Official Series Description


Lab Data Summary

Aggregate lab data for the DICKSON soil series. This aggregation is based on all pedons with a current taxon name of DICKSON, 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 DICKSON 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
12283P06901982KY003005Dickson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.7254295,-86.396225
12287P07061987KY045001Dickson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.187603,-84.969223
12298P03621998TN015001Dickson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7186127,-86.0025024
12299P02891998TN015002Dickson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7186127,-86.0025024
122S70AL-077-270AL077002-pgmDickson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.9891738891602,-87.4077835083008
122S70AL-077-770AL077007-pgmDickson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.9219512939453,-87.2447280883789
12202N0197S2001AL051001Dickson4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.8486176,-86.8849335
12205N0283S2003AL089004Dickson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.9372139,-86.7128601
12802N0183S2002AL089001Dickson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.9016495,-86.5384827
133AS70AL-077-170AL077001-pgmDickson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties34.9819526672363,-87.7980575561523
n/a40A49571954TN031004Dickson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A49581954TN031010Dickson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P02561997TN127001Dickson5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P03711998TN147002Dickson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a98P03721998TN161001Dickson7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a54KY-227-00254KY-227-002Dickson4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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 DICKSON 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 DICKSON 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 DICKSON 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 DICKSON, 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-2012-01-26-01 | Adair County - April 1964

    Diagram of the Westmoreland-Caneyville-Baxter association in Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  2. KY-2012-01-26-02 | Adair County - April 1964

    Diagram of the Baxter-Christian-Bewleyville association (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  3. KY-2012-01-26-03 | Adair County - April 1964

    Pattern of soils in the Frankstown-Bodine-Westmoreland association (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  4. KY-2012-01-26-06 | Adair County - April 1964

    Geological cross section of Adair County showing the relationship of the soils to the underlying rocks (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  5. KY-2012-01-27-11 | Caldwell County - September 1966

    Typical pattern of soils and underlying materials in association 5 (Soil Survey of Caldwell County, Kentucky; September 1966).

  6. KY-2012-01-30-08 | Green and Taylor Counties - July 1982

    Pattern of soils and underlying material in the Frederick-Frankstown-Mountview general soil map unit (Soil Survey of Green and Taylor Counties, Kentucky; July 1982).

  7. KY-2012-01-30-09 | Green and Taylor Counties - July 1982

    Pattern of soils and underlying material in the Frederick-Mountview-Frankstown general soil map unit (Soil Survey of Green and Taylor Counties, Kentucky; July 1982).

  8. KY-2012-01-31-18 | Jefferson County - June 1966

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

  9. KY-2012-02-01-67 | Wayne County - March 1990

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

  10. OK-2012-02-16-01 | Adair County - September 1965

    Soils in the Bodine-Dickson soil association and their general location in the landscape (Soil Survey of Adair County, Oklahoma; September 1965).

  11. TN-2010-11-02-01 | Cannon County - 2003

    Typical pattern of soils and parent material in the Dickson-Mountview general soil map unit (Soil Survey of Cannon County, Tennessee; 2003).

  12. TN-2010-11-02-09 | Hickman County - 2008

    Typical pattern of soils and parent material in the Sengtown-Mountview-Dickson and Sengtown general soil map units (Soil Survey of Hickman County, Tennessee; 2008).

  13. TN-2010-11-02-17 | Lewis County - 2006

    Typical pattern of soils and parent material in the Dickson-Ironcity-Taft general soil map unit (Soil Survey of Lewis County, Tennessee; 2006).

  14. TN-2010-11-02-23 | Moore County - 2006

    Typical pattern of soils and parent material in the Mountview-Dickson-Taft general soil map unit (Soil Survey of Moore County, Tennessee; 2006).

  15. TN-2010-11-02-28 | Overton County - 2005

    The relationship of soils and landscapes in the Mountview-Chirstian-Dickson general soil map unit (Soil Survey of Overton County, Tennessee; 2005).

  16. TN-2012-03-16-01 | Cheatham County - 2002

    Relationship of soils to topography and the underlying material in the Sengtown-Mountview-Dickson general soil map unit (Soil Survey of Cheatham County, TN; 2002).

  17. TN-2012-03-19-18 | Maury County - October 1959

    Sketch showing relative positions of soils in the Mountview-Dickson and the Bodine-Mountview (shallow phases)-Pace assciations (Soil Survey of Maury County, TN; 1959).

