelina County, TX; 1988).

  2. TX-2012-03-21-33 | Leon County - July 1989

    The Gladewater, Kaufman, and Nahatche soils are dominant on the terraces and flood plains of the Trinity River system (Soil Survey of Leon County, TX; 1989).

Map Units

Map units containing BIENVILLE 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
Cahaba-Bienville-Guyton complex, gently undulatingCk2213815861001q7gjla00319781:24000
Bienville loamy fine sand, 1 to 5 percent slopesBn7237158609630g0mla00319781:24000
Bienville loamy fine sand, 1 to 5 percent slopesBmC5206172568730g0mla01119931:24000
Bienville-Guyton complex, gently undulatingBnB463917256881vxqcla01119931:24000
Bienville loamy fine sand, 1 to 5 percent slopesBlC3955172457130cqkla01319921:24000
Bienville loamy fine sand, 1 to 3 percent slopes, occasionally floodedBfB121315902301qcrrla01520051:24000
Guyton and Bienville soils frequently floodedGU3034014136851jg1rla01919831:24000
Bienville-Cahaba-Guyton complex, gently undulatingBn1098014136731jg1cla01919831:24000
Bienville loamy fine sand, 1 to 3 percent slopesBh141114136721jg1bla01919831:24000
Bienville loamy fine sand, 1 to 3 percent slopesBe165117245222sjxlla03119861:24000
Guyton and Bienville soils, frequently floodedGUA500314146721jh2lla05319891:24000
Bienville loamy fine sand, 1 to 3 percent slopesBhB70314146651jh2cla05319891:24000
Bienville-Guyton complex, gently undulatingBnB54314146661jh2dla05319891:24000
Bienville loamy fine sand, 1 to 3 percent slopesBe73016001571qq2zla05919861:24000
Bienville loamy fine sand, 1 to 5 percent slopesBn4099190309530cqkla06919831:24000
Bienville loamy fine sand, 1 to 3 percent slopesBe640917253241vxbmla11119921:24000
Bienville loamy fine sand, 1 to 5 percent slopesBhC2392172553430cqkla11519921:24000
Bienville loamy fine sand, 1 to 5 percent slopesBn143257033630cqkla11919891:24000
Bienville loamy fine sand, 0 to 5 percent slopesBnB36265751852sjxktx00519841:24000
Bienville loamy fine sand, 1 to 3 percent slopesIa824857533730n1ztx07319491:20000
Bienville loamy fine sand, 0 to 1 percent slopesHc301957533630n1ytx07319491:20000
Bienville loamy fine sand, 3 to 5 percent slopesIb127057533830n20tx07319491:20000
Bienville loamy fine sand, 1 to 5 percent slopesBnB31037537130cqktx16119861:24000
Bienville loamy fine sand, 1 to 3 percent slopesBeB17135764222sjxltx20319891:24000
Bienville loamy fine sand, 0 to 3 percent slopesBnB11084369175dd4wtx28919851:24000
Bienville loamy fine sand, 0 to 3 percent slopesBnB2485370270df96tx31319891:24000
Bienville loamy fine sand, 0 to 5 percent slopes1222655756202sjxktx34719761:24000
Bienville loamy fine sand, 1 to 5 percent slopesBe792757568830cqktx36519711:20000
Bienville loamy fine sand, 0 to 2 percent slopesBvB2467578205mdnstx40119931:24000
Bienville loamy fine sand, 0 to 3 percent slopesBeB929576084mbgctx60319841:24000
Bienville loamy fine sand, 0 to 3 percent slopesBeB3613576138mbj3tx60819811:24000
Bienville-Alaga association, gently undulatingBIB25417374410dklrtx61119801:20000

Map of Series Extent

Approximate geographic distribution of the BIENVILLE 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 .