Official Series Description


Lab Data Summary

Aggregate lab data for the HUMPHREYS soil series. This aggregation is based on all pedons with a current taxon name of HUMPHREYS, 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 HUMPHREYS 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
12201P04611900TN135001Humphreys6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.6800003,-87.8874969
12298P03661998TN135001Humphreys7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.7525291,-87.8072815

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the HUMPHREYS 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 HUMPHREYS 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 HUMPHREYS 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 HUMPHREYS 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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Competing Series

Soil series competing with HUMPHREYS 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 HUMPHREYS 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 HUMPHREYS 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 HUMPHREYS, 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-2012-01-26-05 | Adair County - April 1964

    Diagram of the Staser-Taft-Landisburg association on flood plains, terraces, and foot slopes (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. TN-2010-11-02-08 | Hickman County - 2008

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

  6. TN-2010-11-02-16 | Lewis County - 2006

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

  7. TN-2010-11-02-25 | Moore County - 2006

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

  8. TN-2012-03-16-06 | Dickson County - 2002

    The relationship of soils, landscape, and parent material in the Saffell-Lax and the Armour-Humphreys-Sullivan general soil map units (Soil Survey of Dickson County, TN; 2002).

  9. TN-2012-03-19-05 | Hardin County - June 1963

    Major soil series in soil associations 8 and 10 and their relationship to the landscape (Soil Survey of Hardin County, TN; 1963).

  10. TN-2012-03-19-34 | Wayne County - 2000

    Typical pattern of soils and parent material in the Biffle-Sulphura-Ironcity general soil map unit (Soil Survey of Wayne County, TN; 2000).

  11. TN-2012-03-19-38 | Williamson County - August 1964

    Major and minor soils and underlying parent materials in the Mountview-Baxter-Bodine association (Soil Survey of Williamson County, TN; 1964).

Map Units

Map units containing HUMPHREYS 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
Humphreys cherty silt loamHu888523051kk8mal07719731:20000
Humphreys silt loam level phaseHmv3264522784kk00al08319531:20000
Humphreys cherty silt loam undulating phaseHru1452522785kk01al08319531:20000
Humphreys cherty silt loamHw2911523156kkd0al08919581:24000
Humphreys silt loamHx2443523157kkd1al08919581:24000
Humphreys cherty silt loam, 6 to 12 percent slopes, erodedHcC21505549766lg2dky16919651:15840
Humphreys cherty silt loam, 2 to 6 percent slopesHcB737549764lg2bky16919651:15840
Humphreys cherty silt loam, 6 to 12 percent slopesHcC411549765lg2cky16919651:15840
Humphreys cherty silt loam, 6 to 12 percent slopes, erodedHuC2247224529902nbjqky64619661:15840
Humphreys cherty silt loam, 2 to 6 percent slopesHuB97024529892nbjpky64619661:15840
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB179525453472qsg7tn00520111:12000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC90825453482qsg8tn00520111:12000
Humphreys gravelly silt loam, 0 to 3 percent slopes, rarely floodedHuA17925453462qsg5tn00520111:12000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB315527016kpdjtn02119911:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC2325270172qh71tn02119911:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC3436368112qh71tn02720021:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB986368102qh70tn02720021:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHr8095249242qh70tn03119561:20000
Humphreys cherty silt loam, 1 to 4 percent slopesHuB2067523420kknjtn03719771:15840
Humphreys cherty silt loam, undulating phaseGb3518327312bzlgtn03920081:24000
Humphreys cherty silt loam, rolling phaseGa397327311bzlftn03920081:24000
Humphreys cherty silt loamHd224327316bzlltn03920081:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB44525271102qh70tn04319931:24000
Humphreys gravelly silt loam, 0 to 2 percent slopes, occasionally floodedHuA2654527109kphjtn04319931:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC20975271112qh71tn04319931:24000
Humphreys cherty silt loamHk521527213kplwtn05119501:20000
Humphreys cherty silt loam, 5 to 12 percent slopesHuC378527324kpqgtn05519651:15840
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB2155273232qh70tn05519651:15840
Humphreys cherty silt loam, 1 to 6 percent slopesHuB80410178661355dtn06519801:15840
Humphreys cherty silt loam, 2 to 5 percent slopes, erodedHcB2507327576bzvztn07119611:15840
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC9625452632qs87tn07920121:12000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB7525452622qs86tn07920121:12000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB114895274692qh70tn08119971:24000
Tarklin-Humphreys complex, 5 to 12 percent slopes, erodedThC210228527493kpwxtn08119971:24000
Humphreys gravelly silt loam, 0 to 2 percent slopes, occasionally floodedHuA104527468kpw3tn08119971:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHa9655275232qh70tn08319521:20000
Humphreys gravelly silt loam, 2 to 5 percent slopesHg332425275692qh70tn08519431:20000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC7735301962qh71tn08719991:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB5505301952qh70tn08719991:24000
Humphreys cherty silt loamHa700527648kq1xtn09919551:20000
Tarklin-Humphreys complex, 5 to 12 percent slopes, erodedTmC23186530886ktfctn10119991:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB19585308612qh70tn10119991:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC17525308622qh71tn10119991:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB25065277042qh70tn11119921:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC4175277052qh71tn11119921:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesAb35885277252qh71tn11919551:20000
Humphreys gravelly silty clay loam, 5 to 12 percent slopes, severely erodedHpC2233127499302qh7jtn11919551:20000
Humphreys gravelly silt loam, 2 to 5 percent slopesAa20465277242qh70tn11919551:20000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB25045279852qh70tn12519721:15840
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC6036257452qh71tn12720021:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC2048432372qh71tn13320031:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB448432362qh70tn13320031:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB71305606242qh70tn13520001:24000
Humphreys gravelly silt loam, 0 to 3 percent slopes, rarely floodedHuA3261560623ltcmtn13520001:24000
Tarklin-Humphreys complex, 5 to 12 percent slopes, erodedThC220560655ltdntn13520001:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC95606252qh71tn13520001:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHcC6575281762qh71tn14719651:15840
Humphreys gravelly silt loam, 2 to 5 percent slopesHcB3185281752qh70tn14719651:15840
Humphreys gravelly silt loam, 2 to 5 percent slopesGa994323969062qh70tn16119531:20000
Humphreys gravelly silt loam, 1 to 5 percent slopesHmB66631604541ttwvtn16119531:20000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB19845283622qh70tn16519931:20000
Humphreys gravelly silt loam, 2 to 8 percent slopes, rarely floodedHuB194530024ksjktn16919931:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHuC10745328016c0b5tn18119961:24000
Humphreys gravelly silt loam, 2 to 5 percent slopesHuB7671328015c0b4tn18119961:24000
Humphreys gravelly silt loam, 5 to 12 percent slopesHpC395827499292qh71tn18719611:15840
Humphreys gravelly silt loam, 2 to 5 percent slopesHpB127527499172qh70tn18719611:15840
Humphreys gravelly silty clay loam, 5 to 12 percent slopes, severely erodedAmC32275234532qh7jtn18719611:15840

Map of Series Extent

Approximate geographic distribution of the HUMPHREYS 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 .