Official Series Description


Lab Data Summary

Aggregate lab data for the CHICKASHA soil series. This aggregation is based on all pedons with a current taxon name of CHICKASHA, 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 CHICKASHA 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 CHICKASHA 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 CHICKASHA 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 CHICKASHA 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 CHICKASHA 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 CHICKASHA 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 CHICKASHA 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 CHICKASHA 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 .

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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.

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

Soil series sharing subgroup-level classification with CHICKASHA, 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-2012-02-17-03 | Logan County - June 1960

    Soils of the Zaneis-Lucien-Chickasha and the Renfrow-Vernon-Kirkland associations on red clays, sandstone, siltstone, and alluvium. They have developed largely on the Wellington, Garber, and Hennessey formations that dip successively toward the west (Soil Survey of Logan County, Oklahoma; June 1960).

  2. 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).

  3. OK-2012-02-17-49 | Stephens County - 1964

    Typical pattern of soils in association 3 (Soil Survey of Stephens County, Oklahoma; 1964).

  4. OK-2012-02-17-51 | Stephens County - 1964

    Typical pattern of soils in associations 6, 7, and 8 (Soil Survey of Stephens County, Oklahoma; 1964).

Map Units

Map units containing CHICKASHA 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
Chickasha loam, 1 to 3 percent slopes572283820352tp67ok01919771:24000
Chickasha loam, 3 to 5 percent slopes, moderately eroded7410838204630mzfok01919771:24000
Chickasha loam, 3 to 5 percent slopes619143820452tp66ok01919771:24000
Chickasha fine sandy loam, 1 to 3 percent slopesChB334038322230mzcok06719671:24000
Chickasha fine sandy loam, 0 to 1 percent slopesChA259538322130mzbok06719671:24000
Chickasha loam, 1 to 3 percent slopesCaB50973835022tp67ok08119661:24000
Chickasha and Zaneis soils, 1 to 3 percent slopesChB879383700dw8fok08519631:24000
Chickasha loam, 1 to 3 percent slopesCskB15983841422tp67ok10719961:24000
Chickasha loam, 1 to 3 percent slopes820293845812tp67ok11919831:24000
Chickasha fine sandy loam, 3 to 5 percent slopes, eroded715593845702yhdsok11919831:24000
Chickasha-Seminole complex, 3 to 5 percent slopes, gullied7711043845782yhdxok11919831:24000
Chickasha loam, 3 to 5 percent slopes99203845892tp66ok11919831:24000
Chickasha and Zaneis soils and Gullied land, 1 to 8 percent slopes, severely eroded8168493847232yhdyok12519751:24000
Chickasha loam, 3 to 5 percent slopes789703847222tp66ok12519751:24000
Chickasha loam, 1 to 3 percent slopes626313847212tp67ok12519751:24000
Seminole, Chickasha, and Mulhall soils, 3 to 8 percent slopes, severely eroded3934796384826dxfrok13319761:24000
Chickasha loam, 3 to 5 percent slopes629863848412tp66ok13319761:24000
Chickasha-Huska complex, 1 to 3 percent slopesCk481013848552yhdwok13719601:24000
Chickasha loam, 1 to 3 percent slopesChB136993848522tp67ok13719601:24000
Chickasha fine sandy loam, 1 to 3 percent slopesCaB922938484930mzcok13719601:24000
Chickasha and Zaneis soils and Gullied land, 1 to 8 percent slopes, severely erodedEt88893848612yhdyok13719601:24000
Chickasha loam, 3 to 5 percent slopesChC39313848532tp66ok13719601:24000
Chickasha loam, 0 to 1 percent slopesChA20253848512yhdtok13719601:24000
Chickasha fine sandy loam, 3 to 5 percent slopesCaC16773848502yhdrok13719601:24000
Chickasha loam, 5 to 8 percent slopesChD15523848542yhdvok13719601:24000
Chickasha fine sandy loam, 0 to 1 percent slopesCaA76538484830mzbok13719601:24000
Chickasha fine sandy loam, 3 to 8 percent slopesChD1402370919dfz4tx34919681:24000
Chickasha soils, 5 to 10 percent slopes, erodedCkD2333370920dfz5tx34919681:24000
Chickasha, loamy, 5 to 12 percent slopesHAD1203374474dknttx61219731:20000

Map of Series Extent

Approximate geographic distribution of the CHICKASHA 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 .