Official Series Description


Lab Data Summary

Aggregate lab data for the DONAHUE soil series. This aggregation is based on all pedons with a current taxon name of DONAHUE, 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 DONAHUE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

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Soil series sharing subgroup-level classification with DONAHUE, 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. =HYPERLINK(CONCATENATE(M51,E51)) | Mammoth Cave National Park - 2010

    Typical pattern of soils and underlying material in the Wallen-Caneyville-Bledsoe general soil map unit (Soil Survey of Mammoth Cave National Park, Kentucky; 2010).

  2. KY-2010-09-03-45 | Magoffin and Morgan Counties - 2002

    Typical pattern of soils and their relationship to geology and topography in the Rigley-Bledsoe-Alticrest-Berks general soil map unit in Morgan County (Soil Survey of Magoffin and Morgan Counties, Kentucky; 2002).

  3. KY-2010-09-10-10 | Butler and Edmonson Counties -

    Relationship of soils to topography and underlying material in the Johnsburg-Clarkrange association (Soil Survey of Butler and Edmonson Counties, Kentucky).

  4. KY-2010-09-10-11 | Butler and Edmonson Counties -

    Relationship of soils to topography and underlying material in the Wallen-Caneyville association (Soil Survey of Butler and Edmonson Counties, Kentucky).

  5. KY-2012-02-01-29 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Rigley-Brookside-Steinsburg association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

Map Units

Map units containing DONAHUE 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
Hayter-Donahue complex, 15 to 40 percent slopes, very rockyuHadF86025170332q97qky05319901:20000
Hayter-Donahue complex, 15 to 40 percent slopes, very rockyuHadF168225170312q97qky23119851:20000
Donahue rocky sandy loam, 40 to 75 percent slopesDoF1670552264ljnzky62819731:20000
Bledsoe-Donahue-Rock outcrop complex, 15 to 30 percent slopesBeE479550929lh8xky64119941:24000
Rigley-Donahue complex, 30 to 60 percent slopesRoF1025014788211lmtxky64519711:20000
Rigley-Donahue complex, 20 to 30 percent slopesRoE169014788201lmtwky64519711:20000
Rigley-Donahue complex, 6 to 20 percent slopesRoD24014788191lmtvky64519711:20000
Wallen-Bledsoe-Donahue complex, 35 to 50 percent slopes, very rockyWbF792023792292kvsbky64820091:12000
Wallen-Bledsoe-Donahue complex, 15 to 35 percent slopes, very rockyWbE645723792282kvs9ky64820091:12000
Wallen-Bledsoe-Donahue complex, 35 to 50 percent slopes, very rockyWbF420324529122nbg6ky70919951:20000
Wallen-Bledsoe-Donahue complex, 15 to 35 percent slopes, very rockyWbE342324529112nbg5ky70919951:20000
Hayter-Donahue complex, 15 to 40 percent slopes, very rockyuHadF366525170342q97qtn13320031:24000
Hayter-Donahue complex, 15 to 40 percent slopes, very rockyuHadF1383625170322q97qtn70119851:24000

Map of Series Extent

Approximate geographic distribution of the DONAHUE 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 .