Official Series Description


Lab Data Summary

Aggregate lab data for the RENFROW soil series. This aggregation is based on all pedons with a current taxon name of RENFROW, 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 RENFROW 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
80A72-OK-60-172-OK119-60-1Renfrow4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.1517278,-97.2946556
80A90P094690OK103001Renfrow8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.3025017,-97.3152771
80A91P090691OK109005Renfrow7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6947212,-97.6005554
80A40A4722S1953OK117036Renfrow4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.4055557,-97.0008316
84A75-OK-60-275-OK119-60-2Renfrow4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.0779583,-97.1216028

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RENFROW 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 RENFROW 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 RENFROW 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 RENFROW 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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Click the image to view it full size.

Competing Series

Soil series competing with RENFROW 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 RENFROW 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 RENFROW 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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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 RENFROW, 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-2012-01-25-17 | Reno County - March 1966

    Cross section of the Nash-Lucien association in the south-central part of the county (Soil Survey of Reno County, Kansas; 1966).

  2. KS-2012-01-25-18 | Reno County - March 1966

    Cross section of the Clark-Ost association showing the topographic relationship of the Clark and Ost soils to the soils of the Renfrow-Vernon association (Soil Survey of Reno County, Kansas; 1966).

  3. OK-2010-09-29-03 | Logan County - 2006

    Typical pattern of soils and underlying material in the Grainola-Renfrow-Piedmont general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).

  4. OK-2010-09-29-07 | Noble County - 2005

    Typical pattern of soils and underlying material in the Grainola-Lucien-Masham general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).

  5. OK-2010-09-29-15 | Oklahoma County - 2004

    Typical pattern of soils and underlying material in the Renfrow-Grainola-Piedmont general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).

  6. 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).

  7. OK-2012-02-16-12 | Cleveland County - April 1987

    Typical pattern of soils and underlying material in the Renfrow-Grainola-Grant map unit and the Port-Weswood map unit (Soil Survey of Cleveland County, Oklahoma; April 1987).

  8. OK-2012-02-16-33 | Garfield County - October 1967

    Typical pattern of soils in the Renfrow-Vernon-Kirkland association (Soil Survey of Garfield County, Oklahoma; October 1967).

  9. OK-2012-02-16-34 | Garfield County - October 1967

    Typical pattern of soils in the Kirkland-Bethany-Tabler association (Soil Survey of Garfield County, Oklahoma; October 1967).

  10. OK-2012-02-17-02 | Lincoln County - January 1970

    Typical pattern of soils in association 3 (Soil Survey of Lincoln County, Oklahoma; January 1970).

  11. 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).

  12. OK-2012-02-17-05 | Logan County - June 1960

    Soils of central and western Logan County on recent alluvium and on loams and sands of Quaternary age. Red beds are exposed in the upper right corner (Soil Survey of Logan County, Oklahoma; June 1960).

  13. 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).

  14. OK-2012-02-17-12 | Major County - October 1968

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

  15. OK-2012-02-17-13 | Major County - October 1968

    Cross section along a line extending across the middle of the county from the western to the eastern boundary (Soil Survey of Major County, Oklahoma; October 1968).

  16. OK-2012-02-17-15 | Oklahoma County - February 1969

    Typical pattern of soils in soil association 2 (Soil Survey of Oklahoma County, Oklahoma; February 1969).

  17. OK-2012-02-17-22 | Pawnee County - March 1959

    Prairie soils of western Pawnee County formed in clay and sandy strata of the Permian "redbeds" area, and in accompanying alluvium (Soil Survey of Pawnee County, Oklahoma; March 1959).

  18. OK-2012-02-17-27 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Renfrow-Coyle-Grainola map unit (Soil Survey of Payne County, Oklahoma; April 1987).

  19. OK-2012-02-17-30 | Payne County - April 1987

    Typical pattern of soils and underlying material in the Norge-Teller-Konawa map unit (Soil Survey of Payne County, Oklahoma; April 1987).

