Official Series Description


Lab Data Summary

Aggregate lab data for the SCOOTENEY soil series. This aggregation is based on all pedons with a current taxon name of SCOOTENEY, 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 SCOOTENEY 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 SCOOTENEY 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 SCOOTENEY 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 SCOOTENEY 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 SCOOTENEY 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 .

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.

Competing Series

Soil series competing with SCOOTENEY 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 SCOOTENEY 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 SCOOTENEY 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with SCOOTENEY, 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. WA-2012-05-11-15 | Benton County Area - July 1971

    Cross section of Benton County, showing the relationship of elevation, precipitation, and major soil series (Soil Survey of Benton County Area, Washington; April 1980).

Map Units

Map units containing SCOOTENEY 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
Scooteney loam, 0 to 2 percent slopesSmA704368256290twa00119651:20000
Scooteney stony loam, 0 to 15 percent slopesSoD632968261290zwa00119651:20000
Scooteney loam, 2 to 5 percent slopesSmB291768257290vwa00119651:20000
Scooteney loam, 10 to 15 percent slopesSmD112768259290xwa00119651:20000
Scooteney cobbly loam, 0 to 5 percent slopesSnB80368260290ywa00119651:20000
Scooteney loam, 5 to 10 percent slopesSmC64168258290wwa00119651:20000
Scooteney silt loam, gravelly subsoil, 0 to 2 percent slopesSdA6663695812bdkwa60519651:20000
Scooteney silt loam, gravelly subsoil, 2 to 5 percent slopesSdB4023695822bdlwa60519651:20000
Scooteney silt loam, 0 to 5 percent slopesScAB2348695782bdgwa60519651:20000
Scootney silt loam, 2 to 5 percent slopesScB1941695792bdhwa60519651:20000
Scooteney silt loam, gravelly subsoil, 5 to 15 percent slopesSdD1420695832bdmwa60519651:20000
Scooteney silt loam, 0 to 2 percent slopesScA1322695772bdfwa60519651:20000
Scooteney stony silt loam, 0 to 30 percent slopesSeE585695842bdnwa60519651:20000
Scooteney silt loam, 5 to 8 percent slopesScC340695802bdjwa60519651:20000
Scooteney gravelly silt loam, 2 to 5 percent slopesSgB293695852bdpwa60519651:20000
Scooteney silt loam, 2 to 5 percent slopes12510766142kqfwa63920031:24000
Scooteney cobbly silt loam, 0 to 5 percent slopes1271766132kqdwa63920031:24000
Scooteney silt loam, 0 to 2 percent slopes12415536890829pvwa67719791:24000
Scooteney cobbly silt loam, 0 to 5 percent slopes12711776891129pywa67719791:24000
Scooteney silt loam, 2 to 5 percent slopes12511426890929pwwa67719791:24000
Scooteney silt loam, 5 to 15 percent slopes1262326891029pxwa67719791:24000

Map of Series Extent

Approximate geographic distribution of the SCOOTENEY 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 .