Official Series Description


Lab Data Summary

Aggregate lab data for the BOWIE soil series. This aggregation is based on all pedons with a current taxon name of BOWIE, 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 BOWIE 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
133B86P015883TX203001Bowie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4749985,-94.4916687
133B84P024383TX401001Bowie1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2125015,-94.7375031
133B84P024183TX423001Bowien/aPrimary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.4166679,-95.1083298
133B86P015986TX401001Bowie6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2125015,-94.7375031
133B87P040287LA085001Bowie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.7938881,-93.625
133B95P013894TX067002Bowie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties33.0496407,-94.3000031
133B80P0506S1980LA031001Bowie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.0344429,-93.6241684
133B80P0507S1980LA031002Bowie7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties31.9827785,-93.9836121
135B74-OK-64-874-OK127-64-8Bowie1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.1706861,-95.6719917
13840A5049S1960FL121030BOWIE5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.166069,-82.9726563
13840A5050S1960FL121031BOWIE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties30.2682877,-82.9918213

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BOWIE 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 BOWIE 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 BOWIE 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 BOWIE 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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Click the image to view it full size.

Competing Series

Soil series competing with BOWIE 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 BOWIE 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 BOWIE 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 .

Click the image to view it full size.

Click the image to view it full size.

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 BOWIE, 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. FL-2011-05-31-16 | Suwannee County - 1965

    Marine terraces in Suwannee County, and the position of some of the soils (Soil Survye of Suwannee County, Florida; 1965).

  2. FL-2012-04-26-27 | Washington County - May 1965

    Geologic formations of Washington County and the position of most soil series (Soil Survey of Washington County, Florida; May 1965).

  3. TX-2010-11-03-74 | Marion and Cass Counties -

    Pattern of soils and parent material in the Cuthbert-Bowie-Kirvin general soil map unit (Soil Survey of Marion and Cass Counties, Texas).

  4. TX-2010-11-04-15 | San Augustine and Sabine Counties -

    Cuthbert-Tenaha-Bowie association (Soil Survey of San Augustine and Sabine Counties, Texas).

  5. TX-2012-03-21-05 | Harrison County - October 1994

    Pattern of soils and parent material in the Cuthbert-Bowie-Kirvin general soil map unit (Soil Survey of Harrison County, TX; 1994).

  6. TX-2012-03-21-07 | Harrison County - October 1994

    Pattern of soils and parent material in the Lilbert-Warnock-Wolfpen general soil map unit (Soil Survey of Harrison County, TX; 1994).

  7. TX-2012-03-21-78 | Smith County - July 1993

    Typical pattern of soils and parent material in the Bowie-Cuthbert-Kirvin general soil map unit (Soil Survey of Smith County, TX; 1993).

