Official Series Description


Lab Data Summary

Aggregate lab data for the FAIRMOUNT soil series. This aggregation is based on all pedons with a current taxon name of FAIRMOUNT, 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 FAIRMOUNT 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
120A95P019693IL069014EFairmount6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4755891,-88.3238498
120A95P019793IL069025EFairmount6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4789571,-88.326982
12840A4967S1958TN105007Fairmount4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6937103,-84.2299118
12840A4968S1958TN105008Fairmount4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.685833,-84.206665
n/aAD-s181961-OH001-S18Fairmount3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCL-0061966-OH025-006Fairmount3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a93KY-239-00693KY-239-006Fairmount2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the FAIRMOUNT 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 FAIRMOUNT 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 FAIRMOUNT 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 FAIRMOUNT 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 FAIRMOUNT 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 FAIRMOUNT series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the FAIRMOUNT 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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 FAIRMOUNT, 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-2012-01-26-11 | Anderson and Franklin Counties - May 1985

    Relationship of soils to topography and underlying material in the Fairmount-Rock outcrop-McAfee unit (Soil Survey of Anderson and Franklin Counties, Kentucky; May 1985).

  2. KY-2012-01-26-12 | Anderson and Franklin Counties - May 1985

    Relationship of soils to topography and underlying material in the Elk-McAfee-Otwell unit (Soil Survey of Anderson and Franklin Counties, Kentucky; May 1985).

  3. KY-2012-01-26-13 | Anderson and Franklin Counties - May 1985

    Relationship of soils to topography and underlying material in the Ashton-Huntington-Elk unit (Soil Survey of Anderson and Franklin Counties, Kentucky; May 1985).

  4. KY-2012-01-26-14 | Anderson and Franklin Counties - May 1985

    Relationship of soils to topography and underlying material in the McAfee-Faywood-Fairmount unit (Soil Survey of Anderson and Franklin Counties, Kentucky; May 1985).

  5. KY-2012-01-26-21 | Bath County - September 1963

    Typical landscape showing the topography and relative position of the principal soils in association 7 (Soil Survey of Bath County, Kentucky; September 1963).

  6. KY-2012-01-26-25 | Bath County - September 1963

    Cross section of Bath County showing the major soils and their relationship to the rock formations and to relief (Soil Survey of Bath County, Kentucky; September 1963).

  7. KY-2012-01-26-30 | Boyle and Mercer Counties - April 1983

    Typical pattern of soils and underlying material in the Lowell-Faywood-Eden map unit (Soil Survey of Boyle and Mercer Counties, Kentucky; April 1983).

  8. KY-2012-01-26-33 | Boyle and Mercer Counties - April 1983

    Typical pattern of soils and underlying material in the McAfee-Caleast-Fairmount map unit (Soil Survey of Boyle and Mercer Counties, Kentucky; April 1983).

  9. KY-2012-01-27-28 | Casey County - August 1994

    Typical pattern of soils and underlying materials in the Faywood-Lowell-Fairmount general soil map unit (Soil Survey of Casey County, Kentucky; August 1994).

  10. KY-2012-01-27-29 | Casey County - August 1994

    Typical pattern of soils and underlying materials in the Colyer-Faywood-Nolin general soil map unit (Soil Survey of Casey County, Kentucky; August 1994).

  11. KY-2012-01-27-38 | Clark County - 1964

    Major soil series in soil association 5, their relationship to the landscape, and the parent rocks from which the soils formed (Soil Survey of Clark County, Kentucky; 1964).

  12. KY-2012-01-27-59 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Fairmount-Shrouts-Allegheny association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

  13. KY-2012-01-27-69 | Fayette County - February 1968

    Relationship of soils to topography and underlying material in association 4. Unshaded areas represent caverns or sinkholes in the limestone bedrock (Soil Survey of Fayette County, Kentucky; February 1968).

  14. KY-2012-01-31-06 | Henry and Trimble Counties - April 1992

    Pattern of soils and parent material in the Faywood-Lowell-Fairmount general soil map unit in Henry County (Soil Survey of Henry and Trimble Counties, Kentucky; April 1992).

  15. KY-2012-01-31-10 | Henry and Trimble Counties - April 1992

    Pattern of soils and parent material in the Fairmount-Woolper-Brassfield general soil map unit in Trimble County (Soil Survey of Henry and Trimble Counties, Kentucky; April 1992).

  16. KY-2012-01-31-20 | Jefferson County - June 1966

    Diagram showing general parent material, position, and pattern of soils in the Beasley-Fairmount-Russellville association (Soil Survey of Jefferson County, Kentucky; June 1966).

  17. KY-2012-01-31-21 | Jessamine and Woodford Counties - December 1983

    Pattern of soils and underlying material in Maury-McAfee unit (Soil Survey of Jessamine and Woodford Counties, Kentucky; December 1983).