  20. 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 RENFROW 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
Kirkland-Renfrow clay loams, 1 to 3 percent slopes636017982138270230x0wks07719651:24000
Kirkland-Renfrow soils, 1 to 3 percent slopes, eroded6362353213827031hdtbks07719651:24000
Renfrow-Vernon clay loams, 1 to 3 percent slopes6422163713827301hdv6ks07719651:24000
Vernon-Renfrow complex, 3 to 7 percent slopes, eroded644555913827481hdvsks07719651:24000
Renfrow-Grainola complex, 1 to 3 percent slopes64211213827291hdv5ks07719651:24000
Renfrow clay loam, 1 to 3 percent slopes64181679814448352wtxmks09519771:24000
Renfrow silty clay loam, 1 to 3 percent slopes6419185714448362wtxnks09519771:24000
Kirkland-Renfrow clay loams, 1 to 3 percent slopes6360219144482830x0wks09519771:24000
Renfrow-Vernon clay loams, 1 to 3 percent slopes64228214448381khgpks09519771:24000
Renfrow-Grainola complex, 1 to 3 percent slopes64212314448371khgnks09519771:24000
Renfrow-Wellsford clay loams, 1 to 4 percent slopes6423314448392ywswks09519771:24000
Renfrow silty clay loam, 1 to 3 percent slopes64191476814440202wtxnks17319761:24000
Renfrow silty clay loam, 3 to 6 percent slopes6420167214440212ywsvks17319761:24000
Renfrow-Wellsford clay loams, 1 to 4 percent slopes6423152314440222ywswks17319761:24000
Renfrow-Grainola complex, 1 to 3 percent slopes64212621314446661kh94ks19119741:24000
Wellsford-Renfrow clay loams, 2 to 6 percent slopes, eroded5465133114446071kh77ks19119741:24000
Kirkland-Renfrow clay loams, 1 to 3 percent slopes6360523144465430x0wks19119741:24000
Kirkland-Renfrow soils, 1 to 3 percent slopes, eroded63624714446551kh8sks19119741:24000
Renfrow silty clay loam, 1 to 3 percent slopes64193314446652wtxnks19119741:24000
Renfrow clay loam, 1 to 3 percent slopes6418814446642wtxmks19119741:24000
Renfrow silt loam, 0 to 2 percent slopesRcA4585381442dsxlok00319711:24000
Renfrow clay loam, 3 to 5 percent slopes, erodedRcC217239381978dtgwok01719721:24000
Renfrow silt loam, 1 to 3 percent slopesRbB91753819772rj9lok01719721:24000
Renfrow silt loam, 0 to 1 percent slopesRbA2359381976dtgtok01719721:24000
Renfrow silt loam, 1 to 3 percent slopes3781183820212rj9lok01919771:24000
Renfrow silt loam, 3 to 5 percent slopes3826323820222tp5hok01919771:24000
Renfrow-Huska complex, 3 to 5 percent slopes, eroded6510981382128dtmqok02719841:24000
Renfrow-Huska complex, 3 to 5 percent slopes664841382129dtmrok02719841:24000
Renfrow silty clay loam, 3 to 5 percent slopes, eroded6441443821272tp5wok02719841:24000
Renfrow-Urban land-Huska complex, 1 to 5 percent slopes692007382132dtmvok02719841:24000
Renfrow silt loam, 1 to 3 percent slopes6220023821252rj9lok02719841:24000
Renfrow silt loam, 3 to 5 percent slopes6313233821262tp5hok02719841:24000
Renfrow silt loam, 1 to 3 percent slopesRenB7325163672rj9lok03719521:24000
Kirkland-Renfrow complex, 1 to 3 percent slopesKrB968163825012tp5rok04719651:24000
Renfrow silt loam, 3 to 5 percent slopes, eroded63297613825982tp5jok04919821:24000
Renfrow silt loam, 3 to 5 percent slopes, gullied6412006382599dv3xok04919821:24000
Renfrow silt loam, 1 to 3 percent slopes6181043825962rj9lok04919821:24000
Renfrow silt loam, 3 to 5 percent slopes6239133825972tp5hok04919821:24000
Renfrow-Urban land complex, 1 to 5 percent slopes652673826002tp5kok04919821:24000
Renfrow silt loam, 3 to 5 percent slopes, eroded45150303826662tp5jok05119751:24000
Renfrow silt loam, 1 to 3 percent slopes44120783826652rj9lok05119751:24000
Renfrow silt loam, 3 to 5 percent slopes, severely eroded4655843826672tp5lok05119751:24000
Renfrow-Huska complex, 1 to 3 percent slopes471974382668dv64ok05119751:24000
Renfrow silty clay loam, 3 to 5 percent slopes, eroded49176173827392tp5wok05319831:24000
Renfrow silt loam, 3 to 5 percent slopes4889383827382tp5hok05319831:24000
Renfrow-Pawhuska complex, 3 to 5 percent slopes, eroded503817382741dv8hok05319831:24000
Renfrow silt loam, 1 to 3 percent slopesRenB7316014362rj9lok05319831:24000
Renfrow silt loam, 3 to 5 percent slopes, erodedReC212073832402tp5jok06719671:24000