  18. TN-2012-03-19-30 | Warren County - September 1967

    Major and minor soils and underlying parent material in the Dickson-Mountview association (Soil Survey of Warren County, TN; 1967).

  19. TN-2012-03-19-31 | Warren County - September 1967

    Major and minor soils and underlying parent materials in the Baxter-Mountview association (Soil Survey of Warren County, TN; 1967).

Map Units

Map units containing DICKSON 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
Dickson silt loam, 0 to 2 percent slopesDkA17153286942t8fral03319861:20000
Dickson silt loam, 2 to 5 percent slopesDoB791825230442sr6kal07719731:20000
Dickson silt loam, 6 to 10 percent slopesDoC16160523045kk8fal07719731:20000
Dickson silt loam, 0 to 2 percent slopesDoA79645230432t8fral07719731:20000
Dickson silt loam, 2 to 5 percent slopes, erodedDle227165227532s8mcal08319531:20000
Dickson silt loam, 0 to 2 percent slopesDlv178405227562t8fral08319531:20000
Dickson silt loam, 2 to 5 percent slopesDlu128535227552sr6kal08319531:20000
Dickson cherty silt loam eroded rolling phaseDcn3414522747kjytal08319531:20000
Dickson cherty silt loam eroded undulating phaseDce2445522746kjysal08319531:20000
Dickson cherty silt loam undulating phaseDcu1139522748kjyval08319531:20000
Dickson silt loam eroded rolling phaseDln1033522754kjz1al08319531:20000
Dickson cherty silt loam rolling phaseDco841522745kjyral08319531:20000
Dickson cherty silty clay loam severely eroded rolling phaseDkd248522752kjyzal08319531:20000
Dickson silt loam, 2 to 5 percent slopesDt115505231172sr6kal08919581:24000
Dickson silt loam, eroded, undulatingDu6124523118kkbsal08919581:24000
Dickson cherty silt loam, eroded, undulatingDo4970523113kkbmal08919581:24000
Dickson cherty silt loam, undulatingDn3539523112kkblal08919581:24000
Dickson cherty silt loam, eroded, rollingDr3388523115kkbpal08919581:24000
Dickson silt loam, 0 to 2 percent slopesDs24305231162t8fral08919581:24000
Dickson cherty silt loam, rollingDp1151523114kkbnal08919581:24000
Dickson silt loam, 2 to 6 percent slopesDkB4780549759lg25ky16919651:15840
Dickson silt loam, 6 to 12 percent slopes, erodedDkC2483549761lg27ky16919651:15840
Dickson silt loam, 0 to 2 percent slopesDkA307549758lg24ky16919651:15840
Dickson silt loam, 2 to 6 percent slopes, erodedDkB2238549760lg26ky16919651:15840
Dickson silt loam, 2 to 6 percent slopesDkB1248550068lgd4ky23119851:20000
Dickson silt loam, 2 to 6 percent slopesDcB9219552548ljz4ky62019791:20000
Dickson silt loam, 2 to 6 percent slopesDcB2327924529772nbj9ky64619661:15840
Dickson silt loam, 6 to 12 percent slopes, erodedDcC2425624529782nbjbky64619661:15840
Dickson silt loam, 0 to 2 percent slopesDcA86324529762nbj8ky64619661:15840
Dickson silt loam, 2 to 5 percent slopesDkB180315244212rgxrtn01519991:24000
Dickson silt loam, 5 to 12 percent slopesDkC26105244222qh7htn01519991:24000
Dickson silt loam, 2 to 5 percent slopesDkB257995270082rgxrtn02119911:24000
Dickson silt loam, 2 to 5 percent slopesDkB29575310912rgxrtn02720021:24000
Dickson silt loam, 2 to 5 percent slopesDk4513627498652rgxrtn03119561:20000
Dickson silt loam, 2 to 5 percent slopesDkB28045234152rgxrtn03719771:15840
Dickson silt loam, 5 to 12 percent slopesDk329527498912qh7htn03920081:24000
Dickson silt loam, 2 to 5 percent slopesDl130627498672rgxrtn03920081:24000
Dickson silt loam, severely eroded rolling phaseDm360327290bzkrtn03920081:24000
Dickson silt loam, 2 to 5 percent slopesDkB180365270552rgxrtn04119681:15840
Dickson silt loam, 0 to 2 percent slopesDkA16675270542qh74tn04119681:15840