Map Units

Map units containing BOWIE 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
Bowie, Lakeland, and Cuthbert soils, 8 to 12 percent slopesBwD48421328110c0f6al00319611:20000
Bowie, Lakeland, and Cuthbert soils, 12 to 25 percent slopes, erodedBwF223876328112c0f8al00319611:20000
Cuthbert, Bowie, and Sunsweet soils, 8 to 12 percentCuD18577328127c0fral00319611:20000
Cuthbert, Bowie, and Sunsweet soils, 12 to 17 percent slopes, erodedCuE212472328128c0fsal00319611:20000
Bowie, Lakeland, and Cuthbert soils, 5 to 8 percent slopesBwC7277328109c0f5al00319611:20000
Bowie fine sandy loam, thin solum, 2 to 5 percent slopesBtB5016328107c0f3al00319611:20000
Bowie, Lakeland, and Cuthbert soils, 8 to 12 percent slopes, erodedBwD23554328111c0f7al00319611:20000
Cuthbert, Bowie, and Sunsweet soils, 5 to 8 percent slopesCuC873328126c0fqal00319611:20000
Bowie fine sandy loam, 3 to 8 percent slopes10418731793412tf49ar01919831:20000
Bowie fine sandy loam, 1 to 3 percent slopes9232431794282wdl2ar01919831:20000
Smithdale-Bowie-Sacul association, undulating77363179414lypdar01919831:20000
Bowie fine sandy loam, 3 to 8 percent slopesBwC31505652942tf49ar02519651:15840
Bowie fine sandy loam, 1 to 3 percent slopesBwB2245652932wdl2ar02519651:15840
Bowie fine sandy loam, 3 to 8 percent slopes9624185653742tf49ar02719831:20000
Bowie fine sandy loam, 1 to 3 percent slopes8260995653732wdl2ar02719831:20000
Bowie fine sandy loam, 3 to 8 percent slopes3104935656552tf49ar05719761:20000
Bowie fine sandy loam, 1 to 3 percent slopes240865656442wdl2ar05719761:20000
Smithdale-Bowie-Sacul association, undulating7770283179304lypdar05919831:20000
Bowie fine sandy loam, 1 to 3 percent slopes9411031793182wdl2ar05919831:20000
Bowie fine sandy loam, 3 to 8 percent slopes10410831792312tf49ar05919831:20000
Bowie fine sandy loam, 3 to 8 percent slopesBoC286837215092tf49ar09920001:24000
Bowie fine sandy loam, 1 to 3 percent slopesBoB50907215082wdl2ar09920001:24000
Bowie fine sandy loam, 1 to 3 percent slopes9245485649632wdl2ar67019811:20000
Bowie fine sandy loam, 3 to 8 percent slopes10244095648822tf49ar67019811:20000
Bowie fine sandy loam, 5 to 8 percent slopesBoD2324117245732y11wla01319921:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC2106917245722y11vla01319921:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC179225709842y11vla01520051:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC1770828056982y11vla01720131:24000
Bowie fine sandy loam, 5 to 8 percent slopesBoD376128056992y11wla01720131:24000
Bowie fine sandy loam, 1 to 5 percent slopesBw193305693112y11vla02719861:20000
Bowie fine sandy loam, 1 to 5 percent slopesBo87217245242y11vla03119861:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC1549817252532y11vla04919911:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC125115711122y11vla06119911:24000
Bowie fine sandy loam, 5 to 8 percent slopesBoD41325711132y11wla06119911:24000
Bowie fine sandy loam, 1 to 5 percent slopesBwC58019031542y11vla06919831:24000
Bowie fine sandy loam, 5 to 8 percent slopesBwD919031592y11wla06919831:24000
Bowie fine sandy loam, 1 to 5 percent slopesBwC1554819030252y11vla08519911:24000
Bowie fine sandy loam, 5 to 8 percent slopesBwD407719030262y11wla08519911:24000
Bowie fine sandy loam, 1 to 5 percent slopesBh143817253252y11vla11119921:24000
Bowie fine sandy loam, 1 to 5 percent slopesBnC106817255352y11vla11519921:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoB79915751222y11vtx00119701:20000
Bowie fine sandy loam, 3 to 8 percent slopesBoD70205751232tf49tx00119701:20000
Bowie fine sandy loam, 3 to 8 percent slopesBn404605753152tf49tx07319491:20000
Bowie fine sandy loam, 1 to 3 percent slopesBm182585753142wdl2tx07319491:20000
Bowie fine sandy loam, sloping, erodedBo1786575316m9nltx07319491:20000
Bowie fine sandy loam, 1 to 5 percent slopesBoC511335764242y11vtx20319891:24000
Bowie fine sandy loam, 1 to 5 percent slopesBwB65775754932y11vtx22519941:24000
Bowie fine sandy loam, 1 to 8 percent slopes13120515756212tf48tx34719761:24000
Bowie fine sandy loam, 1 to 8 percent slopesBo27755756902tf48tx36519711:20000
Bowie fine sandy loam, 1 to 5 percent slopesBwB234245782062y11vtx40119931:24000
Bowie fine sandy loam, 1 to 5 percent slopesBwB25715757562y11vtx41920021:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoB309135757882y11vtx42319871:24000
Bowie fine sandy loam, 5 to 8 percent slopesBoD54825757892y11wtx42319871:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC162865760402y11vtx49919931:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC746775760852y11vtx60319841:24000
Bowie-Urban land complex, 2 to 5 percent slopesBuC2375576086mbgftx60319841:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC978605761392y11vtx60819811:24000
Bowie-Urban land complex, 2 to 5 percent slopesBuC12376576140mbj5tx60819811:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC1281825764802y11vtx61620041:24000
Bowie fine sandy loam, 1 to 5 percent slopesBoC1134418947522y11vtx61920071:24000

Map of Series Extent

Approximate geographic distribution of the BOWIE 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 .