Official Series Description


Lab Data Summary

Aggregate lab data for the NAKARNA soil series. This aggregation is based on all pedons with a current taxon name of NAKARNA, 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 NAKARNA 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
43A02N0114S2001WA063003Nakarna6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.5467186,-117.1578674

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NAKARNA 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 NAKARNA 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 NAKARNA 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 NAKARNA 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 terrace figure.

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

Competing Series

Soil series competing with NAKARNA 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 NAKARNA 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 NAKARNA 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.

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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 NAKARNA, 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. ID-2010-08-31-06 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 6 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  2. ID-2010-08-31-10 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in general soil map unit 5 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

  3. ID-2011-06-01-19 | St. Joe Area, Parts of Benewah and Shoshone Counties - 2002

    Typical pattern of soils and underlying material in General Soil Map Unit 6 (Soil Survey of St. Joe Area, Parts of Benewah and Shoshone Counties, Idaho; 2002).

Map Units

Map units containing NAKARNA 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
Scand-Nakarna complex, 35 to 65 percent slopesSc13255677875qrcyid05720131:24000
Rettig-Grandad-Nakarna complex, 30 to 65 percent slopesGr72813644889pn1wid05720131:24000
Nakarna complex, 35 to 65 percent slopesNk1j1462250198154qbid05720131:24000
Neva-Nakarna, moist-Nakarna, dry complex, 20 to 65 percent slopesNe11333704714rn9qid05720131:24000
Nakarna ashy silt loam, 35 to 65 percent slopesNk2j1245250198254q7id05720131:24000
Scand-Nakarna, warm complex, 25 to 65 percent slopesSb3808645287pngqid05720131:24000
Nakarna complex, 35 to 65 percent slopes741114715349154qbid60819941:24000
Nakarna ashy silt loam, 35 to 65 percent slopes711101915348854q7id60819941:24000
Nakarna silt loam, 15 to 35 percent slopes70583015348754q6id60819941:24000
Nakarna-Flewsie silt loams, high precipitation, 35 to 65 percent slopes75182215349254qcid60819941:24000
Nakarna silt loam, high precipitation, 15 to 35 percent slopes72168315348954q8id60819941:24000
Nakarna ashy silt loam, high precipitation, 35 to 65 percent slopes7316671534902x1zmid60819941:24000
Nakarna-Grandad-Humic Udivitrands families, complex, mica schist, lower sideslopes toeslopes and stream bottoms of drainages in rolling uplands, south aspects2lgqx429368112lgqxid60819941:24000
Township-Rettig-Nakarna complex, 35 to 65 percent slopes2354501777398v2ycid61220031:24000
Nakarna ashy silt loam, high precipitation, 35 to 65 percent slopes1728807773482x1zmid61220031:24000
Nakarna-Nakarna, warm complex, 35 to 65 percent slopes173330777349v2wsid61220031:24000
Nakarna ashy silt loam, 15 to 35 percent slopes171301776664v25pid61220031:24000
Nakarna-Grandad-Humic Udivitrands families, complex, mica schist, lower sideslopes toeslopes and stream bottoms of drainages within rolling uplands, north aspects718229023974452lgqyid6701:24000
Nakarna-Grandad families, complex, weathered mica schists, dissected rolling uplands with mass wasted inclusions, north aspects761210223974692lgrqid6701:24000
Nakarna-Grandad-Humic Udivitrands families, complex, mica schist, lower sideslopes toeslopes and stream bottoms of drainages in rolling uplands, south aspects71799723974442lgqxid6701:24000
Nakarna silt loam, 15 to 35 percent slopes54q6227285099554q6id6701:24000
Nakarna silt loam, high precipitation, 35 to 65 percent slopes54q978285099854q9id6701:24000
Nakarna ashy silt loam, 35 to 65 percent slopes54q750285099654q7id6701:24000
Nakarna silt loam, high precipitation, 15 to 35 percent slopes54q847285099754q8id6701:24000
Nakarna complex, 35 to 65 percent slopes54qb24285099954qbid6701:24000
Nakarna ashy silt loam, 30 to 60 percent slopes50621392859172wdjwa06320121:24000
Nakarna-Nakarna, dry complex, 15 to 30 percent slopes5061316859162wdhwa06320121:24000

Map of Series Extent

Approximate geographic distribution of the NAKARNA 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 .