Official Series Description


Lab Data Summary

Aggregate lab data for the YANUSH soil series. This aggregation is based on all pedons with a current taxon name of YANUSH, 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 YANUSH 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 YANUSH 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 YANUSH 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 YANUSH 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 YANUSH 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 YANUSH 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 YANUSH series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the YANUSH 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 .

There are insufficient data to create the 2D hillslope position figure.

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 YANUSH, 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 YANUSH 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
Yanush-Carnasaw-Bigfork complex, 8 to 20 percent slopes943043179433lyq0ar01919831:20000
Yanush-Ceda complex, 0 to 8 percent slopes931913179432lypzar01919831:20000
Yanush-Bigfork-Carnasaw complex, 20 to 40 percent slopes951593179434lyq1ar01919831:20000
Yanush-Avant complex, 40 to 60 percent slopes3929657565625lzkzar05119861:20000
Bigfork-Yanush-Carnasaw complex, 40 to 60 percent slopes79648565629lzl3ar05119861:20000
Yanush-Avant complex, 20 to 40 percent slopes388907565624lzkyar05119861:20000
Bigfork-Yanush-Carnasaw complex, 20 to 40 percent slopes63576565628lzl2ar05119861:20000
Yanush very gravelly silt loam, 3 to 12 percent slopes373162565623lzkxar05119861:20000
Yanush-Carnasaw-Bigfork complex, 8 to 20 percent slopes94169203179323lyq0ar05919831:20000
Yanush-Bigfork-Carnasaw complex, 20 to 40 percent slopes95126673179324lyq1ar05919831:20000
Yanush-Ceda complex, 0 to 8 percent slopes9353023179322lypzar05919831:20000
Yanush-Avant-Bengal complex, 35 to 60 percent slopes57G27798577501mcy2ar09719971:24000
Bengal-Bismarck-Yanush complex, 15 to 35 percent slopes, extremely stony6F229055774722y1mtar09719971:24000
Yanush-Bigfork complex, 35 to 60 percent slopes, moderately eroded, very rocky, very rubbly58G144335775022y1ngar09719971:24000
Bigfork-Yanush-Rock outcrop complex, 35 to 60 percent slopes, moderately eroded, very rubbly8G121165775092zmfbar09719971:24000
Bengal-Bismarck-Yanush complex, 8 to 15 percent slopes5D92205774762y1mrar09719971:24000
Yanush-Avant-Bengal complex, 15 to 35 percent slopes57F6759577515mcyjar09719971:24000
Yanush-Bigfork complex, 15 to 35 percent slopes, moderately eroded, very rubbly58F52115775002zmfcar09719971:24000
Yanush gravelly silt loam, 1 to 8 percent slopes56C34345774982zphhar09719971:24000
Yanush gravelly silt loam, 8 to 15 percent slopes56D1897577499mcy0ar09719971:24000
Bigfork-Yanush-Rock outcrop complex, 35 to 60 percent slopes, rubbly9406515429031nsj2ar10920051:20000
Yanush-Bigfork complex, 35 to 60 percent slopes, moderately eroded, very rocky, very rubbly100359215428942y1ngar10920051:20000
Bengal-Bismarck-Yanush complex, 15 to 35 percent slopes, extremely stony6265815428692y1mtar10920051:20000
Yanush very gravelly silt loam, 1 to 8 percent slopes95116415428901nshnar10920051:20000
Bengal-Bismarck-Yanush complex, 8 to 15 percent slopes544415428722y1mrar10920051:20000
Yanush very gravelly silt loam, 8 to 15 percent slopes9635415428911nshpar10920051:20000
Yanush-Avant-Bengal complex, 35 to 60 percent slopes9835415428931nshrar10920051:20000
Yanush-Bigfork complex, 15 to 35 percent slopes, extremely stony9927315428921nshqar10920051:20000
Yanush-Avant-Bengal complex, 15 to 35 percent slopes9710915429061nsj5ar10920051:20000
Bengal-Bismarck-Yanush complex, 15 to 35 percent slopes4F251885708472y1mkar11319911:20000
Yanush-Bigfork complex, 35 to 60 percent slopes, moderately eroded, very rocky, very rubbly41G243825708792y1ngar11319911:20000
Bigfork-Yanush-Rock outcrop complex, 35 to 60 percent slopes, moderately eroded, very rubbly6G108105708892zmfbar11319911:20000
Yanush-Avant complex, 35 to 60 percent slopes40G7494570878m51far11319911:20000
Bengal-Bismarck-Yanush complex, 8 to 15 percent slopes4D58025708512y1mrar11319911:20000
Yanush gravelly silt loam, 1 to 8 percent slopes39C22415708752zphhar11319911:20000
Yanush-Bigfork complex, 15 to 35 percent slopes, moderately eroded, very rubbly41F22095708772zmfcar11319911:20000
Yanush gravelly silt loam, 8 to 15 percent slopes39D997570876m51car11319911:20000
Bigfork-Yanush association, 20 to 45 percent slopes, rocky1314535713252zmf9ok00519771:24000
Yanush gravelly silt loam, 12 to 25 percent slopes69668571386m5ktok00519771:24000
Bigfork-Yanush association, 20 to 45 percent slopes, rocky372225714992zmf9ok07719801:24000
Yanush-Sobol complex, 5 to 20 percent slopes514964571523m5q7ok07719801:24000
Yanush gravelly silt loam, 5 to 20 percent slopes5036895715222zmf8ok07719801:24000
Yanush gravelly silt loam, 3 to 8 percent slopes4919795715202zmf7ok07719801:24000
Yanush gravelly silt loam, 1 to 3 percent slopes4814525715192zphgok07719801:24000
Bigfork-Yanush association, 20 to 45 percent slopes, rocky7126195713182zmf9ok12719771:24000
Yanush gravelly silt loam, 5 to 20 percent slopes6242985713172zmf8ok12719771:24000
Yanush gravelly silt loam, 3 to 8 percent slopes6121585713162zmf7ok12719771:24000
Yanush gravelly silt loam, 1 to 3 percent slopes6010905713152zphgok12719771:24000

Map of Series Extent

Approximate geographic distribution of the YANUSH 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 .