Official Series Description


Lab Data Summary

Aggregate lab data for the NALIM soil series. This aggregation is based on all pedons with a current taxon name of NALIM, 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 NALIM 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
7408KS17300808KS173008Nalim3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8227768,-97.3075027
7908KS09524108KS095241Nalim3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.690033,-97.9307022
7908KS09524208KS095242Nalim3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.6884956,-98.1802597
7908KS09524308KS095243Nalim3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.4241219,-98.4466095
7908KS15901808KS159018Nalim3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2024994,-98.077774
7992P054392KS079003Nalim7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9964342,-97.6081092
7906N1021S2006KS047904Nalim8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.7949715,-99.1805801

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NALIM 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 NALIM 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 NALIM 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 NALIM 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 hills figure.

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 NALIM 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 NALIM 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 NALIM 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.

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

Soil series sharing subgroup-level classification with NALIM, 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-2010-09-03-03 | Reno County - 2002

    Typical pattern of soils and parent material in the Shellabarger-Albion-Nalim association (Soil Survey of Reno County, Kansas; 2002).

Map Units

Map units containing NALIM 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
Nalim loam, 1 to 3 percent slopes5982975224788052r8z0ks00719731:24000
Nalim loam, 0 to 1 percent slopes5908384324787482tt4hks00719731:24000
Nalim and Shellabarger fine sandy loams, 0 to 1 percent slopes5981282024787882tt4jks00719731:24000
Nalim clay loam, 3 to 6 percent slopes, eroded5984274924788502tt4lks00719731:24000
Nalim loam, 1 to 3 percent slopes59822879324788062r8z0ks07719651:24000
Nalim loam, 0 to 1 percent slopes59082684324787492tt4hks07719651:24000
Nalim loam, 3 to 6 percent slopes5983347124788322tt4kks07719651:24000
Nalim clay loam, 3 to 6 percent slopes, eroded5984128924788482tt4lks07719651:24000
Nalim-Shellabarger sandy loams, 0 to 1 percent slopes5896367714736722tt4gks07919701:24000
Nalim loam, 1 to 3 percent slopes59825932524788072r8z0ks09519771:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes59602721714448162tt5vks09519771:24000
Nalim loam, 0 to 1 percent slopes59081944514447892tt4hks09519771:24000
Nalim clay loam, 3 to 6 percent slopes, eroded5984632324788522tt4lks09519771:24000
Nalim loam, 3 to 6 percent slopes5983373324788352tt4kks09519771:24000
Nalim and Shellabarger fine sandy loams, 0 to 1 percent slopes5981167224787892tt4jks09519771:24000
Shellabarger and Nalim soils, 3 to 6 percent slopes59473614448052tt5pks09519771:24000
Nalim loam, 1 to 3 percent slopes598229724788082r8z0ks09719831:24000
Nalim loam, 1 to 3 percent slopes5982579924788092r8z0ks15119651:24000
Nalim clay loam, 3 to 6 percent slopes, eroded5984144624788492tt4lks15119651:24000
Nalim loam, 0 to 1 percent slopes590813214451462tt4hks15119651:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes59603563114438532tt5vks15519991:24000
Nalim loam, 0 to 1 percent slopes59082324714438362tt4hks15519991:24000
Shellabarger and Nalim soils, 3 to 6 percent slopes5947160514438482tt5pks15519991:24000
Nalim loam, 1 to 3 percent slopes59824451124788102r8z0ks17319761:24000
Nalim-Shellabarger sandy loams, 0 to 1 percent slopes58961221414439782tt4gks17319761:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes59601144514439892tt5vks17319761:24000
Nalim loam, 0 to 1 percent slopes59081134714439792tt4hks17319761:24000
Shellabarger-Nalim complex, 1 to 3 percent slopes5960700724787702tt5vks18519751:24000
Nalim and Shellabarger fine sandy loams, 0 to 1 percent slopes5981330016774222tt4jks18519751:24000
Nalim loam, 0 to 1 percent slopes5908173724787512tt4hks18519751:24000
Nalim loam, 1 to 3 percent slopes59823215924788112r8z0ks19119741:24000
Nalim loam, 0 to 1 percent slopes59082287024787522tt4hks19119741:24000
Nalim loam, 3 to 6 percent slopes5983148824788342tt4kks19119741:24000
Nalim clay loam, 3 to 6 percent slopes, eroded5984113024788512tt4lks19119741:24000

Map of Series Extent

Approximate geographic distribution of the NALIM 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 .