Official Series Description


Lab Data Summary

Aggregate lab data for the NEEDMORE soil series. This aggregation is based on all pedons with a current taxon name of NEEDMORE, 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 NEEDMORE 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
12240A48901954KY001017Needmore4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.0166664,-85.2297211
n/a00KY-001-00300KY-001-003Needmore3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a40A48891954KY001016Needmore4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a01P02972000KY001003Needmore6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a01P02982000KY001004Needmore6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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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 NEEDMORE, 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-2012-01-26-06 | 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).

  4. 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).

  5. TN-2010-11-02-19 | McMinn County - 2004

    Relationship of soils and parent material in the Tellico-Red Hills-Nonaburg and Lostcove-Unicoi-Cataska general soil map units (Soil Survey of McMinn County, Tennessee; 2004).

  6. TN-2012-03-19-26 | McMinn County - 2004

    Relationship of soils and parent material in the Tellico-Red Hills-Nonaburg and Lostcove-Unicoi-Cataska general soil map units (Soil Survey of McMinn County, TN; 2004).

Map Units

Map units containing NEEDMORE 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
Needmore silt loam, 6 to 20 percent slopes, very rockyNfD546915924051qg0xky00120061:12000
Needmore silt loam, 6 to 12 percent slopes, erodedNeC2177815924351qg1wky00120061:12000
Needmore silty clay loam, 12 to 20 percent slopes, severely erodedNeD3119015924371qg1yky00120061:12000
Needmore silt loam, 2 to 6 percent slopesNeB35015924321qg1sky00120061:12000
Needmore silty clay loam, 6 to 12 percent slopes, erodedNcC2578552440ljvnky19919691:12000
Needmore silty clay, 6 to 12 percent slopes, severely erodedNdC1152552568ljzsky62019791:20000
Needmore silty clay loam, 6 to 12 percent slopes, erodedNeC2208424529972nbjyky64619661:15840
Needmore silt loam, 2 to 6 percent slopesNdB154724529962nbjxky64619661:15840
Needmore silty clay, 6 to 12 percent slopes, severely erodedNmC333224529982nbjzky64619661:15840
Needmore silty clay loam, eroded rolling phaseNc4742525181kmhbtn05919541:15840
Needmore silt loam, undulating phaseNb1874525180kmh9tn05919541:15840
Needmore silt loam, rolling phaseNa875525179kmh8tn05919541:15840
Needmore silt loam, rolling, 5 to 12 percent slope76C610525342kmnjtn06320071:24000
Dandridge-Needmore complex, 12 to 35 percent slopes (Sulphura)DaF7341327544bztytn07119611:15840
Dandridge-Needmore complex, 8 to 12 percent slopes (Sulphura)DaD515327543bztxtn07119611:15840
Nonaburg-Needmore complex, 12 to 25 percent slopes, very rockyNnD4061526148knhjtn10719991:24000
Needmore-Corryton complex, 5 to 12 percent slopesNcC2408526151knhmtn10719991:24000
Nonaburg-Needmore complex, 5 to 12 percent slopes, very rockyNnC2170526147knhhtn10719991:24000
Nonaburg-Needmore-Rock outcrop complex, 25 to 60 percent slopesNoF1189526149knhktn10719991:24000
Corryton-Needmore complex, 2 to 5 percent slopes, rockyCrB442526150knhltn10719991:24000
Needmore silt loam, 5 to 12 percent slopesNeC2438523775kl0ztn13919971:24000
Needmore silt loam, 12 to 25 percent slopesNeD2255523776kl10tn13919971:24000
Needmore silt loam, 5 to 12 percent slopesNdC2522528597kr1jtn60219731:15840
Needmore silt loam, 2 to 5 percent slopesNdB785528596kr1htn60219731:15840
Needmore-Opequon complex, 35 to 70 percent slopes43F923225148252qdc3va16320101:24000
Needmore-Opequon complex, 15 to 35 percent slopes43E882625148242qdc2va16320101:24000
Litz-Needmore complex, 35 to 70 percent slopes, very stony34F525825148112qdbmva16320101:24000
Needmore-Opequon complex, 3 to 15 percent slopes43C298425148232qdc1va16320101:24000
Litz-Needmore complex, 15 to 35 percent slopes, very stony34E289125148102qdblva16320101:24000
Groseclose-Needmore complex, 25 to 35 percent slopes28E205825148012qdb9va16320101:24000
Groseclose-Needmore-Urban land complex, 0 to 15 percent slopes29C124825148022qdbbva16320101:24000
Needmore-Urban land complex, 15 to 35 percent slopes44E28525148262qdc4va16320101:24000
Litz-Needmore complex, 3 to 15 percent slopes, very stony34C3725148092qdbkva16320101:24000

Map of Series Extent

Approximate geographic distribution of the NEEDMORE 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 .