Dickson silt loam, 2 to 5 percent slopesDkB63935271042rgxrtn04319931:24000
Dickson silt loam, 2 to 5 percent slopes, erodedDz127035271962s8mctn05119501:20000
Dickson silt loam, 2 to 5 percent slopesDy124685271952wc0rtn05119501:20000
Dickson silt loam, eroded, rolling phaseD31676527171kpkjtn05119501:20000
Dickson silt loam, rolling phaseD2341527170kpkhtn05119501:20000
Dickson silty clay loam, severely eroded, rolling phaseD490527172kpkktn05119501:20000
Dickson silt loam, 2 to 5 percent slopesDnB22095273032wc0rtn05519651:15840
Dickson silt loam, 2 to 5 percent slopesDkB18515274582rgxrtn08119971:24000
Dickson silt loam, 2 to 5 percent slopesDa324527498712rgxrtn08319521:20000
Dickson silt loam, 5 to 12 percent slopesDc57027498922qh7htn08319521:20000
Dickson silt loam, shallowDls40366527562kpz4tn08519431:20000
Dickson silt loam, 2 to 5 percent slopesDl54455275612rgxrtn08519431:20000
Dickson silt loam, 5 to 12 percent slopesDlx16835275632qh7htn08519431:20000
Dickson silt loam, 2 to 5 percent slopesDkB210025301862rgxrtn08719991:24000
Dickson silt loam, 5 to 12 percent slopesDkC295301872qh7htn08719991:24000
Dickson silt loam, eroded gently sloping phaseDf8859527635kq1htn09919551:20000
Dickson silt loam, 2 to 5 percent slopesDe28905276342wc0rtn09919551:20000
Dickson silt loam, eroded gently sloping dark brown surface phaseDh971527637kq1ktn09919551:20000
Dickson silt loam, level dark brown surface phaseDg217527636kq1jtn09919551:20000
Dickson silt loam, 2 to 5 percent slopesDkB271235308582rgxrtn10119991:24000
Dickson silt loam, 5 to 12 percent slopesDkC22025308592qh7htn10119991:24000
Dickson silt loam, 2 to 5 percent slopesDkB261025258222wc0rtn10319991:24000
Dickson silt loam, 5 to 12 percent slopes, erodedDkC21217525823kn51tn10319991:24000
Dickson silt loam, 2 to 5 percent slopesDkB2161165277002rgxrtn11119921:24000
Dickson silt loam, 2 to 5 percent slopesDe3405277612rgxrtn11919551:20000
Dickson silt loam, 2 to 5 percent slopesDsB203025279802rgxrtn12519721:15840
Dickson silt loam, 5 to 12 percent slopesDsC28255279812qh7htn12519721:15840
Dickson silt loam, 2 to 5 percent slopesDkB25346257342rgxrtn12720021:24000
Dickson silt loam, 0 to 2 percent slopesDkA10816257332qh74tn12720021:24000
Dickson silt loam, 2 to 5 percent slopesDkB221078433652rgxrtn13320031:24000
Dickson silt loam, 2 to 5 percent slopesDkB21095606162rgxrtn13520001:24000
Dickson silt loam, 2 to 5 percent slopesDsB269215281692rgxrtn14719651:15840
Dickson silt loam, 5 to 12 percent slopesDsC213325281702qh7htn14719651:15840
Dickson silt loam, 5 to 12 percent slopesDa2225623968952qh7htn16119531:20000
Dickson silt loam, 2 to 5 percent slopesDb1089023968962rgxrtn16119531:20000
Dickson silt loam, 0 to 2 percent slopesSa238923969682qh74tn16119531:20000
Dickson-Gullied land complex, 2 to 12 percent slopesRd192423969612lg7btn16119531:20000
Dickson silt loam, 2 to 5 percent slopesDkB2245945283512rgxrtn16519931:20000
Dickson silt loam, 2 to 5 percent slopesDkB208435298792rgxrtn17719651:15840
Dickson silt loam, 2 to 5 percent slopesDkB24173280092wc0rtn18119961:24000
Dickson silt loam, 5 to 8 percent slopesDkC624328010c09ztn18119961:24000
Dickson silt loam, 2 to 5 percent slopesDkB7275234932rgxrtn18719611:15840
Dickson silt loam, 2 to 5 percent slopesDkB33225286422rgxrtn60419741:20000
Dickson silt loam, 2 to 5 percent slopesDk493224274322rgxrtn61019601:15840
Bewleyville-Dickson complex, 2 to 6 percent slopesBeB310024391662mw4stn70119851:24000

Map of Series Extent

Approximate geographic distribution of the DICKSON 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 .