Official Series Description


Lab Data Summary

Aggregate lab data for the SHARESNOUT soil series. This aggregation is based on all pedons with a current taxon name of SHARESNOUT, 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 SHARESNOUT 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 SHARESNOUT 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 SHARESNOUT 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 SHARESNOUT 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 SHARESNOUT 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 SHARESNOUT 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 SHARESNOUT 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 SHARESNOUT 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 SHARESNOUT, 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 SHARESNOUT 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
Sharesnout-Bregar-Coser complex, 5 to 35 percent slopes15131241485997j9qbid67519921:24000
Snell-Sharesnout complex, 5 to 40 percent slopes15729204486009j9qqid67519921:24000
Sharesnout-Monasterio-Pixley complex, 1 to 20 percent slopes15413430486003j9qjid67519921:24000
Sharesnout-Budlewis complex, 1 to 15 percent slopes15210677485999j9qdid67519921:24000
Thacker-Chen-Sharesnout complex, 2 to 4 percent slopes17488104860492w2swid67519921:24000
Hades-Sharesnout complex, 5 to 35 percent slopes677168486246j9zcid67519921:24000
Bauscher-Sharesnout association, 5 to 35 percent slopes146879485972j9pjid67519921:24000
Sharesnout-Coser-Threek complex, 5 to 35 percent slopes1535862486001j9qgid67519921:24000
Kiyi-Sharesnout-Hades complex, 3 to 40 percent slopes925280486296jb0zid67519921:24000
Sharesnout-Bregar complex, 5 to 35 percent slopes1504253485995j9q8id67519921:24000
Doodlelink-Bregar-Sharesnout complex, 5 to 40 percent slopes483805486204j9y0id67519921:24000
Thacker-Chen-Sharesnout complex, 2 to 4 percent slopes174513929282372w2swnv76420211:24000
Chen-Sharesnout-Keman association3044456630598472w2w3nv76420211:24000
Chen-Sharesnout-Keman association3044173432709012w2w3nv76719861:24000
Thacker-Chen-Sharesnout complex, 2 to 4 percent slopes17432232708962w2swnv76719861:24000
Sharesnout-Rock outcrop complex, 30 to 90 percent slopes44010832708742wz59nv77719931:24000
Sharesnout, south-Sharesnout, north-Mahogee association460117532708822wz5gor62819971:24000
Sharesnout-Rock outcrop complex, 30 to 90 percent slopes440107532708812wz59or62819971:24000
Sharesnout, south-Sharesnout, north-Mahogee association4604224629868532wz5gor64420211:24000
Sharesnout-McIvey-Bullvaro complex, 35 to 60 percent slopes4622455729868552wz5jor64420211:24000
Sharesnout-Rock outcrop complex, 30 to 90 percent slopes4401440829868482wz59or64420211:24000
Sharesnout-Erakatak complex, 30 to 60 percent slopes4571276629868642wbkwor64420211:24000
Sharesnout-Perla complex, 15 to 50 percent slopes269142222190332dh2qor64420211:24000
Sharesnout-Bregar complex, 5 to 35 percent slopesID015037624872272ph54or64420211:24000
Sharesnout-Erakatak gravelly ashy loams, 15 to 50 percent slopes27234822190942dh4por64420211:24000

Map of Series Extent

Approximate geographic distribution of the SHARESNOUT 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 .