Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
115B71IL0030011971IL003001Bowdre5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2831098,-89.4687957
115B73IL0770011973IL077001Bowdre1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7298635,-89.5553739
131AM90143011990MO143001Bowdre4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6301117,-89.3681946
131AM02133022002MO133002Bowdre4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.6111565,-89.2839508

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BOWDRE series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the BOWDRE series and siblings. 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 BOWDRE 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 .

Click the image to view it full size.

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.

Competing Series

Soil series competing with BOWDRE share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the BOWDRE 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 BOWDRE 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 BOWDRE, 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. KY-2012-01-27-13 | Carlisle and Hickman Counties - July 1997

    Relationship of soils to topography and underlying material in the Openlake-Bardwell-Commerce-Robinsville general soil map unit in Carlisle County (Soil Survey of Carlisle and Hickman Counties, Kentucky; July 1997).

  2. KY-2012-01-27-18 | Carlisle and Hickman Counties - July 1997

    Relationship of soils to topography and underlying material in the Openlake-Commerce-Bardwell general soil map unit in Carlisle County (Soil Survey of Carlisle and Hickman Counties, Kentucky; July 1997).

  3. TN-2012-03-19-10 | Lauderdale County - June 1990

    Typical pattern of soils and underlying material in the Commerce-Robinsonville and Sharkey-Keyespoint-Openlake general soil map units on the Mississippi River flood plain (Soil Survey of Lauderdale County, TN; 1990).

Map Units

Map units containing BOWDRE 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
Bowdre silty clay loam, gently undulatingBoU5186565249lz5var01719641:20000
Bowdre silty clay loam, 0 to 1 percent slopesBoA3564565248lz5tar01719641:20000
Bowdre silty clay, gently undulatingBrU5540564161ly1rar03519701:20000
Bowdre silty clay, frequently floodedBw4420564162ly1sar03519701:20000
Bowdre silty clay, 0 to 1 percent slopesBrA3390564160ly1qar03519701:20000
Bowdre silty clay loam, gently undulatingBoB1960564374ly8mar03719661:20000
Bowdre silty clay loam, 0 to 1 percent slopesBoA520564373ly8lar03719661:20000
Bowdre silty clay loam, undulatingBoC470564375ly8nar03719661:20000
Bowdre, Desha, and Robinsonville soils, gently undulatingBdU1440564186ly2kar04119681:20000
Bowdre silty clay loamBr22460564336ly7dar09319671:20000
Bowdre silty clay loam, undulatingBoU1197564262ly50ar11119731:20000
Bowdre silty clay, undulatingBeC1410564433lybjar12319641:20000
Bowdre silty clay, gently undulatingBeB690564432lybhar12319641:20000
Bowdre silty clay, 0 to 1 percent slopesBeA170564431lybgar12319641:20000
Bowdre silty clay, 0 to 3 percent slopes, occasionally flooded8589A8676023942y8d9il00320021:12000
Bowdre silty clay, 0 to 3 percent slopes, occasionally flooded8589A143815399282y8d9il07720061:12000
Bowdre silty clay, 0 to 3 percent slopes, occasionally flooded8589A23701994312y8d9il18120011:12000
Bowdre silty clay, 0 to 2 percent slopes, protectedBr2991655015pzljky07520021:12000
Bowdre silty clay, 0 to 2 percent slopes, frequently floodedBw572655044pzmgky07520021:12000
Bowdre-Robinsonville complex, frequently floodedBr1660570517m4nsky61119911:20000
Bowdre silty clay loam, 0 to 3 percent slopes, rarely flooded86075208825010172q0hvmo13319781:24000
Bowdre silty clay loam, 0 to 3 percent slopes, frequently flooded86084138725010342q0j1mo13319781:24000
Bowdre silty clay loam, 0 to 3 percent slopes, occasionally flooded8614639025715762r02nmo13319781:24000
Bowdre silty clay, 0 to 3 percent slopes, rarely flooded860761050894225z0hzmo14319741:24000
Bowdre silty clay loam, 0 to 3 percent slopes, frequently flooded8608441525010332q0j1mo14319741:24000
Bowdre silty clay loam, 0 to 3 percent slopes, occasionally flooded86146156925716012r02nmo20119781:24000
Bowdre silty clay loam, 0 to 3 percent slopes, rarely flooded8607530525010182q0hvmo20119781:24000
Bowdre silty clay loam, 0 to 3 percent slopes, frequently flooded8608420425010352q0j1mo20119781:24000
Bowdre clayBc1863567396m1f3ms00119661:15840
Bowdre-Sharkey associationBS1244567395m1f2ms00119661:15840
Bowdre, Tunica, and Crevasse soils, (bowdre, tunica and bruno)Bc12335567573m1ltms02119611:20000
Bowdre clay, 0 to 2 percent slopesBk4284568037m22sms05519601:20000
Bowdre clay, 2 to 5 percent slopesBm238568038m22tms05519601:20000
Bowdre silty clayBd3105568069m23tms06319761:20000
Bowdre silty clay, 0 to 2 percent slopesBk3664568413m2gxms12519601:20000
Bowdre silty clayBo789568676m2rdms14919621:15840
Bowdre silty clay, 0.5 to 2 percent slopesBh2644568733m2t7ms15119591:20000
Bowdre silty clay loam, 0 to 2 percent slopesBk901568734m2t8ms15119591:20000
Bowdre silty clay, frequently flooded22198571089m587ms15720061:24000
Bowdre clay, coarse subsoilBw7522566771m0rytn04519631:15840
Bowdre clayBt3819566770m0rxtn04519631:15840
Bowdre silty clayBo6703567119m145tn09519661:20000
Bowdre silty clay, frequently floodedBs4224567120m146tn09519661:20000
Bowdre silty clay, occasionally floodedBo6773567146m151tn09719851:24000
Bowdre silty clayBo1521567235m17xtn13119661:15840
Bowdre silty clayBw5174567282m19ftn15719661:15840
Bowdre silty clay, frequently floodedBo5736567330m1bztn16719891:24000

Map of Series Extent

Approximate geographic distribution of the BOWDRE 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 .