Official Series Description


Lab Data Summary

Aggregate lab data for the WINDTHORST soil series. This aggregation is based on all pedons with a current taxon name of WINDTHORST, 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 WINDTHORST 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
84A70-OK-57-2070-OK113-57-20Windthorst4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3868,-96.2278139
84A70-OK-57-2270-OK113-57-22Windthorst4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7555833,-96.1399583
84A70-OK-62-270-OK123-62-2Windthorst4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.78275,-96.5740306
84B68-OK-10-868-OK019-10-8Windthorst4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.0928,-97.160025
84B70-OK-10-170-OK019-10-1Windthorst4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.2495167,-97.2449528
84B78P038977TX143001Windthorst6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2586098,-98.1927795
84B96P030696TX143007Windthorst7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2525826,-98.2016907
84B96P030796TX143008Windthorst7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.245472,-98.1815033
84B96P030896TX143009Windthorst8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.2982483,-98.3027191
8568-OK-62-168-OK123-62-1Windthorst4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.78235,-96.8659667
8540A4630S1974TX367001Windthorst6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties32.7288895,-97.8766632

Water Balance

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

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

Soil series sharing subgroup-level classification with WINDTHORST, 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-2012-02-16-16 | Comanche County - August 1967

    Topography and underlying material of Lawton soils and other extensive soils in northwestern part of county (Soil Survey of Comanche County, Oklahoma; August 1967).

  2. OK-2012-02-17-07 | Love County - September 1966

    Diagram showing typical relief and relative positions of the soils in associations 2 and 5 in the north-central part of Love County (Soil Survey of Love County, Oklahoma; September 1966).

  3. OK-2012-02-17-08 | Love County - September 1966

    Diagram showing typical relief in the northwestern corner of the county and the relative positions of the soils in association 4 (Soil Survey of Love County, Oklahoma; September 1966).

  4. 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).

  5. OK-2012-02-17-37 | Pontotoc County - April 1973

    Pattern of soils in the Stephenville-Darnell-Windthorst association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

  6. OK-2012-02-17-38 | Pontotoc County - April 1973

    Pattern of soils in the Chigley-Windthorst association (Soil Survey of Pontotoc County, Oklahoma; April 1973).

  7. OK-2012-02-17-48 | Stephens County - 1964

    Typical pattern of soils in associations 1 and 5 (Soil Survey of Stephens County, Oklahoma; 1964).

  8. 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).

  9. TX-2012-03-22-19 | Wise County - May 1989

    Typical pattern of the Windthorst-Chaney-Selden general soil map unit (Soil Survey of Wise County, TX; 1989).

