Official Series Description


Lab Data Summary

Aggregate lab data for the MUSHEL soil series. This aggregation is based on all pedons with a current taxon name of MUSHEL, 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 MUSHEL 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
43A75-ID-256775ID049002Mushel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.3797493,-115.5494461
43A78-ID-2912178ID057003Mushel3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9802704,-116.3384094
43A70C0006S1970ID049002Mushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2935583,-115.6635694
43A16N1897S2016ID057001AMushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9251389,-116.3682222
43A16N1898S2016ID057001BMushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9251389,-116.3682222
43A16N1899S2016ID057001CMushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9251389,-116.3682222
43A16N1900S2016ID057001DMushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9251389,-116.3682222
43A16N1901S2016ID057001EMushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9251389,-116.3682222
43A16N1902S2016ID057001FMushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9251389,-116.3682222
43A16N1903S2016ID057001GMushel6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.9251389,-116.3682222

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the MUSHEL 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 MUSHEL 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 MUSHEL 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 MUSHEL 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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Click the image to view it full size.

Click the image to view it full size.

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 MUSHEL 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 MUSHEL 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 MUSHEL 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 MUSHEL, 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 MUSHEL 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
Jacot, warm-Mushel complex, 35 to 70 percent slopesJm26942644910pn2kid05720131:24000
Jacot-Mushel complex, 35 to 70 percent slopesJm13036644908pn2hid05720131:24000
Brequito-Mushel-Brodeer complex, 5 to 35 percent slopesBr21537579785mg9rid05720131:24000
Brodeer, moist-Brequito-Mushel complex, 10 to 40 percent slopesMb61320645277pngdid05720131:24000
Lado-Brequito-Mushel complex, 30 to 60 percent slopesBa1942813997wb0zid05720131:24000
Brodeer, cool, moist-Mushel complex, 25 to 60 percent slopesMb7628645278pngfid05720131:24000
Brodeer-Mushel complex, 35 to 75 percent slopesBr5j2152501171v125id05720131:24000
Brequito-Mushel complex, 15 to 35 percent slopesBr2j1952501169v123id05720131:24000
Brodeer, dry-Mushel complex, 35 to 60 percent slopesMb4j1362501978v2wlid05720131:24000
Brodeer, dry-Mushel complex, 35 to 60 percent slopesMb4192663019v2wlid60819941:24000
Brodeer, moist-Brequito-Mushel complex, 10 to 40 percent slopesMb6182663024pngdid60819941:24000
Brodeer-Mushel complex, 35 to 75 percent slopes4232755775594v125id61220031:24000
Brodeer, dry-Mushel complex, 35 to 60 percent slopes4118613777343v2wlid61220031:24000
Mushel-Dullaxe complex, 35 to 70 percent slopes17013728776633v24pid61220031:24000
Brequito-Mushel complex, 15 to 35 percent slopes324264775592v123id61220031:24000
Mushel-Brodeer complex, 15 to 35 percent slopes1694163777340v2whid61220031:24000
Brequito-Mushel complex, 35 to 75 percent slopes333087775593v124id61220031:24000
Brodeer-Mushel complex, 15 to 35 percent slopes352919777342v2wkid61220031:24000
Brodeer, warm-Mushel, dry complex, 15 to 35 percent slopes361328777341v2wjid61220031:24000
Brodeer, dry-Mushel complex, 35 to 60 percent slopes412363002656v2wlid67119891:24000
Brodeer-Mushel complex, 35 to 75 percent slopes42143002655v125id67119891:24000

Map of Series Extent

Approximate geographic distribution of the MUSHEL 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 .