Official Series Description


Lab Data Summary

Aggregate lab data for the RADLEY soil series. This aggregation is based on all pedons with a current taxon name of RADLEY, 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 RADLEY 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
11240A47381960OK131001Radley6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2208328,-95.7086105
112M04217022004MO217002Radley4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8218056,-94.5119444
11240A473960OK131002Radley6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.2041664,-95.7447205
116BM95097031995MO097003Radley4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2955556,-94.3894444

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RADLEY 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 RADLEY 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 RADLEY 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 RADLEY 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 RADLEY 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 RADLEY series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

Click the image to view it full size.

Geomorphic description summaries for the RADLEY 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 .

There are insufficient data to create the 2D hillslope position figure.

There are insufficient data to create the 3D hills figure.

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 RADLEY, 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-2012-01-20-40 | Crawford County - December 1973

    Typical cross section of the major soils that formed in material weathered from acid clayey and sandy shale or sandstone or in alluvium derived from these materials. These soils are in associations 1, 2, 3, and 4 (Soil Survey of Crawford County, Kansas; 1973).

Map Units

Map units containing RADLEY 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
Radley-Hepler silt loams, frequently flooded8241566813869841hk8fks03719691:24000
Radley silt loam, occasionally flooded8240487113869831hk8dks03719691:24000
Hepler-Radley complex, 1 to 3 percent slopes, occasionally flooded461121316625798532wqgjmo01119691:24000
Radley-Verdigris soils, 0 to 2 percent slopes, occasionally flooded460208037886827yrtbmo01119691:24000
Hepler-Radley complex, 0 to 1 percent slopes, occasionally flooded46012147025325402wqgkmo01119691:24000
Radley-Verdigris complex, 1 to 3 percent slopes, occasionally flooded4612081925798402q014mo01119691:24000
Radley silty clay loam, 0 to 2 percent slopes, occasionally flooded460219637886776yrrpmo21719741:24000
Hepler-Radley complex, 1 to 3 percent slopes, occasionally flooded46112397525798542wqgjmo21719741:24000
Hepler-Radley complex, 0 to 1 percent slopes, occasionally flooded46012358925325412wqgkmo21719741:24000
Radley silt loam, 0 to 1 percent slopes, occasionally floodedRa98701065232w223ok03519681:20000
Eram-Radley complex, 0 to 8 percent slopesErD186921065872ydt8ok10519751:24000
Radley silt loam, 0 to 1 percent slopes, frequently floodedRD171941065982w222ok10519751:24000
Radley silt loam, 0 to 1 percent slopes, occasionally floodedRa22571065992w223ok10519751:24000
Eram-Radley complex, 0 to 12 percent slopesErRE59803841552ydt7ok10719961:24000
Dennis-Radley complex, 0 to 12 percent slopes16252581066962wqf7ok14319751:12000
Radley silt loam, 0 to 1 percent slopes, frequently flooded48135141067312w222ok14319751:12000
Radley silt loam, 0 to 1 percent slopes, occasionally flooded4753981067302w223ok14319751:12000
Dennis-Radley complex, 0 to 15 percent slopesDxE333991067612wqf9ok14519721:24000
Radley silt loam, 0 to 1 percent slopes, occasionally floodedRa70661067862w223ok14519721:24000
Radley silt loam, 0 to 1 percent slopes, frequently floodedRc70161067872w222ok14519721:24000

Map of Series Extent

Approximate geographic distribution of the RADLEY 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 .