Official Series Description


Lab Data Summary

Aggregate lab data for the ELKINSVILLE soil series. This aggregation is based on all pedons with a current taxon name of ELKINSVILLE, 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 ELKINSVILLE 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
114A93P0186S1991IN119045Elkinsville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4652786,-86.734726
114A93P0238S1992IN119022Elkinsville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.4361115,-86.7513885
114BJE70061970IN079006Elkinsville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8684056,-85.6188444
114BDC78151978IN031015Elkinsville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3201861,-85.2984306
114BJF79162016IN077001Elkinsville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7610694,-85.6287
115AKX77041977IN083004Elkinsville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5337111,-87.5028222
115APK79051979IN125005Elkinsville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5409,-87.2763278
115AGB82171982IN051017Elkinsville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4304806,-87.6782
120B93P0760S1993IN123015Elkinsville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9972229,-86.5294418
120CMR76121976IN109012Elkinsville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.3516111,-86.4682306
121SW81131981IN155013Elkinsville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7354278,-85.0934056
121RI80012017IN137001Elkinsville2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.997059,-85.179678
122WS80162016IN175004Elkinsville3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.4277278,-86.1798861

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ELKINSVILLE 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 ELKINSVILLE 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 ELKINSVILLE 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 ELKINSVILLE 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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Click the image to view it full size.

Competing Series

Soil series competing with ELKINSVILLE 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 ELKINSVILLE 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 ELKINSVILLE 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 ELKINSVILLE, 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. IN-2010-09-24-20 | Perry County -

    Typical pattern of soils and parent materials of alluvial, stream terrace lacustrine and aeolian landforms adjacent to hills underlain with interbedded shale and limestone in Ohio River Valley (Soil Survey of Perry County, Indiana).

  2. IN-2012-01-19-30 | Jefferson County - May 1985

    Pattern of soils and parent material in the Huntington-Dearborn-Elkinsville map unit (Soil Survey of Jefferson County, Indiana; 1985).

  3. IN-2012-01-19-40 | Perry County - September 1969

    Relationship of relief and geologic strata to certain of the soil series represented in Perry County. The vertical scale is greatly exaggerated (Soil Survey of Perry County, Indiana; 1969).

  4. OH-2012-02-16-15 | Belmont County - July 1981

    Typical pattern of soils in the Elkinsville-Nolin Variant-Brookside association (Soil Survey of Belmont County, Ohio; July 1981).

