Official Series Description


Lab Data Summary

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

Click the image to view it full size.

Geomorphic description summaries for the SHEEGE 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 hills figure.

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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 SHEEGE, 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-2011-06-01-09 | Bingham Area - 1973

    Representative pattern of soils in association 9 (Soil Survey of Bingham Area, Idaho; 1973).

Map Units

Map units containing SHEEGE 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
Sheege-Pavohroo association, very steep8823037826682s0qid70919761:24000
Rock outcrop-Sheege-Starman association352331194975123fw6id75819981:24000
Fritz, stony-Katpa-Sheege complex, 30 to 70 percent slopes1273856228093432mp6wid75819981:24000
Fritz, stony-Katpa-Sheege complex, 30 to 70 percent slopes12738265624334652mp6wid76120181:24000
Sheege very stony loam, steep, extremely stonySOG9033800222p8cid77019681:24000
Sheege very stony loam, hilly, extremely stonySOF5767800212p8bid77019681:24000
Sheege-Pavohroo association, hillySPF2063800232p8did77019681:24000
Sheege-Robin association, hillySRF1611800242p8fid77019681:24000
Sheege-Robin association, steepSRG1328800252p8gid77019681:24000
Sheege-Skaggs very stony loams, 2 to 15 percent slopes20422423342440chbgmt02719791:24000
Skaggs-Sheege very stony loams, 15 to 60 percent slopes20614579342442chbjmt02719791:24000
Kildor-Sheege complex, 25 to 60 percent slopes1377575342365ch81mt02719791:24000
Sheege-Rock outcrop complex, 15 to 60 percent slopes2037063342439chbfmt02719791:24000
Firada-Sheege-Rock outcrop complex, 25 to 60 percent slopes1026448342327ch6tmt02719791:24000
Skaggs-Sheege complex, 2 to 15 percent slopes2072745342443chbkmt02719791:24000
Kildor-Sheege complex, 25 to 60 percent slopes437F124717156931vl9ymt02719791:24000
Skaggs-Sheege very stony loams, 15 to 60 percent slopes406F29317156891vl9tmt02719791:24000
Hanson-Sheege complex, 15 to 40 percent slopes9218864341981cgvnmt61319751:24000
Hanson-Sheege complex, 4 to 15 percent slopes918796341980cgvmmt61319751:24000
Sheege-Rock outcrop complex, 35 to 70 percent slopes1808774341846cgq9mt61319751:24000
Sheege-Whitore complex, 15 to 40 percent slopes1818630341847cgqbmt61319751:24000
Sheege stony loam, 4 to 15 percent slopes1792504341844cgq7mt61319751:24000
Raynesford-Sheege complex, 4 to 15 percent slopes1602499341824cgplmt61319751:24000
Firada-Sheege-Rock outcrop complex, 25 to 60 percent slopes402F95915316631ndthmt66620081:24000
Skaggs-Sheege very stony loams, 15 to 60 percent slopes406F76115316651ndtkmt66620081:24000
Kildor-Sheege complex, 25 to 60 percent slopes437F69315316731ndttmt66620081:24000
Sheege-Skaggs very stony loams, 2 to 15 percent slopes404D16015316641ndtjmt66620081:24000
Fusulina-Sheege associationFU18038477930j1b3nv62119711:24000
Sheege-Croesus associationSE11872477969j1ccnv62119711:24000
Croesus-Sheege associationCS3582477920j19snv62119711:24000
Hopeka-Sheege associationHS450477937j1bbnv62119711:24000
Sheege-Swapps complex, 30 to 50 percent slopes1301269504360jxtput63619841:24000
Pahreah-Sheege complex, 1 to 20 percent slopes105732504332jxssut63619841:24000
Rock outcrop-Sheege-Starman association *35467315328454hnwy66619781:24000

Map of Series Extent

Approximate geographic distribution of the SHEEGE 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 .