Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
7996KS15531296KS155312Nash1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8055,-98.1268616

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the NASH series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the NASH series and siblings. 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 NASH 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 .

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.

Click the image to view it full size.

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

Competing Series

Soil series competing with NASH share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the NASH 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 NASH 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.

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 NASH, 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-2012-01-25-17 | Reno County - March 1966

    Cross section of the Nash-Lucien association in the south-central part of the county (Soil Survey of Reno County, Kansas; 1966).

  2. OK-2012-02-16-32 | Garfield County - October 1967

    Typical pattern of soils in the Grant-Pond Creek association, and Port, Reinach, and Pulaski soils of soil association 2 on the bordering flood plains (Soil Survey of Garfield County, Oklahoma; October 1967).

  3. OK-2012-02-17-11 | Major County - October 1968

    Soil associations in the eastern part of the county (Soil Survey of Major County, Oklahoma; October 1968).

  4. OK-2012-02-17-49 | Stephens County - 1964

    Typical pattern of soils in association 3 (Soil Survey of Stephens County, Oklahoma; 1964).

Map Units

Map units containing NASH 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
Nash silt loam, 1 to 3 percent slopes6384609614438652yws8ks15519991:24000
Nash-Lucien silt loams, 7 to 15 percent slopes, moderately eroded6386228614438672ywsbks15519991:24000
Nash-Lucien silt loams, 3 to 7 percent slopes638576314438662yws9ks15519991:24000
Grant-Nash complex, 3 to 8 percent slopes, erodedGtD219827381429dsx5ok00319711:24000
Ironmound-Nash complex, 3 to 12 percent slopesIrNE1248622474nwqtok00319711:24000
Ironmound-Nash complex, 5 to 12 percent slopesQwD23832381916dtdwok01519671:24000
Nash-Ironmound complex, 3 to 8 percent slopesNaD12683381962dtgcok01719721:24000
Nash-Ironmound complex, 3 to 8 percent slopes, erodedNaD25730381963dtgdok01719721:24000
Nash-Ironmound complex, 3 to 8 percent slopes, severely erodedNaD31230381964dtgfok01719721:24000
Nash silt loam, 1 to 3 percent slopesNaB2585382507dv0yok04719651:24000
Nash silt loam, 3 to 5 percent slopesNaC1650382508dv0zok04719651:24000
Ironmound-Nash complex, 5 to 12 percent slopes478394382580dv39ok04919821:24000
Lucien-Nash complex, 5 to 12 percent slopes2172180382640dv57ok05119751:24000
Nash-Lucien complex, 1 to 5 percent slopes3023580382650dv5kok05119751:24000
Nash loam, 5 to 8 percent slopes297657382648dv5hok05119751:24000
Nash loam, 3 to 5 percent slopes287385382647dv5gok05119751:24000
Ironmound-Nash complex, 3 to 12 percent slopes465635382736dv8bok05319831:24000
Nash-Lucien complex, 5 to 12 percent slopes3363433383790dwcbok08719761:24000
Nash-Lucien complex, 3 to 5 percent slopes3213341383789dwc9ok08719761:24000
Grant-Nash complex, 5 to 8 percent slopes, erodedGnD23671383830dwdmok09319651:24000
Grant-Nash complex, 5 to 8 percent slopesGnD420383829dwdlok09319651:24000
Nash and Noble soils, 5 to 8 percent slopesNnD5216384872dxh7ok13719601:24000
Nash and Noble soils, 3 to 5 percent slopesNnC3042384871dxh6ok13719601:24000
Nash very fine sandy loam, 1 to 3 percent slopesNaB1310384870dxh5ok13719601:24000

Map of Series Extent

Approximate geographic distribution of the NASH 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 .