Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
12886P093986TN163016Keener6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.4883347,-82.0622253
130B87P014186TN163030Keener6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5294456,-81.996109
130B87P025287TN091001Keener7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.4658318,-81.9294434
130B88P095888NC199010Keener6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.0488892,-82.4269409

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the KEENER series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

There are insufficient data to create the sibling sketch figure.

Select annual climate data summaries for the KEENER series and siblings. 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 KEENER 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

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

There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with KEENER share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the KEENER 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 KEENER 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 .

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with KEENER, 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. TN-2010-11-02-19 | McMinn County - 2004

    Relationship of soils and parent material in the Tellico-Red Hills-Nonaburg and Lostcove-Unicoi-Cataska general soil map units (Soil Survey of McMinn County, Tennessee; 2004).

  2. TN-2012-03-19-26 | McMinn County - 2004

    Relationship of soils and parent material in the Tellico-Red Hills-Nonaburg and Lostcove-Unicoi-Cataska general soil map units (Soil Survey of McMinn County, TN; 2004).

Map Units

Map units containing KEENER 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
Keener loam, 8 to 15 percent slopes, stonyKnC116714021t376nc11520061:12000
Keener-Lostcove complex, 15 to 30 percent slopes, very stonyKcD626547576lcsrnc12119971:12000
Keener loam, 8 to 15 percent slopes, stonyKnC246561810lvlxnc18920011:12000
Keener loam, 15 to 30 percent slopes, stonyKnD165561818lvm5nc18920011:12000
Keener-Lostcove complex, 30 to 50 percent slopes, very boulderyKcE902547851ld2mnc19919971:12000
Keener-Lostcove complex, 15 to 30 percent slopes, very boulderyKcD783547850ld2lnc19919971:12000
Keener loam, 35 to 50 percent slopesKeF5401526464kntqtn01920001:24000
Keener loam, 20 to 35 percent slopesKeE5221526463kntptn01920001:24000
Keener loam, 5 to 12 percent slopesKeC2481526461kntmtn01920001:24000
Keener loam, 12 to 20 percent slopesKeD2457526462kntntn01920001:24000
Keener loam, 5 to 12 percent slopes22C820923959302lf52tn05919541:15840
Keener loam, 5 to 12 percent slopes, stony21C397623959262lf4ytn05919541:15840
Keener loam, 12 to 20 percent slopes22D191923959312lf53tn05919541:15840
Keener loam, 12 to 20 percent slopes, stony21D152223959272lf4ztn05919541:15840
Keener loam, 20 to 35 percent slopes, stony21E93823959282lf50tn05919541:15840
Keener loam, 20 to 35 percent slopes22E81223959322lf54tn05919541:15840
Keener loam, 35 to 50 percent slopes, stony21F13523959292lf51tn05919541:15840
Keener loam, 35 to 50 percent slopes22F8223959342lf56tn05919541:15840
Keener loam, 20 to 35 percent slopesKeE9494526543knx8tn09120001:24000
Keener loam, 35 to 50 percent slopesKeF9212526544knx9tn09120001:24000
Keener loam, 12 to 20 percent slopesKeD5180526542knx7tn09120001:24000
Keener loam, 5 to 12 percent slopesKeC2987526541knx6tn09120001:24000
Keener-Lostcove complex, 35 to 50 percent slopes, very stonyKeF948526195knk1tn10719991:24000
Keener-Lostcove complex, 3 to 12 percent slopes, very stonyKeC186526196knk2tn10719991:24000
Lostcove-Keener complex, 25 to 65 percent slopes, very stonyLkF5491523770kl0ttn13919971:24000
Lostcove-Keener complex, 12 to 25 percent slopes, very stonyLkD4252523769kl0stn13919971:24000
Keener loam, 12 to 25 percent slopesKeD2962523766kl0ptn13919971:24000
Keener loam, 3 to 12 percent slopesKeC2336523765kl0ntn13919971:24000
Lostcove-Keener complex, 3 to 12 percent slopes, stonyLkC2061523768kl0rtn13919971:24000
Keener gravelly fine sandy loam, 12 to 20 percent slopes, cobblyKeD4178530076ksl7tn16319911:20000
Keener gravelly fine sandy loam, 5 to 12 percent slopes, cobblyKeC3971530075ksl6tn16319911:20000
Keener gravelly fine sandy loam, 20 to 35 percent slopes, cobblyKeE1587530077ksl8tn16319911:20000
Keener loam, 20 to 35 percent slopes21E152924013282lls6tn17119801:24000
Keener loam, 12 to 20 percent slopes, stony21D124024013272lls5tn17119801:24000
Keener loam, 35 to 50 percent slopes21F86224013292lls7tn17119801:24000
Keener loam, 5 to 12 percent slopes, stony21C16124013262lls4tn17119801:24000
Keener loam, 5 to 12 percent slopesKeC174516896671tq7dtn17919551:15840
Keener loam, 20 to 35 percent slopes, stonyKsE161516896691tq7gtn17919551:15840
Keener loam, 12 to 20 percent slopes, stonyKsD109516896701tq7htn17919551:15840
Keener loam, 5 to 12 percent slopes, stonyKsC105516896711tq7jtn17919551:15840
Keener loam, 35 to 50 percent slopes, stonyKsF80616896681tq7ftn17919551:15840
Keener loam, 12 to 20 percent slopesKeD40316896661tq7ctn17919551:15840
Keener loam, 20 to 35 percent slopesKeE29716896651tq7btn17919551:15840
Keener loam, 12 to 20 percent slopes, stonyKfD8732524804km35tn60620011:24000
Keener loam, 5 to 12 percent slopes, stonyKfC6656524803km34tn60620011:24000
Keener loam, 20 to 35 percent slopes, stonyKfE3917524805km36tn60620011:24000
Keener loam, 15 to 35 percent slopes, very stony35D118316705521t2bsva07720061:24000
Keener loam, 15 to 25 percent slopes34D32116705201t29rva07720061:24000
Keener loam, 7 to 15 percent slopes, very stony35C170516775kbr5va07720061:24000
Keener loam, 7 to 15 percent slopes34C141516731kbprva07720061:24000
Keener loam, 2 to 7 percent slopes34B105516730kbpqva07720061:24000
Keener loam, 15 to 35 percent slopes, very stony826D287925252842qm2mva6061:24000
Keener loam, 3 to 15 percent slopes, very stony826C83125252832qm2lva6061:24000
Keener loam, 35 to 60 percent slopes, very stony826E40325252852qm2nva6061:24000

Map of Series Extent

Approximate geographic distribution of the KEENER 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 .