Official Series Description


Lab Data Summary

Aggregate lab data for the GOWEN soil series. This aggregation is based on all pedons with a current taxon name of GOWEN, 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 GOWEN 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 GOWEN 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 GOWEN 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 GOWEN 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 GOWEN 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with GOWEN 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 GOWEN 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 GOWEN 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with GOWEN, 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. OK-2012-02-17-09 | Love County - September 1966

    Diagram showing relief typical of the central part of the county and the relative positions of the soils in association 7 (Soil Survey of Love County, Oklahoma; September 1966).

  2. OK-2012-02-17-26 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Agra-Coyle and Steedman-Lucien-Grainola map units (Soil Survey of Payne County, Oklahoma; April 1987).

  3. OK-2012-02-17-50 | Stephens County - 1964

    Typical pattern of soils in association 4 (Soil Survey of Stephens County, Oklahoma; 1964).

  4. TX-2010-11-03-41 | Jack County - 2005

    Typical pattern of soils and underlying material in the Exray-Truce-Bonti general soil map unit (Soil Survey of Jack County, Texas; 2005).

  5. TX-2010-11-03-44 | Jack County - 2005

    Typical pattern of soils and underlying material in the Duffau-Windthorst-Keeter general soil map unit (Soil Survey of Jack County, Texas; 2005).

  6. TX-2010-11-05-04 | Young County - 2009

    Pattern of soils and underlying material in the Grandfield-Gowen and Lincoln-Westola-Padgett general soil map units (Soil Survey of Young County, Texas; 2009).

  7. TX-2010-11-05-05 | Young County - 2009

    Pattern of soils and underlying material in the Sagerton general soil map unit (Soil Survey of Young County, Texas; 2009).

  8. TX-2012-03-21-51 | Navarro County - December 1974

    Typical pattern of soils in the Crockett-Wilson soil association (Soil Survey of Navarro County, TX; 1974).

  9. TX-2012-03-21-53 | Navarro County - December 1974

    Typical pattern of soils in the Wilson-Burleson association (Soil Survey of Navarro County, TX; 1974).

Map Units

Map units containing GOWEN 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
Steedman-Gowen, frequently flooded, complex, 0 to 8 percent slopes874412384588dx62ok11919831:24000
Zavala and Gowen soils, 0 to 2 percent slopes, frequently floodedZg3922390521f3cgtx02920001:24000
Gowen clay loam, 0 to 2 percent slopes, occasionally floodedGo1393390465f39ntx02920001:24000
Gowen soils, frequently floodedGs6214363509d683tx05519721:20000
Gowen clay loam, occasionally floodedGo1660363508d682tx05519721:20000
Gowen soils, frequently flooded2318391363875d6mxtx07719771:24000
Gowen soils, frequently flooded346408364483d78jtx09719731:24000
Gowen fine sandy loam, 0 to 1 percent slopes, rarely flooded321225364481d78gtx09719731:24000
Gowen clay loam, 0 to 1 percent slopes, rarely flooded33697364482d78htx09719731:24000
Gowen loam, occasionally flooded391086364821d7mftx11319751:20000
Gowen loam, frequently flooded40927364823d7mhtx11319751:20000
Gowen clay loam, occasionally flooded393185364990d7swtx12119751:24000
Gowen clay loam, frequently flooded402783364992d7sytx12119751:24000
Gowen clay loam, occasionally floodedGo2966365373d867tx14319661:20000
Gowen clay loam, frequently flooded289336365446d88ltx14519751:20000
Gowen clay loam, occasionally flooded271103365445d88ktx14519751:20000
Gowen clay loam, frequently flooded423276367756dbp3tx21719751:20000
Gowen loam, occasionally floodedGo19153368037dbz5tx23719921:24000
Gowen loam, frequently floodedGw13325368038dbz6tx23719921:24000
Gowen clay loam, frequently floodedGy2889368173dc3ktx25119811:20000
Gowen clay loam, occasionally floodedGw2882368172dc3jtx25119811:20000
Gowen clay loam, frequently floodedGo5771370099df3ptx30919921:24000
Gowen clay loam, frequently floodedGwA2811370676dfq9tx33119881:24000
Gowen soils, frequently flooded2115513370766dft6tx33719751:24000
Gowen loam, occasionally flooded206769370765dft5tx33719751:24000
Gowen clay loam, frequently floodedGy9822370938dfzrtx34919681:24000
Gowen clay loam, occasionally floodedGw6310370937dfzqtx34919681:24000
Gowen fine sandy loam, occasionally floodedGn5318370935dfzntx34919681:24000
Gowen fine sandy loam, frequently floodedGo1175370936dfzptx34919681:24000
Gowen clay loam, frequently flooded342391373162dj9htx47719791:24000
Gowen loam, 0 to 1 percent slopes, occasionally floodedGeA35147373751djxhtx50320031:24000
Gowen clay loam, frequently floodedGf14066374473dknstx61219731:20000
Gowen clay loam, occasionally floodedGc5985374472dknrtx61219731:20000

Map of Series Extent

Approximate geographic distribution of the GOWEN 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 .