Map Units

Map units containing ELKINSVILLE 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
Elkinsville silt loam, 0 to 2 percent slopes, rarely floodedEepAQ832072686yp2in00520021:12000
Elkinsville-Millstone silt loams, 2 to 6 percent slopesEesB13432010966r7zin01920011:12000
Elkinsville-Millstone silt loams, 0 to 2 percent slopesEesA10262010956r7yin01920011:12000
Elkinsville-Millstone silt loams, 6 to 12 percent slopes, erodedEesC22692010996r82in01920011:12000
Elkinsville-Millstone silt loams, 18 to 40 percent slopes, rarely floodedEesFQ2092011046r87in01920011:12000
Elkinsville-Millstone silt loams, 12 to 18 percent slopes, erodedEesD21722011016r84in01920011:12000
Elkinsville silt loam, 2 to 6 percent slopesEepB72516525742wh48in02519701:20000
Elkinsville silt loam, 6 to 12 percent slopes, erodedEepC232016525752wh43in02519701:20000
Millstone-Elkinsville complex, 6 to 12 percent slopes, erodedMsbC21316525541sgm6in02519701:20000
Elkinsville silt loam, 6 to 12 percent slopes, erodedEkC222116006571qqm3in02919791:15840
Elkinsville silt loam, 0 to 2 percent slopes, rarely floodedEkA21816006552wlthin02919791:15840
Elkinsville silt loam, 2 to 6 percent slopes, erodedEkB221316006561qqm2in02919791:15840
Elkinsville silt loam, 2 to 6 percent slopesEepB2321851632wh48in04320001:12000
Elkinsville silt loam, 25 to 60 percent slopes, rarely floodedEepGQ8418516766p4in04320001:12000
Elkinsville silt loam, 0 to 2 percent slopesEkA19341601165cm1in05119861:15840
Elkinsville silt loam, 2 to 6 percent slopesEkB3461601175cm2in05119861:15840
Elkinsville silt loam, 2 to 6 percent slopes, erodedEepB21086798171vskgin06120071:12000
Elkinsville-Millstone complex, 18 to 40 percent slopes, rarely floodedEesFQ68116775251t9lqin06120071:12000
Elkinsville-Millstone complex, 2 to 6 percent slopesEesB48016775201t9lkin06120071:12000
Elkinsville silt loam, 6 to 12 percent slopes, erodedEepC247116764882wh43in06120071:12000
Elkinsville-Millstone complex, 6 to 12 percent slopes, erodedEesC245516775211t9llin06120071:12000
Urban land-Elkinsville-Haymond complex, 0 to 6 percent slopes, rarely floodedUekAQ35616866161tm1zin06120071:12000
Elkinsville silt loam, 0 to 2 percent slopesEepA27916764872wltjin06120071:12000
Elkinsville-Millstone complex, 0 to 2 percent slopesEesA21416775191t9ljin06120071:12000
Elkinsville silt loam, 25 to 60 percent slopes, rarely floodedEepGQ1210871028s8xin06120071:12000
Elkinsville silt loam, 2 to 8 percent slopes, rarely floodedEkB187396464911csqin07719821:15840
Elkinsville silt loam, 0 to 2 percent slopes, rarely floodedEkA7489646482wlthin07719821:15840
Elkinsville-Millstone complex, 2 to 6 percent slopes, erodedEesB299016513871sfdkin07920101:12000
Elkinsville silt loam, 0 to 2 percent slopes, rarely floodedEepAQ5024279342mhggin07920101:12000
Elkinsville silt loam, 0 to 2 percent slopesEkA31221644745j4min08319791:15840
Elkinsville variant loam, 2 to 6 percent slopes, erodedEhrB282916515361sfkcin09319821:15840
Elkinsville silt loam, 2 to 6 percent slopesEepB57317081292wh48in10119841:15840
Elkinsville silt loam, upland, 20 to 40 percent slopesEkF2984535535kz8bin10519791:15840
Elkinsville silt loam, 2 to 6 percent slopesEkB7445355342wh48in10519791:15840
Elkinsville silt loam, 6 to 12 percent slopes, erodedEsC24631632075gtrin10919791:15840
Elkinsville silt loam, 6 to 12 percent slopes, erodedEkC215416005491qqhmin11519791:15840
Elkinsville silt loam, 0 to 2 percent slopes, rarely floodedEkA10116005472wlthin11519791:15840
Elkinsville silt loam, 2 to 6 percent slopes, erodedEkB28916005481qqhlin11519791:15840
Elkinsville silt loam, 2 to 6 percent slopesEepB174614429812wh48in11719801:15840
Elkinsville silt loam, 6 to 12 percent slopes, erodedEepC268414429822wh43in11719801:15840
Elkinsville silt loam, 0 to 2 percent slopesEepA44414429792wltjin11719801:15840
Urban land-Elkinsville-Hatfield complex, 0 to 6 percent slopesUehB785535923kznvin12319971:12000
Millstone-Elkinsville complex, 2 to 6 percent slopesMsbB487535835kzl0in12319971:12000
