Official Series Description


Lab Data Summary

Aggregate lab data for the RENOX soil series. This aggregation is based on all pedons with a current taxon name of RENOX, 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 RENOX 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
12289KY-057-00789KY-057-007Renox4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7500801,-85.2968903
12289KY-057-00589KY057 Renox-OSDRenox4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.8782921,-85.4011536

Water Balance

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

Soil series competing with RENOX 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 RENOX 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 RENOX 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 terrace figure.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with RENOX, 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. KY-2010-09-03-13 | Knott and Letcher Counties - 2004

    Typical pattern of soils and their relationship to geology and topography in the Kimper-Cloverlick-Renox-Highsplint general soil map unit in Letcher County (Soil Survey of Knott and Letcher Counties, Kentucky; 2004).

  2. KY-2010-09-03-25 | Cumberland County - 1998

    Relationship of the soils in Garmon-Newbern-Carpenter general soil map unit and the underlying material (Soil Survey of Cumberland County, Kentucky; 1998).

  3. KY-2012-01-26-26 | Bell and Harlan Counties - December 1992

    Typical pattern of soils in the Kimper-Shelocta-Varilla general soil map unit, showing the relationship of the soils to parent material and topography (Soil Survey of Bell and Harlan Counties, Kentucky; December 1992).

  4. TN-2010-11-02-03 | Clay County - 2004

    The relatiohship between soils and landscape in the Dellrose-Renox-Barfield and Garmon-Newbern general soil map units (Soil Survey of Clay County, Tennessee; 2004)

Map Units

Map units containing RENOX 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
Renox-Faywood complex, 20 to 50 percent slopes, erodedRfF29695551470lhvcky05719911:20000
Renox gravelly loam, 6 to 12 percent slopes, erodedReC24595551468lhv9ky05719911:20000
Renox gravelly loam, 12 to 25 percent slopes, erodedReD2770551469lhvbky05719911:20000
Renox-Rock outcrop complex, 30 to 70 percent slopesReF132918846682184rky06320071:12000
Renox silt loam, 6 to 12 percent slopesRaC350549780lg2vky16919651:15840
Kimper-Cloverlick-Renox complex, 30 to 80 percent slopes, extremely stonyKrF3243550743lh2xky62619971:24000
Caneyville-Renox-Bledsoe complex, 50 to 80 percent slope, extremely stonyCbF1711550723lh28ky62619971:24000
Kimper-Renox-Sharondale complex, very rocky, 35 to 75 percent slopesKrF4725552125ljjhky63819891:24000
Renox gravelly fine sandy loam, 2 to 6 percent slopesReB37014788131lmtnky64519711:20000
Renox gravelly fine sandy loam, 6 to 12 percent slopesReC24014788141lmtpky64519711:20000
Renox silt loam, 5 to 12 percent slopes, erodedReC21929531138ktphtn02720021:24000
Renox silt loam, 2 to 5 percent slopesReB475636792pcmptn02720021:24000

Map of Series Extent

Approximate geographic distribution of the RENOX 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 .