Official Series Description


Lab Data Summary

Aggregate lab data for the RIGLEY soil series. This aggregation is based on all pedons with a current taxon name of RIGLEY, 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 RIGLEY 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
12504KY-025-UK104KY-025-001Rigley4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.5410919,-83.3439026
12595KY-119-00395KY-119-003Rigley1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.3667336,-83.0432053
n/a65KY-125-06812KY-125-001Rigley4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCA-0291978-OH019-029Rigley5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJK-0141979-OH079-014Rigley5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a65KY-125-07065KY-125-070Rigley4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a67KY-205-00567KY-205-005Rigley3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a81KY-109-00481KY-109-004Rigley4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RIGLEY 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 RIGLEY 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 RIGLEY 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 RIGLEY 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 RIGLEY 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 RIGLEY 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 RIGLEY 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 RIGLEY, 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-2010-09-03-43 | Magoffin and Morgan Counties - 2002

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

  2. KY-2010-09-03-44 | Magoffin and Morgan Counties - 2002

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

  3. 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).

  4. KY-2012-01-27-25 | Carter County - April 1983

    Pattern of soils, topography, and underlying material in the Rigley-Lily-Rock outcrop map unit (Soil Survey of Carter County, Kentucky; April 1983).

  5. KY-2012-01-31-12 | Jackson and Owsley Counties - April 1989

    Typical pattern of soils and parent material in the Shelocta-Gilpin map unit (Soil Survey of Jackson and Owsley Counties, Kentucky; April 1989).

  6. KY-2012-01-31-26 | Knox County and Eastern Part of Whitley County - May 1988

    Pattern of soils, topography, and underlying material in the Rigley-Lily-Shelocta map unit (Soil Survey of Knox County and Eastern Part of Whitley County, Kentucky; May 1988).

  7. 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).

  8. KY-2012-02-01-30 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

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

  9. KY-2012-02-01-70 | Wayne County - March 1990

    The relationship of soils to topography and underlying material in the Caneyville-Rock outcrop-Rigley-Shelocta general soil map unit (Soil Survey of Wayne County, Kentucky; March 1990).

  10. OH-2010-09-29-13 | Coshocton County - 2001

    Typical pattern of soils and parent material in the Coshocton-Westmoreland-Rigley association (Soil Survey of Coshocton County, Ohio; 2001).

  11. OH-2010-09-29-14 | Coshocton County - 2001

    Typical pattern of soils and parent material in the Coshocton-Brownsville-Westmoreland association (Soil Survey of Coshocton County, Ohio; 2001).

