Official Series Description


Lab Data Summary

Aggregate lab data for the CHOTEAU soil series. This aggregation is based on all pedons with a current taxon name of CHOTEAU, 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 CHOTEAU 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
11240A469653OK145021Choteau4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.8833351,-95.3405533
11240A469753OK145024Choteau4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.9047203,-95.4061127
11276-OK-51-776-OK101-51-7Choteau4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7536694,-95.6417778

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the CHOTEAU 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 CHOTEAU 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 CHOTEAU 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 CHOTEAU 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 CHOTEAU 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 CHOTEAU series and competing. 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 CHOTEAU 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 .

There are insufficient data to create the 2D hillslope position figure.

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 CHOTEAU, 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-2012-02-16-07 | Cherokee and Delaware Counties - December 1970

    Major soils in soil association 2 and their relation to the landscape (Soil Survey of Cherokee and Delaware Counties, Oklahoma; December 1970).

  2. OK-2012-02-17-32 | Pittsburg County - May 1971

    Major soils and underlying material in soil associations 1, 2, 3, and 7 (Soil Survey of Pittsburg County, Oklahoma; May 1971).

  3. OK-2012-02-17-43 | Rogers County - August 1966

    General locations of soil associations 1, 2, and 4 in a landscape that is typical of the central and eastern parts of Rogers County (Soil Survey of Rogers County, Oklahoma; August 1966).

Map Units

Map units containing CHOTEAU 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
Choteau loam, 1 to 3 percent slopesChB938571590m5sdok02919691:24000
Choteau silt loam, 1 to 3 percent slopesChB49291064962tgtkok03519681:20000
Choteau silt loam, 0 to 1 percent slopesChA44591064952tgtlok03519681:20000
Choteau very fine sandy loam, 0 to 1 percent slopesCb2231382269dts8ok03719521:24000
Choteau very fine sandy loam, 1 to 3 percent slopesCa1069382268dts7ok03719521:24000
Choteau silt loam, 1 to 3 percent slopesChB10035718472tgtkok04119671:24000
Choteau silt loam, 0 to 1 percent slopesChA6275718462tgtlok04119671:24000
Choteau silt loam, 1 to 3 percent slopes831745717722tgtkok09119801:24000
Choteau silt loam, 0 to 1 percent slopesChA78951065422tgtlok09719721:24000
Choteau silt loam, 1 to 3 percent slopesChB52171065432tgtkok09719721:24000
Choteau loam, 1 to 3 percent slopes940431064462tgtmok10119841:24000
Choteau silt loam, 3 to 5 percent slopesCouC2792384141dwqnok10719961:24000
Choteau silt loam, 1 to 3 percent slopesCouB27503841402tgtkok10719961:24000
Choteau loam, 1 to 3 percent slopesChB14761064532tgtmok11119681:24000
Choteau silt loam, 1 to 3 percent slopesChB42511066182tgtkok11519611:24000
Choteau silt loam, 0 to 1 percent slopesChA19931066172tgtlok11519611:24000
Choteau very fine sandy loam, 0 to 3 percent slopesCohB3076697345rdn0ok12119661:24000
Choteau very fine sandy loam, 0 to 3 percent slopesCoB2643571536m5qnok12119661:24000
Arents-Urban land-Choteau complex, 1 to 15 percent slopesAUCF2450697338rdmsok12119661:24000
Choteau loam, 1 to 3 percent slopesChB1787571535m5qmok12119661:24000
Choteau loam, 0 to 1 percent slopesChA1571571534m5qlok12119661:24000
Choteau silt loam, 1 to 3 percent slopesChB133101066542tgtkok13119631:24000
Choteau silt loam, 1 to 3 percent slopesChB33141067552tgtkok14519721:24000

Map of Series Extent

Approximate geographic distribution of the CHOTEAU 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 .