Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

Monthly water balance estimated using a leaky-bucket style model for the NUSS 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 NUSS 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 NUSS 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 NUSS 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 NUSS 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 NUSS 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 NUSS 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 flats position figure.

Soil series sharing subgroup-level classification with NUSS, 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 NUSS 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
Booth-Nuss complex, 30 to 50 percent north slopes18For1199189941021rh9ca70319831:24000
Booth-Nuss-Royst association, 40 to 60 percent south slopes24Gor43189942021rhmca70319831:24000
Nuss-Rock outcrop complex, 20 to 40 percent south slopes2395278490633jgjwor62819971:24000
Nuss stony loam, 20 to 40 percent south slopes2372906490631jgjtor62819971:24000
Rubble land-Nuss-Ateron association, 20 to 60 percent slopes2942425490711jgmdor62819971:24000
Nuss-Merlin complex, 20 to 40 percent north slopes2381911490632jgjvor62819971:24000
Bullump-Rock outcrop-Nuss complex, 20 to 70 percent south slopes23489916897451tq9xor63520061:24000
Dunres-Moonbeam-Nuss complex, 1 to 20 percent slopes28365116897921tqcfor63520061:24000
Dunres-Murlose-Nuss complex, 1 to 20 percent slopes28458616897931tqcgor63520061:24000
Royst-Nuss complex, 2 to 30 percent slopes56836316900681tqnbor63520061:24000
Booth-Nuss-Royst association, 15 to 40 percent south slopes24E14025489109jdyqor63619911:24000
Booth-Nuss-Royst association, 0 to 15 percent slopes23C7516489097jdybor63619911:24000
Booth-Nuss-Royst association, 40 to 60 percent south slopes24G5903489110jdyror63619911:24000
Mound-Royst-Nuss association, 15 to 40 percent slopes171E5531488993jdtzor63619911:24000
Royst-Nuss-Rock outcrop complex, 30 to 50 percent north slopes239F5398489095jdy8or63619911:24000
Mound-Royst-Nuss association, 40 to 60 percent slopes171G4580488994jdv0or63619911:24000
Royst-Nuss-Rock outcrop complex, 30 to 50 percent south slopes240F4250489098jdycor63619911:24000
Booth-Nuss complex, 5 to 30 percent slopes17E3404489003jdv9or63619911:24000
Bullump-Rock outcrop-Nuss complex, 20 to 70 percent south slopes36G2952489203jf1ror63619911:24000
Nuss gravelly loam, 0 to 5 percent slopes, eroded183B2896489008jdvgor63619911:24000
Royst-Nuss complex, 2 to 30 percent slopes238E1885489094jdy7or63619911:24000
Bullump-Nuss-Rock outcrop complex, 30 to 70 percent north slopes34G1789489198jf1lor63619911:24000
Bullump-Nuss-Rock outcrop complex, 30 to 50 percent south slopes35F1521489201jf1por63619911:24000
Booth-Nuss complex, 30 to 50 percent north slopes18F1199489022jdvxor63619911:24000
Booth-Nuss complex, 30 to 50 percent south slopes19F417489037jdwdor63619911:24000
Nuss-Royst association, gently sloping59B31843488804jdmwor64019771:20000
Rock outcrop-Nuss complex, 5 to 40 percent slopes67E17202488812jdn4or64019771:20000

Map of Series Extent

Approximate geographic distribution of the NUSS 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 .