Official Series Description


Lab Data Summary

Aggregate lab data for the NELSE soil series. This aggregation is based on all pedons with a current taxon name of NELSE, 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 NELSE were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

There are insufficient data to create the lab data summary figure.


Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

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 NELSE, 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-2010-09-03-17 | Lawrence and Martin Counties - 2005

    Typical pattern of soils, parent material, and topography in the Udorthents-Nelse-Allegheny and Shelocta-Hazleton-Blairton general soil map units. The Udorthents-Nelse-Allegheny general soil map unit is along the Tug and Lavista Forks of the Big Sandy River and their major tributaries, and the Shelocta-Hazleton-Blairton general soil map unit is on the mountains (Soil Survey of Lawrence and Martin Counties, Kentucky; 2005).

  2. KY-2010-09-03-27 | Cumberland County - 1998

    Typical pattern of the soils in the Huntington-Elk-Nelse-Grigsby and Holston-Monongahela-Waynesboro general soil map units and the underlying material (Soil Survey of Cumberland County, Kentucky; 1998).

  3. KY-2012-02-01-01 | Livingston County - September 1993

    Relationship of soils to topography and underlying material in the Huntington-Otwell-Lindside-Wheeling general soil map unit (Soil Survey of Livingston County, Kentucky; September 1993).

  4. KY-2012-02-01-37 | Pike County - June 1990

    Along the Levisa and Russell Forks of the Big Sandy River, the soils in the valleys are in the Nelse-Shelbiana-Udorthents general soil map unit and those on the mountains are in the Marrowbone-Fedscreek-Kimper-Dekalb map unit (Soil Survey of Pike County, Kentucky; June 1990).

Map Units

Map units containing NELSE 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
Nelse fine sandy loam, 10 to 25 percent slopes, frequently floodedNeD2000551465lhv6ky05719911:20000
Chagrin-Nelse-Wheeling complex, 2 to 75 percent slopes, frequently floodedCnF66115327371nfy4ky11120051:12000
Nelse loam, frequently floodedNa1711549342lfmqky13919891:20000
Nelse-Huntington-Wheeling complex, 2 to 55 percent slopes, frequently floodedNcE1312549344lfmsky13919891:20000
Nelse-Huntington complex, frequently floodedNb259549343lfmrky13919891:20000
Nelse loam, 4 to 25 percent slopes, frequently floodedNeD1724550045lgcdky19519861:24000
Nelse, frequently flooded-Urban land, rarely flooded complex, 4 to 25 percent slopesuNeuD154727382692qdmfky63319791:24000
Nelse loam, 4 to 25 percent slopes, frequently floodedNeD1981550875lh75ky63919911:24000
Nelse fine sandy loam, 4 to 25 percent slopes, frequently floodedNeD2770550909lh88ky64019961:24000
Nelse fine sandy loam, 0 to 3 percent slopes, occasionally floodedNeA61824012292llp0md00120091:12000
Chagrin-Nelse-Wheeling complex, 2 to 75 percent slopes, frequently floodedCNWXFF54926528402q6yloh06119801:15840
Nelse sandy loam, occasionally floodedNe2854524812km3ftn60620011:24000
Nelse silt loam, 3 to 25 percent slopes, frequently floodedNe737553354lkt4wv04320051:24000
Nelse silt loam, 3 to 25 percent slopesNeD825515031k8xxwv09919931:24000
Potomac-Nelse complex, 0 to 5 percent slopes, extremely stony, frequently floodedPxA47824851102pdyvwv62220101:12000
Potomac-Nelse complex, 0 to 5 percent slopes, extremely stony, frequently floodedPxA11324977572pdyvwv62320101:12000

Map of Series Extent

Approximate geographic distribution of the NELSE 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 .