Map Units

Map units containing RIGLEY 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
Rigley-Rock outcrop association, steepRSF5145550257lgl7ky04319801:20000
Rigley-Rock outcrop complex, 30 to 70 percent slopesRgF672818846692184sky06320071:12000
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF1841929970762qyt0ky19919691:12000
Shelocta-Highsplint-Rigley complex, 30 to 50 percent slopes, stony, rockyuShrF1118829970792qytdky19919691:12000
Rigley-Shelocta-Muse complex, steepRMF47145550083lgdmky23119851:20000
Rigley-Rock outcrop association, steepRCF17397550712lh1xky62319851:20000
Shelocta-Highsplint-Rigley complex, 30 to 50 percent slopes, stony, rockyuShrF5290529970802qytdky62819731:20000
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF1976129970772qyt0ky62819731:20000
Shelocta-Rigley complex, 20 to 30 percent slopesSgE8677552295ljpzky62819731:20000
Rigley stony fine sandy loam, 30 to 60 percent slopesRgF6452552287ljpqky62819731:20000
Shelocta-Highsplint-Rigley complex, 30 to 50 percent slopes, stony, rockyuShrF3214429970812qytdky63019661:15840
Rigley-Shelocta-Alticrest complex, 20 to 80 percent slopes, stony, very rockyuRshF2404029970782qyt0ky63019661:15840
Lily-Gilpin-Rigley complex, 15 to 35 percent slopesLyE1593550844lh65ky63419891:20000
Rigley-Rock outcrop complex, 30 to 70 percent slopesRoF880550878lh78ky63919911:24000
Rigley-Rock outcrop complex, 30 to 70 percent slopesRoF614550912lh8cky64019961:24000
Rigley-Rock outcrop complex, 25 to 60 percent slopesRlF11157550953lh9pky64119941:24000
Rigley stony fine sandy loam, 30 to 60 percent slopesRlF2655014788231lmtzky64519711:20000
Rigley-Donahue complex, 30 to 60 percent slopesRoF1025014788211lmtxky64519711:20000
Rigley gravelly fine sandy loam, 20 to 30 percent slopesRgE191014788181lmttky64519711:20000
Rigley-Donahue complex, 20 to 30 percent slopesRoE169014788201lmtwky64519711:20000
Rigley gravelly fine sandy loam, 12 to 20 percent slopesRgD34014788171lmtsky64519711:20000
Rigley gravelly fine sandy loam, 2 to 6 percent slopesRgB28014788151lmtqky64519711:20000
Rigley-Donahue complex, 6 to 20 percent slopesRoD24014788191lmtvky64519711:20000
Rigley gravelly fine sandy loam, 6 to 12 percent slopesRgC21014788161lmtrky64519711:20000
Rigley sandy loam, 6 to 12 percent slopesRrC1802881909nwgoh00519761:15840
Rigley sandy loam, 15 to 25 percent slopesRgD84815380052t32voh01919811:15840
Rigley sandy loam, 8 to 15 percent slopesRgC69925380042t32toh01919811:15840
Rigley sandy loam, 25 to 40 percent slopesRgE3207538006l1v1oh01919811:15840
Rigley sandy loam, 3 to 8 percent slopesRgB7465380032t32soh01919811:15840
Rigley loam, 25 to 40 percent slopesReE53816700261t1stoh01919811:15840
Rigley loam, 15 to 25 percent slopesReD10416700251t1ssoh01919811:15840
Rigley sandy loam, 15 to 25 percent slopesRgD85135366832t32voh03119961:15840
Rigley sandy loam, 25 to 35 percent slopesRgE4094536684l0gdoh03119961:15840
Rigley sandy loam, 6 to 15 percent slopesRgC39755366822t32roh03119961:15840
Coshocton-Rigley complex, 25 to 35 percent slopesCrE1510536623l0dfoh03119961:15840
Rigley sandy loam, 12 to 25 percent slopes, very stonyRhD491536685l0gfoh03119961:15840
Coshocton-Rigley complex, 15 to 25 percent slopesCrD158536622l0ddoh03119961:15840
Rigley-Coshocton complex, 25 to 40 percent slopesRkE77210896528sk4oh03119961:15840
Rigley channery loam, 15 to 25 percent slopesRdD31210896428sk3oh03119961:15840
Rigley sandy loam, 25 to 40 percent slopesRlE23210898628sktoh03119961:15840
Rigley loam, 8 to 15 percent slopesRfC19210896328sk2oh03119961:15840
Rigley fine sandy loam, 25 to 35 percent slopesReF8210899728sl5oh03119961:15840
Rigley-Latham association, steepRgLZE12024504522n7wvoh05319881:15840
Rigley loam, 25 to 40 percent slopesRgE342536773l0k8oh06719931:15840
Rigley loam, 15 to 25 percent slopesRgD84536772l0k7oh06719931:15840
