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 (updated 2020-03-13). Methods used to assemble the KSSL snapshot used by SoilWeb / SDE
Pedons used in the lab summary:
MLRA | Lab ID | Pedon ID | Taxonname | CI | NSSL / NASIS Reports | Link To SoilWeb GMap |
---|---|---|---|---|---|---|
80A | 72-OK-60-1 | 72-OK119-60-1 | Renfrow | 4 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 36.1517278,-97.2946556 |
80A | 90P0946 | 90OK103001 | Renfrow | 8 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 36.3025017,-97.3152771 |
80A | 91P0906 | 91OK109005 | Renfrow | 7 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 35.6947212,-97.6005554 |
80A | 40A4722 | S1953OK117036 | Renfrow | 4 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 36.4055557,-97.0008316 |
84A | 75-OK-60-2 | 75-OK119-60-2 | Renfrow | 4 | Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties | 36.0779583,-97.1216028 |
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.
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 (updated 2024-10-24), parsed OSD records (updated 2025-02-20) and snapshot of SC database (updated 2025-02-20).
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 (updated 2024-10-23).
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 (updated 2024-10-23).
There are insufficient data to create the 3D mountains figure.
Soil series competing with RENFROW share the same family level classification in Soil Taxonomy. Source: parsed OSD records (updated 2025-02-20) and snapshot of the SC database (updated 2025-02-20).
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 (updated 2024-10-23).
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 (updated 2024-10-23).
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 (updated 2025-02-20).
Click a link below to display the diagram. Note that these diagrams may be from multiple survey areas.
Cross section of the Nash-Lucien association in the south-central part of the county (Soil Survey of Reno County, Kansas; 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).
Typical pattern of soils and underlying material in the Grainola-Renfrow-Piedmont general soil map unit (Soil Survey of Logan County, Oklahoma; 2006).
Typical pattern of soils and underlying material in the Grainola-Lucien-Masham general soil map unit (Soil Survey of Noble County, Oklahoma; 2005).
Typical pattern of soils and underlying material in the Renfrow-Grainola-Piedmont general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).
Typical pattern of soils in associations 1, 3, 4, and 6 (Soil Survey of Blaine County, Oklahoma; February 1968).
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).
Typical pattern of soils in the Renfrow-Vernon-Kirkland association (Soil Survey of Garfield County, Oklahoma; October 1967).
Typical pattern of soils in the Kirkland-Bethany-Tabler association (Soil Survey of Garfield County, Oklahoma; October 1967).
Typical pattern of soils in association 3 (Soil Survey of Lincoln County, Oklahoma; January 1970).
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).
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).
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).
Soil associations in the central part of the county (Soil Survey of Major County, Oklahoma; 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).
Typical pattern of soils in soil association 2 (Soil Survey of Oklahoma County, Oklahoma; February 1969).
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).
Typical pattern of soils and underlying material in the Renfrow-Coyle-Grainola map unit (Soil Survey of Payne County, Oklahoma; April 1987).
Typical pattern of soils and underlying material in the Norge-Teller-Konawa map unit (Soil Survey of Payne County, Oklahoma; April 1987).
Typical pattern of soils in associations 6, 7, and 8 (Soil Survey of Stephens County, Oklahoma; 1964).
Map units containing RENFROW as a major component. Limited to 250 records.
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 (updated 2024-10-30).