Official Series Description


Lab Data Summary

Aggregate lab data for the NAKAI soil series. This aggregation is based on all pedons with a current taxon name of NAKAI, 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 NAKAI 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
3582P088882AZ017009Nakai7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties35.5711098,-110.558609
n/a82P078782UT037007Nakai7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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Soil series sharing subgroup-level classification with NAKAI, 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

No block diagrams are available.

Map Units

Map units containing NAKAI 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
Urban land-Nakai complex, 1 to 15 percent slopes6271416782822sdvvaz71120081:24000
Monue-Sheppard-Nakai complex, 1 to 6 percent slopes329611824084172sdx9az71320111:24000
Nakai-Somorent family complex, 1 to 15 percent slopes347218924333442sdxlaz71320111:24000
Nakai very fine sandy loam, 0 to 6 percent slopes3383024954232sdytaz71320111:24000
Nakai-Monue very fine sandy loams,2377820547111txwaz71419851:24000
Sheppard-Nakai complex, 1 to 8 percent slopes336475547241ty9az71419851:24000
Nakai fine sandy loam, 3 to 15 percent slopes224190547101txvaz71419851:24000
Nakai-Monue very fine sandy loams, 1 to 5 percent slopes679192579812qsx9az71520071:24000
Nakai fine sandy loam, 3 to 10 percent slopes4021617504535jy0but62419851:24000
Nakai-Sheppard complex4310281504538jy0fut62419851:24000
Nakai-Redlands complex4210271504537jy0dut62419851:24000
Nakai-Moenkopie complex417602504536jy0cut62419851:24000
Shalet-Nakai complex655176504562jy16ut62419851:24000
Nakai fine sand, 2 to 8 percent slopes583659553801vmgut63319831:24000
Bluechief-Limeridge-Nakai complex, 1 to 6 percent slopes740753554931vr3ut63819851:24000
Myton family-Nakai-Redhouse complex3219075554561vpxut63819851:24000
Nakai-Moffat-Sheppard association3716324554611vq2ut63819851:24000
Nakai fine sandy loam, 1 to 6 percent slopes366203554601vq1ut63819851:24000
Sheppard-Nakai complex, 0 to 8 percent slopes921224423979892lh9hut6421:63360
Nakai very fine sandy loam, 2 to 6 percent slopesNbC38425552931vjnut64319761:63000
Deleco-Nakai-Rock outcrop association, slopingDND24410552721vhzut64319761:63000
Nakai loamy fine sand, 1 to 8 percent slopesNaB5410552921vjmut64319761:63000
Moffat-Sheppard-Nakai complex, 2 to 30 percent slopes50461363559791206rut68620041:24000
Nakai-Sheppard complex, 2 to 15 percent slopes51389033598652094ut68620041:24000

Map of Series Extent

Approximate geographic distribution of the NAKAI 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 .