Official Series Description


Lab Data Summary

Aggregate lab data for the FRANKSTOWN soil series. This aggregation is based on all pedons with a current taxon name of FRANKSTOWN, 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 FRANKSTOWN 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
12287P07071987KY045002Frankstown4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.2470703,-84.7323151
127WVU0014S01WV025002Frankstown5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.92,-80.3738889
14769PA0090031969PA009003Frankstown5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1352778,-78.6008333
14769PA0090041969PA009004Frankstown5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1402778,-78.6152778
n/a83KY-155-00383KY-155-003Frankstown4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a88P029587WV075004Frankstown6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a88P029687WV075005Frankstown6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a88P029787WV075006Frankstown6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

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

Soil series sharing subgroup-level classification with FRANKSTOWN, 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-2010-09-03-09 | Garrard and Lincoln Counties - 2006

    Typical pattern of soils and underlying material in the Garmon-Frankstown-Carpenter general soil map unit (Soil Survey of Garrard and Lincoln Counties, Kentucky; 2006).

  2. KY-2010-09-03-10 | Garrard and Lincoln Counties - 2006

    Typical pattern of soils and underlying material in the Pricetown-Teddy-Frankstown general soil map unit (Soil Survey of Garrard and Lincoln Counties, Kentucky; 2006).

  3. 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).

  4. 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).

  5. KY-2012-01-26-04 | Adair County - April 1964

    Diagram of the Sango-Mountview-Lawrence association in the uplands (Soil Survey of Adair County (Soil Survey of Adair County, Kentucky; April 1964).

  6. 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).

  7. KY-2012-01-27-30 | Casey County - August 1994

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

  8. KY-2012-01-27-32 | Casey County - August 1994

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

  9. KY-2012-01-27-33 | Casey County - August 1994

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

  10. 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).

  11. 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).

  12. KY-2012-01-30-10 | Green and Taylor Counties - July 1982

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

  13. KY-2012-02-01-10 | Marion County - August 1991

    Typical pattern of soils and parent material in the Carpenter-Garmon-Rohan general soil map unit (Soil Survey of Marion County, Kentucky; August 1991).

  14. KY-2012-02-01-46 | Pulaski County - December 1974

    Pattern of soils and underlying material in association 1 (Soil Survey of Pulaski County, Kentucky; December 1974).

  15. TN-2012-03-19-19 | Maury County - October 1959

    Sketch showing relative positions of soils in the Dellrose-Frankstown-Mimosa (cherty) assciation (Soil Survey of Maury County, TN; 1959).

