Official Series Description


Lab Data Summary

Aggregate lab data for the RENTHIN soil series. This aggregation is based on all pedons with a current taxon name of RENTHIN, 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 RENTHIN 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
7904KS09500104KS095001Renthin3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6036644,-97.904953
84A91P0902S1996OK109065Renthin7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.57251,-97.49033

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RENTHIN 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 RENTHIN 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 RENTHIN 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 RENTHIN 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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Competing Series

Soil series competing with RENTHIN 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 RENTHIN 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 RENTHIN 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 RENTHIN, 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-2010-09-29-16 | Oklahoma County - 2004

    Typical pattern of soils and underlying material in the Kirkland-Urban land-Renthin general soil map unit (Soil Survey of Oklahoma County, Oklahoma; 2004).

Map Units

Map units containing RENTHIN 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
Renthin silty clay loam, 1 to 3 percent slopesRcB168983817652tp6fok01119651:24000
Renthin-Grainola complex, 3 to 5 percent slopes, erodedRnC213641381766dt81ok01119651:24000
Renthin silty clay loam, 0 to 1 percent slopesRcA2257381764dt7zok01119651:24000
Renthin-Masham complex, 3 to 5 percent slopes, erodedRvC250768382527dv1lok04719651:24000
Renthin clay loam, 1 to 3 percent slopesRfB20933825252tp6hok04719651:24000
Renthin clay loam, 0 to 1 percent slopesRfA1782382524dv1hok04719651:24000
Renthin clay loam, 1 to 3 percent slopesRcB496603834132tp6hok07319601:24000
Renthin-Grainola complex, 3 to 5 percent slopes, severely erodedRvC345226383531dw2zok08119661:24000
Renthin silty clay loam, 3 to 5 percent slopes, erodedRfC2169323835302tp6dok08119661:24000
Renthin silt loam, 1 to 3 percent slopesReB55313835282tp6gok08119661:24000
Renthin silt loam, 3 to 5 percent slopesReC4734383529dw2xok08119661:24000
Renthin silty clay loam, 3 to 5 percent slopes, erodedRnnC249853836712tp6dok08319941:12000
Renthin silt loam, 1 to 3 percent slopesRinB23453836702tp6gok08319941:12000
Renthin silt loam, 3 to 5 percent slopes49140383956dwjpok09919821:24000
Renthin-Urban land complex, 1 to 5 percent slopesRnUC21369384350dwydok10919961:12000
Renthin silty clay loam, 3 to 5 percent slopes, erodedRnnC2122353843522tp6dok10919961:12000
Renthin silt loam, 1 to 3 percent slopesRinB56383843492tp6gok10919961:12000
Renthin silty clay loam, 1 to 3 percent slopesRnnB25243843512tp6fok10919961:12000

Map of Series Extent

Approximate geographic distribution of the RENTHIN 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 .