Official Series Description


Lab Data Summary

Aggregate lab data for the RADDLE soil series. This aggregation is based on all pedons with a current taxon name of RADDLE, 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 RADDLE 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
105X49-977-1S1988IA097039Raddle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties42.0729602,-90.8183273
115B81P0040S1980IL157134RADDLE6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0683327,-90.0888901
115C81IL0130021981IL013002Raddle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.0882231,-90.6115039
115C85P007983IL195225Raddle6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8391685,-90.0338898
n/a78IL1570331978IL157033Raddle4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a80IL1570391980IL157039Raddle2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RADDLE 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 RADDLE 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 RADDLE 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 RADDLE 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 RADDLE 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 RADDLE 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 RADDLE 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.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with RADDLE, 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. IL-2010-09-01-69 | Schuyler County - 2003

    Typical pattern of soils and underlying material in the Wakeland-Wilbur association (Soil Survey of Schuyler County, Illinois; 2003).

  2. IL-2011-06-01-06 | Brown County - 1988

    Typical cross section showing the relationship of parent material to soils in Brown County (Soil Survey of Brown County, Illinois; 1988).

Map Units

Map units containing RADDLE 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
Raddle silt loam, 0 to 2 percent slopes9762022403448fjtgia02319781:15840
Raddle silt loam, 2 to 5 percent slopes976B276403449fjthia02319781:15840
Raddle silt loam, 1 to 3 percent slopes976358403898fk8zia03319781:15840
Raddle silt loam, 0 to 2 percent slopes9761450404481fkwsia04519781:15840
Raddle silt loam, 0 to 2 percent slopes976189406058fmjnia06719891:15840
Raddle silt loam, 1 to 4 percent slopes976B777407582fp3tia09719881:15840
Raddle silt loam, 1 to 3 percent slopes9761147408070fpmkia10319791:15840
Raddle silt loam, 0 to 2 percent slopes9761214408224fpsjia10519881:15840
Raddle silt loam, 2 to 5 percent slopes976B383408225fpskia10519881:15840
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B10961729805t00il00919841:12000
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B237125420352qr9til01319861:15840
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B18852628188th0il01720031:12000
Raddle silt loam, 5 to 10 percent slopes430C3612628198th1il01720031:12000
Raddle silt loam, 0 to 2 percent slopes, frequently flooded3430A18461748315vxqil03519921:15840
Raddle silt loam, 0 to 3 percent slopes430A7711734095tfvil05119911:15840
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B171014537731ksrxil05719971:12000
Raddle silt loam, 0 to 2 percent slopes430A4274632704p7ctil07120051:12000
Raddle silt loam, 2 to 5 percent slopes430B972632705p7cvil07120051:12000
Raddle silt loam, 2 to 5 percent slopes430B58724469386mbil07320011:12000
Raddle silt loam, 0 to 2 percent slopes430A35324469286m9il07320011:12000
Raddle silt loam, 0 to 2 percent slopes, rarely flooded7430A69915398221np9pil07720061:12000
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B2181194988023g0cil08519901:12000
Raddle silt loam, 0 to 2 percent slopes, rarely flooded7430A6771989346p07il11920011:12000
Raddle silt loam, 2 to 5 percent slopes430B2171777995z0gil12519891:15840
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B16625185972qj4zil12519891:15840
Raddle silt loam, 0 to 2 percent slopes430A524624498786xtil13120001:12000
Raddle silt loam, 2 to 5 percent slopes430B353224498886xvil13120001:12000
Raddle-Sparta complex, 2 to 5 percent slopes899B221124501286ymil13120001:12000
Raddle silt loam, 0 to 2 percent slopes, rarely flooded7430A38418411165l2il13319981:12000
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B38832013036rgnil14920011:12000
Raddle silt loam, 0 to 2 percent slopes, rarely flooded7430A5802005616qpqil15720011:12000
Raddle silt loam, 0 to 2 percent slopes430A34941987246nsgil16120021:12000
Raddle silt loam, 2 to 5 percent slopes430B23741987256nshil16120021:12000
Raddle silt loam, 2 to 5 percent slopes, rarely flooded7430B16012022386sftil16920001:12000
Raddle silt loam, 2 to 5 percent slopes430B56124489386tsil18720021:12000
Raddle silt loam, 0 to 2 percent slopes430A4547793068vm7vil19520031:12000
Raddle silt loam, 2 to 5 percent slopes430B1805793069vm7wil19520031:12000

Map of Series Extent

Approximate geographic distribution of the RADDLE 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 .