Official Series Description


Lab Data Summary

Aggregate lab data for the RINEY soil series. This aggregation is based on all pedons with a current taxon name of RINEY, 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 RINEY 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
n/a83P08951983KY099005Riney5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a83KY-099-00583KY-099-005Riney4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the RINEY 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 RINEY 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 RINEY 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 RINEY 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 flats position figure.

Competing Series

Soil series competing with RINEY 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 RINEY 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 RINEY 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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Soil series sharing subgroup-level classification with RINEY, 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-2010-09-03-46 | Magoffin and Morgan Counties - 2002

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

  3. KY-2012-01-30-22 | Hart County - May 1993

    Typical pattern of soils and underlying material in the Riney-Sonora-Canmer general soil map unit (Soil Survey of Hart County, Kentucky; May 1993).

  4. KY-2012-05-09-04 | Mammoth Cave National Park - 2010

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

Map Units

Map units containing RINEY 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
Riney loam, 12 to 35 percent slopesRmcE1224115245017p6tin06120071:12000
Riney loam, 6 to 12 percent slopesRnC83115924301qg1qky00120061:12000
Riney loam, 2 to 6 percent slopesRnB5115924291qg1pky00120061:12000
Riney loam, 12 to 20 percent slopes, erodedReD26945490752zs5rky04719771:20000
Riney loam, 6 to 12 percent slopes, erodedReC24535490742zs5qky04719771:20000
Riney clay loam, 12 to 30 percent slopes, severely erodedRmE3421549076lfc4ky04719771:20000
Riney loam, 6 to 12 percent slopes, erodedReC26405487202zs5qky14119721:20000
Riney loam, 2 to 6 percent slopesReB1475487192zs5pky14119721:20000
Riney-Christian complex, 20 to 35 percent slopes, erodedRcE21110552364ljs6ky15519861:20000
Riney loam, 6 to 12 percent slopesRaC640552363ljs5ky15519861:20000
Riney loam, 6 to 12 percent slopes, erodedReC25905511762zs5qky21919841:20000
Riney gravelly loam, 12 to 30 percent slopes, severely erodedRmE3290551178lhjyky21919841:20000
Riney loam, 12 to 20 percent slopes, erodedReD21405511772zs5rky21919841:20000
Riney loam, 6 to 12 percent slopesRnC1773550418lgrfky60519751:20000
Riney-Lily complex, 12 to 20 percent slopesReD860549613lfxgky60719921:20000
Riney loam, 6 to 12 percent slopes, erodedRaC2824549612lfxfky60719921:20000
Riney-Lily complex, 20 to 30 percent slopesReE731549614lfxhky60719921:20000
Riney loam, 6 to 12 percent slopesReC5183552575lk00ky62019791:20000
Riney loam, 12 to 20 percent slopesReD1418552576lk01ky62019791:20000
Riney sandy clay loam, 6 to 20 percent slopes, severely erodedRcD34830551066lhfbky62119751:20000
Riney loam, 12 to 20 percent slopesRbD3880551064lhf8ky62119751:20000
Riney loam, 6 to 12 percent slopesRbC3510551063lhf7ky62119751:20000
Gullied land (riney)Gu2145551042lhdkky62119751:20000
Riney loam, 20 to 30 percent slopesRbE1285551065lhf9ky62119751:20000
Riney-Allegheny complex, 4 to 12 percent slopesReC900550713lh1yky62319851:20000
Riney-Ezel complex, 6 to 20 percent slopesRnD357550954lh9qky64119941:24000
Nolichucky fine sandy loam, 6 to 12 percent slopes, eroded (riney)NoC237324530012nbk2ky64619661:15840
Nolichucky fine sandy loam, 2 to 6 percent slopes (riney)NoB31224530002nbk1ky64619661:15840
Riney loam, karst, 12 to 20 percent slopes, erodedRnD2721524530992nbn7ky64719891:20000
Riney loam, 12 to 20 percent slopes, erodedReD2666124531022zs5rky64719891:20000
Riney loam, karst, 6 to 12 percent slopes, erodedRnC2547024530982nbn6ky64719891:20000
Riney loam, 6 to 12 percent slopes, erodedReC2464424531012zs5qky64719891:20000
Riney loam, karst, 20 to 30 percent slopesRnE350624531002nbn8ky64719891:20000
Riney loam, karst, 2 to 6 percent slopesRnB45024530972nbn5ky64719891:20000
Riney silt loam, 12 to 20 percent slopes, erodedReD294423792142kvrvky64820091:12000
Riney silt loam, 6 to 12 percent slopes, erodedReC263323792132kvrtky64820091:12000
Riney silt loam, 20 to 30 percent slopesReE8623792152kvrwky64820091:12000
Riney loam, karst, 2 to 6 percent slopesRnB3623794132kvz8ky64820091:12000
Riney silt loam, 2 to 6 percent slopes, erodedReB22723792122kvrsky64820091:12000
Riney loam, 6 to 12 percent slopes, erodedReC2297024528962zs5qky70919951:20000
Riney loam, 12 to 20 percent slopes, erodedReD2190024528972zs5rky70919951:20000
Riney loam, 2 to 6 percent slopesReB39624528952zs5pky70919951:20000

Map of Series Extent

Approximate geographic distribution of the RINEY 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 .