Renfrow silt loam, 3 to 5 percent slopes, severely erodedRfC311873832412tp5lok06719671:24000
Kirkland-Renfrow complex, 3 to 5 percent slopes, erodedKrC241437383334dvwmok07119651:24000
Renfrow-Kirkland complex, 3 to 5 percent slopesRkC5823383363dvxkok07119651:24000
Renfrow, Grainola, and Pawhuska soils, 3 to 8 percent slopes, severely erodedEs17263833282tp5mok07119651:24000
Renfrow silt loam, 1 to 3 percent slopesRenB296234842rj9lok07119651:24000
Renfrow clay loam, 0 to 1 percent slopesRcA8158383412dvz4ok07319601:24000
Renfrow silty clay loam, 3 to 5 percent slopes, erodedRewC2139383836692tp5wok08319941:12000
Renfrow silt loam, 1 to 3 percent slopesRenB82023836672rj9lok08319941:12000
Renfrow silt loam, 3 to 5 percent slopesRenC5553836682tp5hok08319941:12000
Renfrow silt loam, 1 to 3 percent slopesReB8763837352rj9lok08519631:24000
Renfrow silt loam, 3 to 5 percent slopes, eroded41115503837992tp5jok08719761:24000
Renfrow silt loam, 3 to 5 percent slopes4034103837982tp5hok08719761:24000
Renfrow silt loam, 3 to 5 percent slopes, severely eroded4213743838002tp5lok08719761:24000
Renfrow silt loam, 1 to 3 percent slopesRenB57017264172rj9lok08719761:24000
Renfrow silty clay loam, 1 to 3 percent slopesRcB6776383856dwfgok09319651:24000
Renfrow silty clay loam, 0 to 1 percent slopesRcA981383855dwffok09319651:24000
Renfrow silt loam, 1 to 3 percent slopes485243839552rj9lok09919821:24000
Renfrow and Grainola soils, 3 to 5 percent slopes, erodedReGC2247453841062tp5sok10319941:24000
Renfrow silt loam, 1 to 3 percent slopesRenB141293841092rj9lok10319941:24000
Renfrow silt loam, 3 to 5 percent slopesRenC96093841102tp5hok10319941:24000
Renfrow, Grainola, and Pawhuska soils, 3 to 8 percent slopes, severely erodedRGPD345113841052tp5mok10319941:24000
Renfrow loam, 3 to 5 percent slopes, erodedRefC2443841072tp5vok10319941:24000
Renfrow silty clay loam, 3 to 5 percent slopes, erodedRewC2333841112tp5wok10319941:24000
Renfrow silt loam, 3 to 5 percent slopesRenC13253842002tp5hok10719961:24000
Renfrow silt loam, 1 to 3 percent slopesRenB58543843482rj9lok10919961:12000
Renfrow silt loam, 3 to 5 percent slopes, erodedRenC21029714231852tp5jok11720071:24000
Renfrow silt loam, 1 to 3 percent slopesRenB926314231832rj9lok11720071:24000
Renfrow silt loam, 3 to 5 percent slopesRenC871714129942tp5hok11720071:24000
Renfrow, Grainola, and Pawhuska soils, 3 to 8 percent slopes, severely erodedRGPD3251916770332tp5mok11720071:24000
Renfrow loam, 3 to 5 percent slopes, erodedRefC21919017612tp5vok11720071:24000
Renfrow loam, 3 to 5 percent slopes, eroded47140383845452tp5vok11919831:24000
Renfrow and Grainola soils, 3 to 8 percent slopes, severely eroded499496384547dx4rok11919831:24000
Renfrow silt loam, 3 to 5 percent slopes4650223845442tp5hok11919831:24000
Renfrow silt loam, 1 to 3 percent slopes4541513845432rj9lok11919831:24000
Renfrow-Urban land complex, 1 to 5 percent slopes8031533845822tp5kok11919831:24000
Renfrow silt loam, 1 to 3 percent slopes3677983846972rj9lok12519751:24000
Renfrow silt loam, 3 to 5 percent slopes3759123846982tp5hok12519751:24000
Kirkland-Renfrow complex, 1 to 3 percent slopesKrB237943848662tp5rok13719601:24000
Renfrow and Pawhuska soils, 1 to 5 percent slopes, severely erodedEs5247384860dxgvok13719601:24000
Renfrow and Kirkland soils, 1 to 5 percent slopes, erodedRfB24764384880dxhhok13719601:24000
Renfrow silt loam, 3 to 5 percent slopesReC31163848792tp5hok13719601:24000
Renfrow-Kirkland-Anocon association, nearly level4585489363899d6nptx07719771:24000
Renfrow-Waurika complex, 0 to 2 percent slopes4640059363900d6nqtx07719771:24000
Renfrow loam, 1 to 4 percent slopes2836106370773dftftx33719751:24000
Waurika-Renfrow complex, 0 to 1 percent slopes4114511370788dftxtx33719751:24000
Renfrow loam, 1 to 3 percent slopesReB4257373382djjltx48519721:20000
Renfrow loam, 0 to 1 percent slopesReA579373381djjktx48519721:20000
Renfrow-Urban land complex, 1 to 5 percent slopesRfB5313733832tp5ktx48519721:20000

Map of Series Extent

Approximate geographic distribution of the RENFROW 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 .