Official Series Description


Lab Data Summary

Aggregate lab data for the OWENS soil series. This aggregation is based on all pedons with a current taxon name of OWENS, 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 OWENS 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
80B84P077584TX429002Owens8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.8272209,-98.7386093
80B84P077684TX429003Owens6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.9261093,-99.0336075

Water Balance

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

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.

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

Competing Series

Soil series competing with OWENS 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 OWENS 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 OWENS 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 OWENS, 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. KS-2012-01-20-23 | Clark County - December 1982

    Typical pattern of soils in the Penden-Campus-Canlon association (Soil Survey of Clark County, Kansas; 1982).

  2. KS-2012-01-20-24 | Clark County - December 1982

    Typical pattern of soils in the Carey-Woodward-Quinlan association (Soil Survey of Clark County, Kansas; 1982).

  3. TX-2010-11-03-42 | Jack County - 2005

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

  4. TX-2010-11-05-03 | Young County - 2009

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

  5. 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).

  6. TX-2012-03-21-46 | McCulloch County - November 1974

    Pattern of soils in Rowena-Mereta association (Soil Survey of McCulloch County, TX; 1974).

  7. TX-2012-03-21-79 | Stephens County - May 1994

    Typical pattern of soils and parent material in the Bonti-Truce-Bluegrove general soil map unit (Soil Survey of Stephens County, TX; 1994).

  8. TX-2012-03-21-85 | Stonewall County - January 1975

    Tillman-Vernon soil association (Soil Survey of Stonewall County, TX; 1975).

  9. TX-2012-03-21-86 | Stonewall County - January 1975

    Owens-Cottonwood soil association (Soil Survey of Stonewall County, TX; 1975).

Map Units

Map units containing OWENS 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
Owens stony clay, 5 to 30 percent slopesOsF25787362727d5fwtx02319711:24000
Throck-Owens-Lueders association, hilly4349698363619d6cntx05919791:24000
Throck-Callahan-Owens association, undulating4233479363618d6cmtx05919791:24000
Owens-Throck association, hilly2910278363603d6c4tx05919791:24000
Stony land and Owens soils, moderately steepSTE52493364037d6t4tx08319681:24000
Purves and Owens soils, undulatingPOB47804364030d6sxtx08319681:24000
Bonti-Owens complex, 1 to 20 percent slopes, extremely boulderyBWB38653640032sz2htx08319681:24000
Owens clay, 1 to 5 percent slopesOwB6243640292szq1tx08319681:24000
Owens clay, 5 to 30 percent slopes, extremely stonyOwG27533644002tc3ftx09319741:20000
Owens clay, 1 to 5 percent slopesOcC12423643992szq1tx09319741:20000
Owens clay, 5 to 30 percent slopes, extremely stonyOWE268153652582tc3ftx13319721:20000
Owens clay, 1 to 5 percent slopesOcB100283652592szq1tx13319721:20000
Owens clay, 5 to 30 percent slopes, extremely stonyOwE71043653942tc3ftx14319661:20000
Owens clay, 1 to 3 percent slopesOcB1001367506dbf1tx20719601:20000
Owens clay, 5 to 30 percent slopes, extremely stonyOwE192953680492tc3ftx23719921:24000
Owens-Vernon complexOv2143368248dc5ztx25319661:20000
Owens clay, 5 to 30 percent slopes, extremely stonyOwE2453688732tc3ftx28119901:24000
Owens and Tarrant soils, hillyOTE31355369958ddz4tx30719701:24000
Bonti-Owens complex, 1 to 20 percent slopes, extremely boulderyBOC77783699302sz2htx30719701:24000
Owens-Nukrum association, rollingOKD6863369957ddz3tx30719701:24000
Owens-Blanket association, undulatingOBC3248369956ddz2tx30719701:24000
Truce-Owens complex, 5 to 20 percent slopes3513640370781dftptx33719751:24000
Owens-Harpersville complex, 8 to 45 percent slopes, extremely boulderyOhG130573909602szpztx36319791:24000
Owens very stony clay, 1 to 8 percent slopesOnE1864390959f3tltx36319791:24000
Owens clay, 1 to 5 percent slopesOnC13543909582szq1tx36319791:24000
Owens-Harpersville complex, 8 to 45 percent slopes, extremely boulderyOtG33203908982szpztx36719731:20000
Owens clay, 3 to 12 percent slopesOcE2096390897f3rltx36719731:20000
Owens-Harpersville complex, 8 to 45 percent slopes, extremely boulderyOXF36993720732szpztx41719851:24000
Owens-Harpersville association, undulating, very stonyOXC2566372072dh5btx41719851:24000
Owens-Harpersville complex, 8 to 45 percent slopes, extremely boulderyOxE356863722062szpztx42919851:24000
Owens clay, 1 to 5 percent slopesOcC27813722052szq1tx42919851:24000
Owens-Lueders complex, 5 to 30 percent slopes, extremely boulderyOsE43525372705dhtrtx44719911:24000
Owens-Harpersville complex, 8 to 45 percent slopes, extremely boulderyOrE347613727042szpztx44719911:24000
Owens clay, 3 to 8 percent slopesOnD2349372703dhtptx44719911:24000
Owens clay, 5 to 30 percent slopes, extremely stonyOwE36413736732tc3ftx49719841:20000
Owens-Harpersville complex, 8 to 45 percent slopes, extremely boulderyOhG121083737672szpztx50320031:24000
Owens clay, 5 to 12 percent slopes, rubblyOnE7912373797djyztx50320031:24000
Owens clay, 10 to 30 percent slopes34764037392830gjztx60119771:31680
Bonti-Owens complex, 8 to 30 percent slopes1126849390984f3vdtx60219751:24000
Owens-Harpersville complex, 8 to 45 percent slopes, extremely bouldery76241943910552szpztx60219751:24000

Map of Series Extent

Approximate geographic distribution of the OWENS 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 .