Official Series Description


Lab Data Summary

Aggregate lab data for the ST. PAUL soil series. This aggregation is based on all pedons with a current taxon name of ST. PAUL, 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 ST. PAUL 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
78C40A472659OK043001St. Paul7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.128334,-98.8969421
78C93P040392OK151001ST. PAUL7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8372231,-99.1344452
78C93P069093OK059005St. Paul8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9538879,-99.5950012
78C94P039794OK059001St. Paul7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9550018,-99.6880569
78C94P039894OK059002St. Paul7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9561119,-99.6905594
78C94P039994OK059003St. Paul7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9577789,-99.6916656
78C94P040094OK059004St. Paul7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.9708328,-99.7016678
78C40A4725S1959OK153003St. Paul7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2413826,-99.1472168

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ST. PAUL 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 ST. PAUL 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 ST. PAUL 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 ST. PAUL 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 ST. PAUL 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 ST. PAUL 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 ST. PAUL 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 ST. PAUL, 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-2010-09-29-20 | Woods County - 2003

    Typical pattern of soils and underlying material in the Quinlan-Woodward-Deepwood general soil map unit (Soil Survey of Woods County, Oklahoma; 2003).

  2. OK-2012-02-16-04 | Blaine County - February 1968

    Typical pattern of soils in associations 1, 3, 4, and 6 (Soil Survey of Blaine County, Oklahoma; February 1968).

  3. OK-2012-02-16-24 | Dewey County - December 1963

    Typical pattern of the soils in associations 1 and 2 (Soil Survey of Dewey County, Oklahoma; December 1963).

  4. OK-2012-02-16-27 | Dewey County - December 1963

    Typical pattern of most of the soils in association 5 (Soil Survey of Dewey County, Oklahoma; December 1963).

  5. OK-2012-02-16-28 | Ellis County - April 1966

    Major soils of associations 1, 2, 3, and 11 (Soil Survey of Ellis County, Oklahoma; April 1966).

  6. OK-2012-02-16-30 | Ellis County - April 1966

    Major soils of associations 7, 8, and 10 (Soil Survey of Ellis County, Oklahoma; April 1966).

  7. OK-2012-02-16-36 | Greer County - March 1967

    Major soils in soil association 2, and their relation to the landscape (Soil Survey of Greer County, Oklahoma; March 1967).

  8. OK-2012-02-16-45 | Harper County - June 1960

    A schematic drawing showing a normal pattern of soils formed over Permian redbeds. The typical slope range is given for each soil. Alternating layers of sandstone and shale underlie these soils (Soil Survey of Harper County, Oklahoma; June 1960).

  9. OK-2012-02-17-10 | Major County - October 1968

    Soil associations in the western part of the county (Soil Survey of Major County, Oklahoma; October 1968).

  10. OK-2012-02-17-42 | Roger Mills County - August 1963

    Typical pattern of soils in association 8. Woodward silt loam is a variation, which is described in the section "Descriptions of Soils" (Soil Survey of Roger Mills County, Oklahoma; August 1963).

  11. OK-2012-02-17-58 | Woodward County - November 1963

    Typical pattern of soils of the St. Paul-Carey-Woodward association (Soil Survey of Woodward County, Oklahoma; November 1963).

