Official Series Description


Lab Data Summary

Aggregate lab data for the NESS soil series. This aggregation is based on all pedons with a current taxon name of NESS, 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 NESS 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
7289P073189KS081014Ness7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4269447,-101.035553
7381P065481KS135001Ness7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6094437,-99.9338913
7300P0075S1999KS083001Ness6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1385002,-99.9357758

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NESS 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 NESS 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 NESS 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 NESS 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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There are insufficient data to create the 3D flats position figure.

Competing Series

Soil series competing with NESS 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 NESS 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 NESS 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 NESS, 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. KS-2012-01-20-22 | Clark County - December 1982

    Typical pattern of soils in the Harney association (Soil Survey of Clark County, Kansas; 1982).

  2. KS-2012-01-20-46 | Edwards County - September 1973

    Typical pattern of soils in association 1 (Soil Survey of Edwards County, Kansas; 1973).

  3. KS-2012-01-20-48 | Edwards County - September 1973

    Soils of associations 5 and 6 (Soil Survey of Edwards County, Kansas; 1973).

  4. KS-2012-01-23-34 | Hodgeman County - June 1973

    Pattern of soils in association 1 (Soil Survey of Hodgeman County, Kansas; 1973).

  5. KS-2012-01-23-36 | Hodgeman County - June 1973

    Pattern of soils in associations 6 and 12 (Soil Survey of Hodgeman County, Kansas; 1973).

  6. KS-2012-01-23-51 | Lane County - November 1972

    Pattern of soils in association 1 (Soil Survey of Lane County, Kansas; 1972).

  7. TX-2012-03-20-33 | Dallam County - March 1975

    Relationship of soils and underlying material in the Gruver-Sherm-Dumas association (Soil Survey of Dallam County, TX; 1975).

  8. TX-2012-03-21-74 | Sherman County - July 1975

    Typical pattern of soils in the Sherm-Gruver association (Soil Survey of Sherman County, TX; 1975).

  9. TX-2012-03-21-75 | Sherman County - July 1975

    Typical pattern of soils in the Sunray-Conlen association (Soil Survey of Sherman County, TX; 1975).

Map Units

Map units containing NESS 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
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded698213968612zwlnco06319961:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded1748921052552zwlnco07320011:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded5710091950202zwlnco12119821:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded27148941440465307plks00919791:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271430161149574307plks02319871:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271430491381728307plks02519801:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded27142601150583307plks03919851:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded27148551380382307plks04719671:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded2714106431152327307plks05519621:24000
Ness-Pleasant complex, 0 to 3 percent slopes1665101411523212zwlkks05519621:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271458741380445307plks05719621:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded27144031150696307plks06319741:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271425431380666307plks06719651:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded2714108331380583307plks06919651:24000
Ness-Pleasant complex, 0 to 3 percent slopes1665161513805762zwlkks06919651:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271436411151836307plks07119591:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271412931152233307plks07519591:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271468981380624307plks08119651:24000
Ness-Pleasant complex, 0 to 3 percent slopes166569213806202zwlkks08119651:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271420561152412307plks08319661:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271417061152280307plks09319611:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded27147351380532307plks09719831:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271450561152029307plks10119661:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271413561150538307plks10919621:24000
Ness silty clay271560414292012zt7dks11319801:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded2714111481381798307plks11919731:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded27145511152082307plks13519711:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded27147691380134307plks14519761:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded2714407772986307plks15319791:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271469971151988307plks17119631:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271439911382648307plks17519631:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271413931150008307plks17919821:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271438181149625307plks18119671:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271414091382568307plks18719591:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271434541150463307plks19319781:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271418401150205307plks19919841:24000
Ness silty clay loam, 0 to 1 percent slopes, occasionally ponded271429401151950307plks20319631:24000
Ness clay, 0 to 1 percent slopes, frequently pondedRa34713820702rgf9ok02519581:20000
Ness clay, 0 to 1 percent slopes, frequently pondedRa50503849182rgf9ok13919591:24000
Ness clay, 0 to 1 percent slopes, frequently pondedNe40873647692rgf9tx11119701:24000
Ness clay, 0 to 1 percent slopes, frequently pondedNe37823674482rgf9tx20519731:24000
Ness clay, 0 to 1 percent slopes, frequently pondedNe32733679302rgf9tx23319721:24000
Ness clay, 0 to 1 percent slopes, frequently pondedRa2323694752rgf9tx29519711:24000
Ness clay, 0 to 1 percent slopes, frequently pondedNc44073708272rgf9tx34119681:24000
Ness clay, 0 to 1 percent slopes, frequently pondedRa152773710952rgf9tx35719661:20000
Ness clay, 0 to 1 percent slopes, frequently pondedNe44963721072rgf9tx42119701:24000

Map of Series Extent

Approximate geographic distribution of the NESS 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 .