  18. KY-2012-01-31-22 | Jessamine and Woodford Counties - December 1983

    Pattern of soils and underlying material in McAfee-Maury-Fairmount unit (Soil Survey of Jessamine and Woodford Counties, Kentucky; December 1983).

  19. KY-2012-01-31-23 | Jessamine and Woodford Counties - December 1983

    Pattern of soils and underlying material in Fairmount-Rock outcrop unit (Soil Survey of Jessamine and Woodford Counties, Kentucky; December 1983).

  20. KY-2012-02-01-15 | Mason County - September 1986

    Typical pattern of soils and parent material in the Cynthiana-Faywood-Lowell general soil map unit (Soil Survey of Mason County, Kentucky; September 1986).

  21. KY-2012-02-01-63 | Washington County - August 1986

    Typical pattern of soils and underlying material in the Fairmount-Shrouts-Faywood map unit (Soil Survey of Washington County, Kentucky; August 1986).

  22. KY-2012-02-01-64 | Washington County - August 1986

    Typical pattern of soils and underlying material in the Lowell-Faywood-Shelbyville map unit (Soil Survey of Washington County, Kentucky; August 1986).

Map Units

Map units containing FAIRMOUNT 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
Fairmount silty clay loam, 35 to 50 percent slopesFaG55916128351r48yin04119581:15840
Fairmount silty clay loam, 25 to 35 percent slopesFaF15116128341r48xin04119581:15840
Fairmount silty clay loam, 18 to 25 percent slopesFaE2116128331r48win04119581:15840
Fairmount silty clay loam, 12 to 18 percent slopesFaD1216128321r48vin04119581:15840
Fairmount silty clay loam, 6 to 12 percent slopesFaC316128311r48tin04119581:15840
Fairmount silty clay loam, 2 to 6 percent slopesFaB316128301r48sin04119581:15840
Fairmount silty clay loam, 25 to 35 percent slopesFaF52616129831r4fqin16119581:15840
Fairmount silty clay loam, 35 to 50 percent slopesFaG48316129841r4frin16119581:15840
Fairmount silty clay loam, 18 to 25 percent slopesFaE21016129821r4fpin16119581:15840
Fairmount silty clay loam, 6 to 12 percent slopesFaC7716129801r4fmin16119581:15840
Fairmount silty clay loam, 12 to 18 percent slopesFaD7316129811r4fnin16119581:15840
Fairmount silty clay loam, 2 to 6 percent slopesFaB416129791r4flin16119581:15840
Fairmount-Faywood complex, 20 to 60 percent slopes, erodedFaF2274417274931vzllky01120061:12000
Faywood-Fairmount-Rock outcrop complex, 20 to 30 percent slopes, erodedFfE210900548889lf53ky04519891:20000
Fairmount silty clay loam, very rocky, 30 to 60 percent slopesFaF730548887lf51ky04519891:20000
Fairmount flaggy clay, 30 to 50 percent slopes, severely erodedFaF31697550143lggkky04919621:15840
Ashwood very rocky clay, 20 to 30 percent slopes, severely eroded (fairmount)AvE31152550104lgf9ky04919621:15840
Ashwood very rocky silty clay loam, 12 to 20 percent slopes (fairmount)AwD706550106lgfcky04919621:15840
Ashwood very rocky silty clay loam, 20 to 30 percent slopes (fairmount)AwE679550107lgfdky04919621:15840
Ashwood very rocky clay, 6 to 12 percent slopes, severely eroded (fairmount)AvC3633550102lgf7ky04919621:15840
Fairmount flaggy silty clay loam, 20 to 30 percent slopesFfE625550144lgglky04919621:15840
Ashwood very rocky clay, 12 to 20 percent slopes, severely eroded (fairmount)AvD3612550103lgf8ky04919621:15840
Ashwood very rocky silty clay loam, 6 to 12 percent slopes (fairmount)AwC367550105lgfbky04919621:15840
Fairmount flaggy clay, 20 to 30 percent slopes, severely erodedFaE3318550142lggjky04919621:15840
Fairmount-Woolper complex, very rocky, 20 to 60 percent slopesFaF4154552710lk4cky06919891:20000
Fairmount and Cynthiana extremely rocky soils, 20 to 30 percent slopesFcE1233551798lj5yky09719651:15840
Fairmount and Cynthiana extremely rocky soils, 30 to 50 percent slopesFcF1216551799lj5zky09719651:15840
Fairmount-Faywood complex, 20 to 55 percent slopes, very rocky, erodedFaF27211550296lgmhky13519981:20000
Fairmount-Rock outcrop complex, 30 to 60 percent slopesFaF897313978732vp3cky15119681:20000