Millstone-Elkinsville complex, 2 to 6 percent slopes, rarely floodedMsbBQ418535991kzr1in12319971:12000
Elkinsville-Millstone complex, 18 to 40 percent slopes, rarely floodedEesFQ290535742kzh0in12319971:12000
Millstone-Elkinsville complex, 6 to 12 percent slopes, eroded, rarely floodedMsbCQ288535990kzr0in12319971:12000
Elkinsville-Millstone complex, 0 to 2 percent slopesEesA244535740kzgyin12319971:12000
Millstone-Elkinsville complex, 6 to 12 percent slopes, erodedMsbC2206535836kzl1in12319971:12000
Elkinsville-Millstone complex, 0 to 2 percent slopes, rarely floodedEesAQ177535994kzr4in12319971:12000
Elkinsville-Millstone complex, 12 to 18 percent slopes, eroded, rarely floodedEesDQ164535993kzr3in12319971:12000
Elkinsville-Millstone complex, 12 to 18 percent slopes, erodedEesD258535741kzgzin12319971:12000
Elkinsville silt loam, 0 to 2 percent slopesEkA5721619015fgmin12519831:15840
Elkinsville silt loam, 0 to 2 percent slopes, rarely floodedEkA69071598825cchin12919781:15840
Elkinsville silt loam, 2 to 6 percent slopes, eroded, rarely floodedEkB218761598835ccjin12919781:15840
Elkinsville silt loam, 2 to 6 percent slopesElB2671598275c9qin13319791:15840
Elkinsville silt loam, 2 to 6 percent slopesEkB100214796312wh4bin13719821:15840
Elkinsville silt loam, 6 to 12 percent slopes, erodedEkC248514796321lnp2in13719821:15840
Elkinsville silt loam, 18 to 35 percent slopesEepF1941656615kcxin14319951:12000
Elkinsville silt loam, 2 to 6 percent slopesEepB831656602wh48in14319951:12000
Elkinsville silt loam, 0 to 2 percent slopesEepA351656595kcvin14319951:12000
Elkinsville silt loam, rarely flooded, 0 to 2 percent slopesEkA786535277kz00in15519841:15840
Elkinsville silt loam, rarely flooded, 2 to 8 percent slopesEkB438535278kz01in15519841:15840
Elkinsville silt loam, 2 to 6 percent slopesElB4845354802wh48in17519841:15840
Elkinsville silt loam, 6 to 12 percent slopes, erodedElC22445354812wh43in17519841:15840
Elkinsville silt loam, 1 to 6 percent slopesEkB46421700835pzkoh00119871:15840
Elkinsville silt loam, 2 to 6 percent slopesEnB86189587721mtboh00119871:15840
Elkinsville silt loam, 8 to 15 percent slopesElC8335370852zj1hoh01319781:15840
Elkinsville silt loam, 3 to 8 percent slopesElB5265370842zj1goh01319781:15840
Elkinsville silt loam, 15 to 25 percent slopesElD4715370862zj1coh01319781:15840
Elkinsville silt loam, 2 to 6 percent slopesEkB18021697185plsoh01519871:15840
Elkinsville silt loam, 6 to 12 percent slopes, erodedEkC24331697195pltoh01519871:15840
Elkinsville silt loam, 0 to 3 percent slopes, rarely floodedEk4195379802zj1moh01919811:15840
Elkinsville silt loam, 2 to 6 percent slopesEkB2124403412mxcpoh02519721:20000
Elkinsville silt loam, 1 to 6 percent slopesEkB21295368022zj19oh05319881:15840
Urban land-Alfic Udarents-Elkinsville complex, 0 to 12 percent slopesUAKXC73926528792pyz8oh06119801:15840
Elkinsville silt loam, 2 to 6 percent slopesEvB7926528452wh4boh06119801:15840
Elkinsville silt loam, 6 to 12 percent slopesEvC6826528462q6yvoh06119801:15840
Elkinsville silt loam, 1 to 6 percent slopesEkB1414206631jp9voh07119731:15840
Elkinsville-Urban land complex, 1 to 8 percent slopesEmB3701536144kzwzoh08719891:15840
Elkinsville silt loam, 1 to 6 percent slopesEkB31825361422zj19oh08719891:15840
Elkinsville silt loam, 15 to 40 percent slopesEkE3645361432zj1doh08719891:15840
Elkinsville silt loam, 0 to 2 percent slopesEkA2615371542zj16oh10519911:15840
Elkinsville silt loam, 0 to 2 percent slopes, rarely floodedEn21825376252zj1noh13119841:15840
Elkinsville silt loam, 1 to 8 percent slopesEkB27685372412zj1boh14519841:15840
Elkinsville silt loam, 25 to 40 percent slopesEkE16795372422zj1foh14519841:15840
Elkinsville-Urban land complex, 1 to 8 percent slopesEmB1541537243l11foh14519841:15840
Elkinsville silt loam, 1 to 6 percent slopesEhB1214608082zj19oh14519841:15840
Elkinsville silt loam, 0 to 3 percent slopesEkA6005363032zj18oh15719811:15840

Map of Series Extent

Approximate geographic distribution of the ELKINSVILLE 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 .