Map Units

Map units containing ST. PAUL 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
St. Paul silt loam, 1 to 3 percent slopes54611724813812932txy6ks03319871:24000
St. Paul silt loam, 0 to 1 percent slopes5460408913812922tckpks03319871:24000
St. Paul silt loam, 1 to 3 percent slopesStpB42331012782txy6ok00720211:24000
St. Paul silt loam, 3 to 5 percent slopesStpC10731012792txy7ok00720211:24000
St. Paul silt loam, 1 to 3 percent slopes53153073816922txy6ok00919781:24000
St. Paul silt loam, 0 to 1 percent slopes5266063816912tckpok00919781:24000
St. Paul silt loam, 1 to 3 percent slopesSpB70683817722txy6ok01119651:24000
St. Paul silt loam, 0 to 1 percent slopesSpA32883817712tckpok01119651:24000
St. Paul silt loam, 1 to 3 percent slopesStB555533823432txy6ok03919731:24000
St. Paul and Carey soils, 3 to 5 percent slopesStC27036382344dtvpok03919731:24000
St. Paul silt loam, 0 to 1 percent slopesStA94483823422tckpok03919731:24000
St. Paul silt loam, 1 to 3 percent slopesSaB371503823982txy6ok04319611:24000
St. Paul silt loam, 3 to 5 percent slopesSaC182223823992txy7ok04319611:24000
St. Paul silt loam, 0 to 1 percent slopesSaA54823823972tckpok04319611:24000
St. Paul clay loam, 3 to 5 percent slopes, moderately erodedScC24424382400307sbok04319611:24000
St. Paul silt loam, 1 to 3 percent slopesSaB272183824692txy6ok04519631:24000
St. Paul silt loam, 0 to 1 percent slopesSaA25533824682tckpok04519631:24000
St. Paul silt loam, 1 to 3 percent slopesStpB190323830302txy6ok05919981:24000
St. Paul silt loam, 0 to 1 percent slopesStpA126203830292tckpok05919981:24000
St. Paul silt loam, 3 to 5 percent slopesStpC24253830312txy7ok05919981:24000
St. Paul silt loam, 5 to 8 percent slopesStpD1227383032dvkwok05919981:24000
St. Paul silt loam, 1 to 3 percent slopesSaB255603834792txy6ok07519731:24000
St. Paul silt loam, 0 to 1 percent slopesSaA166673834782tckpok07519731:24000
St. Paul-Hinkle complex, 0 to 1 percent slopesSbA1650383480dw1bok07519731:24000
St. Paul silt loam, 1 to 3 percent slopesSpB51003838602txy6ok09319651:24000
St. Paul silt loam, 3 to 5 percent slopesSpC16533838612txy7ok09319651:24000
St. Paul silt loam, 0 to 1 percent slopesSpA5683838592tckpok09319651:24000
St. Paul silt loam, 1 to 3 percent slopesSaB44243847732txy6ok12919611:24000
St. Paul silt loam, 3 to 5 percent slopes, erodedSaC21684384774dxd2ok12919611:24000
St. Paul silt loam, 0 to 1 percent slopesSaA4073847722tckpok12919611:24000
St. Paul silt loam, 1 to 3 percent slopes47861513850332txy6ok14919761:24000
St. Paul silt loam, 0 to 1 percent slopes46139213850322tckpok14919761:24000
St. Paul silt loam, 3 to 5 percent slopes4860973850342txy7ok14919761:24000
St. Paul silt loam, 1 to 3 percent slopesStpB21763852352txy6ok15119951:24000
St. Paul silt loam, 0 to 1 percent slopesStpA6233852342tckpok15119951:24000
St. Paul silt loam, 1 to 3 percent slopesSaB113583853012txy6ok15319611:24000
St. Paul silt loam, 3 to 5 percent slopesSaC92863853022txy7ok15319611:24000
St. Paul silt loam, 0 to 1 percent slopesSaA47323853002tckpok15319611:24000
St. Paul silt loam, 0 to 1 percent slopesSpA13033363843d6lwtx07519611:20000
St. Paul silt loam, 1 to 2 percent slopesSpB1151363844d6lxtx07519611:20000
St. Paul silt loamSp1627364616d7dttx10119691:20000
St. Paul silt loam, 0 to 1 percent slopesSpA9930366964d9vktx19119651:20000
St. Paul silt loam, 1 to 2 percent slopesSpB2678366965d9vltx19119651:20000
St. Paul silt loam, 0 to 1 percent slopesSpA6304368609dckmtx26919991:31680
St. Paul silt loam, 0 to 1 percent slopesSpA3889372306dhdwtx43319701:24000

Map of Series Extent

Approximate geographic distribution of the ST. PAUL 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 .