Map Units

Map units containing WINDTHORST 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
Windthorst-Weatherford complex, 5 to 12 percent slopes55771363820412sz2wok01919771:24000
Windthorst fine sandy loam, 3 to 8 percent slopes, eroded53241003820392tc3wok01919771:24000
Windthorst fine sandy loam, 3 to 5 percent slopes52142613820382tc3tok01919771:24000
Windthorst very fine sandy loam, 1 to 3 percent slopes5196773820372tc3qok01919771:24000
Windthorst-Darnell-Rock outcrop complex, 5 to 25 percent slopes5494603820402tc3zok01919771:24000
Windthorst sandy loam, 3 to 5 percent slopesWhC4518382214dtqhok03119651:24000
Windthorst sandy loam, 1 to 3 percent slopesWhB3025382213dtqgok03119651:24000
Windthorst-Weatherford complex, 5 to 12 percent slopesWsD269173837612sz2wok08519631:24000
Weatherford-Windthorst-Konsil complex, 1 to 8 percent slopes, severely erodedSw322261383744dw9vok08519631:24000
Windthorst-Darnell-Rock outcrop complex, 5 to 25 percent slopesWn59343837602tc3zok08519631:24000
Windthorst fine sandy loam, 1 to 5 percent slopesWdC27803837582tc3rok08519631:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, erodedWdC217033837592tc3sok08519631:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB257783630312zht3tx03519771:24000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely erodedHwD340653630322zhsztx03519771:24000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB29063630292zht2tx03519771:24000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB259932211862zht2tx09319741:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely erodedHwD3198732211852zhsztx09319741:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB22932211872zht3tx09319741:20000
Windthorst and Duffau soils, 2 to 8 percent slopes, severely eroded2143463644692tc22tx09719731:24000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded1939893644662xmd9tx09719731:24000
Windthorst fine sandy loam, 5 to 8 percent slopes8333663645372tc3vtx09719731:24000
Windthorst fine sandy loam, 1 to 5 percent slopes8226613645362tc3rtx09719731:24000
Windthorst loamy fine sand, 5 to 8 percent slopes81957364535d7b6tx09719731:24000
Windthorst loamy fine sand, 1 to 5 percent slopes806763645342tc3xtx09719731:24000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB98732211982zht2tx13319721:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely erodedHwD378432211962zhsztx13319721:20000
Windthorst fine sandy loam, 1 to 5 percent slopesWnBC33232211972zht1tx13319721:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB2316433654182zht3tx14319661:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely erodedHwD3247503653712zhsztx14319661:20000
Windthorst loamy fine sand, 1 to 5 percent slopesWnC166643654162tc3xtx14319661:20000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB158823654172zht2tx14319661:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely erodedWnD3112703654222zht0tx14319661:20000
Windthorst fine sandy loam, 1 to 5 percent slopesWnBC14693654192zht1tx14319661:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, erodedWdC320042366884d9rztx18719731:20000
Windthorst fine sandy loam, 1 to 3 percent slopesWdB2551366883d9rytx18719731:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB235803766722zht3tx19319941:24000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB35133766712zht2tx19319941:24000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely erodedHwD345332212232zhsztx19319941:24000
Windthorst fine sandy loam, 1 to 5 percent slopesWnBC91693680682zht1tx23719921:24000
Windthorst and Duffau soils, 2 to 8 percent slopes, severely eroded45457753707922tc22tx33719751:24000
Windthorst fine sandy loam, 1 to 5 percent slopes43398633707902tc3rtx33719751:24000
Windthorst fine sandy loam, 5 to 8 percent slopes44331623707912tc3vtx33719751:24000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately eroded15191533707592xmd9tx33719751:24000
Windthorst loamy fine sand, 1 to 5 percent slopes4280603707892tc3xtx33719751:24000
Windthorst fine sandy loam, 1 to 5 percent slopesWnBC37643909792zht1tx36319791:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB2732212312zht3tx36319791:24000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB2403743909212zht3tx36719731:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately erodedDwC2244163908762xmd9tx36719731:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely erodedWnD3118663909242zht0tx36719731:20000
Windthorst loamy fine sand, 1 to 5 percent slopesWnC77243909182tc3xtx36719731:20000
Windthorst fine sandy loam, 1 to 5 percent slopesWnBC54983909202zht1tx36719731:20000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB42643909192zht2tx36719731:20000
Windthorst-Urban land complex, 2 to 8 percent slopesWuD5153909232xmf9tx36719731:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely erodedHwD320832212452zhsztx36719731:20000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB11363724372zht2tx43919791:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately erodedDwC249730544452xmd9tx43919791:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB21243724392zht3tx43919791:20000
Windthorst fine sandy loam, 1 to 5 percent slopesWtC217793737042tc3rtx49719841:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately erodedWeC128213737012xmd9tx49719841:20000
Windthorst fine sandy loam, 3 to 8 percent slopes, erodedWtC3108793737052tc3wtx49719841:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely erodedWnD357732212552zht0tx49719841:20000
Windthorst fine sandy loam, 1 to 5 percent slopes, moderately erodedWoB2213333743712zht3tx60919751:20000
Windthorst and Duffau sandy clay loams, 1 to 8 percent slopes, severely erodedWnD383463743732zht0tx60919751:20000
Windthorst very fine sandy loam, 1 to 5 percent slopesWoB72363743692zht2tx60919751:20000
Windthorst loamy fine sand, 1 to 5 percent slopesWnC46893743682tc3xtx60919751:20000
Windthorst fine sandy loam, 1 to 5 percent slopesWnBC9523743702zht1tx60919751:20000
Duffau-Windthorst complex, 1 to 5 percent slopes, moderately erodedDwC29433743342xmd9tx60919751:20000
Hico and Windthorst sandy clay loams, 1 to 8 percent slopes, severely erodedHwD32403743722zhsztx60919751:20000

Map of Series Extent

Approximate geographic distribution of the WINDTHORST 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 .