Map Units

Map units containing FRANKSTOWN 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
Frankstown gravelly silt loam, 12 to 20 percent slopes, erodedFkD21291315924841qg3gky00120061:12000
Frankstown gravelly silt loam, 6 to 12 percent slopes, erodedFkC21068615924821qg3dky00120061:12000
Frankstown gravelly silt loam, 2 to 6 percent slopesFkB102215924811qg3cky00120061:12000
Frankstown silt loam, 12 to 20 percent slopesFkD35120548892lf56ky04519891:20000
Frankstown silt loam, 6 to 12 percent slopesFkC21370548891lf55ky04519891:20000
Frankstown silt loam, 2 to 6 percent slopesFkB1360548890lf54ky04519891:20000
Frankstown gravelly silt loam, 6 to 12 percent slopesFrC2495552337ljrbky15519861:20000
Frankstown gravelly silt loam, 12 to 20 percent slopesFrD1115552338ljrcky15519861:20000
Frankstown cherty silt loam, 12 to 20 percent slopesFcD12846552400ljtcky19919691:12000
Frankstown cherty silt loam, 6 to 12 percent slopesFcC3250552399ljtbky19919691:12000
Frankstown cherty silt loam, 20 to 30 percent slopesFcE2651552401ljtdky19919691:12000
Frankstown cherty silt loam, 2 to 6 percent slopesFcB142552398ljt9ky19919691:12000
Frankstown gravelly silt loam, 12 to 25 percent slopes, erodedFrD214369552955lkd8ky61819931:12000
Frankstown gravelly silt loam, 6 to 12 percent slopesFrC9421552954lkd7ky61819931:12000
Frankstown gravelly silt loam, 2 to 6 percent slopesFrB735552953lkd6ky61819931:12000
Frankstown silt loam, 6 to 12 percent slopesFkC11416552552ljz8ky62019791:20000
Frankstown silt loam, 12 to 20 percent slopesFkD9888552553ljz9ky62019791:20000
Frankstown silt loam, 20 to 30 percent slopesFkE9886552554ljzbky62019791:20000
Frankstown silt loam, 2 to 6 percent slopesFkB2069552551ljz7ky62019791:20000
Frankstown variant-Mertz complex, 2 to 6 percent slopes, very stonyFrB4851710295qz2oh08919861:15840
Frankstown channery silt loam, 8 to 15 percent slopesFrC810544863l8z7pa05719991:24000
Frankstown channery silt loam, 25 to 35 percent slopesFrE733544867l8zcpa05719991:24000
Frankstown channery silt loam, 15 to 25 percent slopesFrD560544865l8z9pa05719991:24000
Frankstown channery silt loam, 3 to 8 percent slopesFrB401544861l8z5pa05719991:24000
Frankstown coarse cherty silt loam, steep phaseFh8841527780kq65tn11919551:20000
Frankstown coarse cherty silt loam, eroded sloping phaseFe2863527777kq62tn11919551:20000
Frankstown cherty silt loam, eroded sloping phaseFa2274527773kq5ytn11919551:20000
Frankstown coarse cherty silt loam, eroded moderately steep phaseFg646527779kq64tn11919551:20000
Frankstown coarse cherty silt loam, sloping phaseFd577527776kq61tn11919551:20000
Frankstown coarse cherty silt loam, moderately steep phaseFf114527778kq63tn11919551:20000
Frankstown cherty silt loam, eroded moderately steep phaseFc105527775kq60tn11919551:20000
Frankstown cherty silt loam, moderately steep phaseFb7527774kq5ztn11919551:20000
Frankstown cherty silt loam, 5 to 12 percent slopesFrC706523505kkr8tn18719611:15840
Frankstown cherty silt loam, 12 to 20 percent slopesFrD667523506kkr9tn18719611:15840
Frankstown channery silt loam, 7 to 15 percent slopes13C1140521060kh6dva06919831:15840
Frankstown channery silt loam, 15 to 25 percent slopes13D666521061kh6fva06919831:15840
Frankstown channery silt loam, 2 to 7 percent slopes13B516521059kh6cva06919831:15840
Frankstown channery silt loam, 25 to 35 percent slopes13E385521062kh6gva06919831:15840
Frankstown channery silt loam, 15 to 25 percent slopes13D1730256462xr82va84020171:12000
Frankstown channery silt loam, 25 to 35 percent slopes13E130256472xr83va84020171:12000
Frankstown channery silt loam, 7 to 15 percent slopes13C130256482xr84va84020171:12000
Frankstown silt loam, karst, 8 to 15 percent slopesFkC5197553017lkg8wv02520021:24000
Frankstown silt loam, karst, 3 to 8 percent slopesFkB5013553018lkg9wv02520021:24000
Frankstown silt loam, karst, 15 to 35 percent slopes, very rockyFoE2469553115lkkfwv02520021:24000
Frankstown silt loam, karst, 15 to 25 percent slopesFkD1665553016lkg7wv02520021:24000
Frankstown silt loam, karst, 3 to 15 percent slopes, very rockyFoC862553114lkkdwv02520021:24000
Frankstown silt loam, 8 to 15 percent slopesFaC342117130991vhm8wv06319621:24000
Frankstown-Rock outcrop complex, 15 to 25 percent slopesFeD235417131061vhmhwv06319621:24000
Frankstown silt loam, 15 to 25 percent slopesFaD161917131021vhmcwv06319621:24000
Frankstown-Rock outcrop complex, 8 to 15 percent slopesFeC146317131051vhmgwv06319621:24000
Frankstown silt loam, 3 to 8 percent slopesFaB127517130981vhm7wv06319621:24000
Frankstown-Rock outcrop complex, 25 to 35 percent slopesFeE115817131071vhmjwv06319621:24000
Frankstown silt loam, karst, 8 to 15 percent slopesFcC102117130901vhlzwv06319621:24000
Frankstown silt loam, karst, 3 to 8 percent slopesFcB82417130891vhlywv06319621:24000
Frankstown silt loam, 25 to 35 percent slopesFaE34317131031vhmdwv06319621:24000
Frankstown silt loam, karst, 15 to 35 percent slopes, very rockyFdE26417131081vhmkwv06319621:24000
Frankstown silt loam, karst, 15 to 25 percent slopesFcD12217130971vhm6wv06319621:24000

Map of Series Extent

Approximate geographic distribution of the FRANKSTOWN 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 .