Rigley sandy loam, 15 to 25 percent slopesRgD36802869322t32voh07519891:15840
Rigley sandy loam, 8 to 15 percent slopesRgC35052869312t32toh07519891:15840
Rigley sandy loam, 3 to 8 percent slopesRgB9002869302t32soh07519891:15840
Rigley sandy loam, 6 to 15 percent slopesRfC17816770082t32roh07519891:15840
Rigley sandy loam, 2 to 6 percent slopesRfB2316773582t32poh07519891:15840
Rigley-Latham association, steepRgLZE11245524510512n8j5oh07919811:15840
Rigley-Clymer association, steepRmE10609536042kzspoh07919811:15840
Rigley-Latham complex, 15 to 25 percent slopesRgLXD1643124510492n8j3oh07919811:15840
Rigley-Rock outcrop association, very steepRrG4905536044kzsroh07919811:15840
Rigley sandy loam, 15 to 25 percent slopesRgD3772536040kzsmoh07919811:15840
Rigley sandy loam, 8 to 15 percent slopesRgC1776536039kzsloh07919811:15840
Rigley-Rarden complex, 15 to 25 percent slopesRgRXD188624510502n8j4oh07919811:15840
Rigley-Rarden association, steepRgRZE141324510522n8j6oh07919811:15840
Rigley sandy loam, 8 to 15 percent slopesRgC219536110kzvwoh08119871:15840
Rigley sandy loam, 15 to 25 percent slopesRgD130536111kzvxoh08119871:15840
Rigley sandy loam, 12 to 18 percent slopesRgD1799614621nmkhoh08319831:15840
Rigley sandy loam, 6 to 12 percent slopesRgC17826146202t32qoh08319831:15840
Rigley sandy loam, 2 to 6 percent slopesRgB5576146192t32poh08319831:15840
Rigley-Coshocton complex, 18 to 25 percent slopesRhE413614622nmkjoh08319831:15840
Rigley sandy loam, 8 to 15 percent slopesReC5915930662t32toh08319831:15840
Coshocton-Rigley complex, 15 to 25 percent slopesCxD3322160052dcy1oh08319831:15840
Rigley sandy loam, 15 to 25 percent slopesRyD2822160202t32voh08319831:15840
Rigley sandy loam, 15 to 25 percent slopesReD1215930671qgq8oh08319831:15840
Rigley sandy loam, 6 to 15 percent slopesRyC1122160192t32roh08319831:15840
Rigley-Latham association, steepRgLZE188924511792n8n9oh08719891:15840
Rigley-Latham complex, 15 to 25 percent slopesRgLXD125024511142n8l6oh08719891:15840
Rigley-Coshocton complex, 18 to 25 percent slopesRhE17651710765r0loh08919861:15840
Rigley fine sandy loam, 12 to 18 percent slopesRgD15551710735r0hoh08919861:15840
Rigley fine sandy loam, 18 to 25 percent slopesRgE14301710745r0joh08919861:15840
Rigley fine sandy loam, 6 to 12 percent slopesRgC12851710725r0goh08919861:15840
Rigley fine sandy loam, 25 to 35 percent slopesRgF8601710755r0koh08919861:15840
Rigley channery loam, 15 to 25 percent slopesRdD14215407741nq9doh08919861:15840
Rigley-Coshocton complex, 25 to 40 percent slopesRhF4015407751nq9foh08919861:15840
Rigley sandy loam, 15 to 25 percent slopesReD3922160502t32voh08919861:15840
Rigley loam, 8 to 15 percent slopesRfC3915407731nq9coh08919861:15840
Rigley-Coshocton complex, 25 to 40 percent slopesRhE8642537933l1rpoh11919891:15840
Rigley channery loam, 15 to 25 percent slopesRgD8171537932l1rnoh11919891:15840
Rigley loam, 8 to 15 percent slopesRfC3747537931l1rmoh11919891:15840
Shelocta-Rigley association, steepSoF9719537724l1jyoh13119841:15840
Rigley-Rock outcrop association, very steepRnF39616890411tpl6oh13119841:15840
Rigley-Clymer association, steepRkE416890401tpl5oh13119841:15840
Shelocta-Rigley association, steepSkE10721709615qwwoh14119971:15840
Rigley-rock outcrop association, very steepRcF651709485qwgoh14119971:15840
Rigley sandy loam, 25 to 40 percent slopesRgE2320536334l033oh15719811:15840
Rigley sandy loam, 15 to 25 percent slopesRgD8305363332t32voh15719811:15840
Rigley sandy loam, 8 to 15 percent slopesRgC2405363322t32toh15719811:15840
Rigley sandy loam, 6 to 15 percent slopesRiC4115894002t32roh15719811:15840
Rigley-Weikert-Berks complex, 15 to 25 percent slopes, very stony37D2868518852kdx5va18719801:15840
Rigley sandy loam, 25 to 60 percent slopes, very stony36E1396518851kdx4va18719801:15840

Map of Series Extent

Approximate geographic distribution of the RIGLEY 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 .