Fairmount-Rock outcrop complex, 30 to 60 percent slopesFrF65105489292vp3cky16119831:20000
Fairmount flaggy clay, 20 to 50 percent slopes, severely erodedFmF36065549959lg8mky17919671:15840
Fairmount flaggy clay, 6 to 20 percent slopes, severely erodedFmD34620549958lg8lky17919671:15840
Fairmount flaggy silty clay loam, 12 to 30 percent slopesFfE1990549957lg8kky17919671:15840
Fairmount silty clay loam, 6 to 20 percent slopesFaD415549956lg8jky17919671:15840
Woolper-Fairmount complex, 30 to 65 percent slopesWpF1070551672lj1wky21119781:20000
Fairmount-Rock outcrop complex, 20 to 50 percent slopesFaF8570551495lhw5ky22919831:20000
Fairmount-Rock outcrop complex, 6 to 20 percent slopesFaD7605551494lhw4ky22919831:20000
Fairmount-Rock outcrop complex, 30 to 60 percent slopesFcF96315516222vp3cky60119821:20000
Fairmount-Rock outcrop complex, 12 to 30 percent slopesFcE8053551621lj07ky60119821:20000
Fairmount flaggy silty clay, 6 to 12 percent slopesFaC1280551620lj06ky60119821:20000
Fairmount-Rock outcrop complex, 30 to 60 percent slopesFrF18545520852vp3cky60419781:20000
Fairmount-Rock outcrop complex, 12 to 30 percent slopesFrD1460552084ljh5ky60419781:20000
Fairmount-Rock outcrop complex, 12 to 30 percent slopesFaD10054551538lhxkky60619791:20000
Fairmount-Rock outcrop complex, 30 to 60 percent slopesFaF73955515392vp3cky60619791:20000
Fairmount-Rock outcrop complex, 6 to 12 percent slopesFaC5954551537lhxjky60619791:20000
Faywood-Fairmount-Woolper complex, 30 to 60 percent slopesFnF10359550990lhbwky60819831:20000
Fairmount-Rock outcrop complex, 30 to 60 percent slopesFrF402505519912vp3cky61219721:15840
Fairmount flaggy silty clay, 12 to 20 percent slopesFaD5049551990ljd4ky61219721:15840
Faywood-Fairmount complex, phosphatic, 12 to 25 percent slopes, eroded, very rockyFfD24981552950lkd3ky61819931:12000
Faywood-Fairmount complex, phosphatic, 6 to 12 percent slopes, eroded, rockyFfC22972552949lkd2ky61819931:12000
Rock outcrop-Fairmount complex, 50 to 120 percent slopesRoF2149552989lkfcky61819931:12000
Fairmount-Faywood-Rock outcrop complex, 25 to 50 percent slopes, erodedFdF21428552946lkczky61819931:12000
Fairmount silty clay loam, 6 to 12 percent slopes, eroded, very rockyFaC2157552944lkcxky61819931:12000
Fairmount-Woolper complex, 30 to 65 percent slopesFwF27978551918lj9tky62219891:20000
Fairmount flaggy silty clay loam, 12 to 30 percent slopes, very rockyFaE15443551917lj9sky62219891:20000
Fairmount-Rock outcrop complex, 12 to 30 percent slopesFcE9968551880lj8lky62419761:20000
Fairmount-Rock outcrop complex, 30 to 60 percent slopesFcF95435518812vp3cky62419761:20000
Fairmount flaggy silty clay, 6 to 12 percent slopesFaC8573551879lj8kky62419761:20000
Fairmount flaggy silty clay loam, very rocky, 20 to 60 percent slopesFrF863551837lj76ky63719891:12000
Fairmount very rocky silty clay loam, 6 to 30 percent slopes, severely eroded (fairmount-Rock outcrop complex)FaD3224813988551hymcky64319651:15840
Rock land (rock outcrop-fairmount complex, 20 to 50 percent slopes)Rk146313988981hynrky64319651:15840
Fairmount very rocky silty clay loam, 6 to 20 percent slopes (fairmount-Rock outcrop complex)FaD142913988541hymbky64319651:15840
Fairmount very rocky silty clay loam, 20 to 50 percent slopes (fairmount-Rock outcrop complex)FaF100513988561hymdky64319651:15840
Fairmount very flaggy silty clay loam, 25 to 50 percent slopes, moderately erodedFaG215041687865nmqoh02519721:20000
Edenton and Fairmount soils, 25 to 50 percent slopes, severely erodedEdG38361687835nmmoh02519721:20000
Fairmount very flaggy silty clay loam, 18 to 25 percent slopes, moderately erodedFaE271687855nmpoh02519721:20000
Hickory-Fairmount complex, 25 to 50 percent slopes, moderately erodedHtF277771713635r9voh16519671:20000
Hickory-Fairmount complex, 18 to 25 percent slopes, moderately erodedHtE217611713625r9toh16519671:20000

Map of Series Extent

Approximate geographic distribution of the FAIRMOUNT 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 .