Official Series Description


Lab Data Summary

Aggregate lab data for the DESCHUTES soil series. This aggregation is based on all pedons with a current taxon name of DESCHUTES, 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 DESCHUTES 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
1087P051087OR017001Deschutes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2000008,-121.3666687
1087P051187OR017002Deschutes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2358322,-121.2616653
1087P051287OR017003Deschutes6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.3666649,-121.1666641

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DESCHUTES 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 DESCHUTES 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 DESCHUTES 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 DESCHUTES 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.

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Competing Series

Soil series competing with DESCHUTES 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 DESCHUTES 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 DESCHUTES 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 mountains figure.

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Soil series sharing subgroup-level classification with DESCHUTES, 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 DESCHUTES 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
Stukel-Rock outcrop-Deschutes complex, dry, 0 to 8 percent slopes142Bm923734375772mnvor6181:24000
Stukel-Deschutes complex, dry, 0 to 8 percent slopes140Bm909134375782mntor6181:24000
Deschutes-Stukel complex, dry, 0 to 8 percent slopes35Bm310934349672mn1or6181:24000
Deschutes ashy sandy loam, 0 to 3 percent slopes18729913434972wg1mor6181:24000
Deschutes-Stukel complex, 0 to 8 percent slopes18625093437432wg1lor6181:24000
Stukel-Deschutes-Rock outcrop complex, 0 to 8 percent slopes18524903437433wg1kor6181:24000
Deschutes ashy sandy loam, dry, 0 to 3 percent slopes32Am189234375572mn0or6181:24000
Stukel-Deschutes complex, 0 to 8 percent slopes18813953437466wg1nor6181:24000
Stukel-Rock outcrop-Deschutes complex, dry, 0 to 8 percent slopes142B2939563473241jor62019921:24000
Deschutes-Stukel complex, 0 to 15 percent slopes34C2857963633246por62019921:24000
Stukel-Deschutes-Rock outcrop complex, 0 to 15 percent slopes141C2004663472241hor62019921:24000
Deschutes-Stukel complex, dry, 0 to 8 percent slope35B1368263640246xor62019921:24000
Deschutes sandy loam, 0 to 3 percent slopes31A5870636162464or62019921:24000
Deschutes sandy loam, dry, 0 to 3 percent slopes32A546763628246jor62019921:24000
Statz-Deschutes complex, 0 to 15 percent slopes128C311463439240for62019921:24000
Deschutes sandy loam, 3 to 8 percent slopes31B2077636172465or62019921:24000
Stukel-Deschutes complex, dry, 0 to 8 percent slopes140B174863471241gor62019921:24000
Redmond-Deschutes-Stukel complex, 0 to 15 percent slopes105C9516338523ypor62019921:24000
Lickskillet-Deschutes complex, 0 to 15 percent slopes78C9356386124g1or62019921:24000
Deschutes-Houstake complex, 0 to 8 percent slopes33B79363631246mor62019921:24000
Statz-Deschutes complex, 15 to 30 percent slopes128D54863440240gor62019921:24000

Map of Series Extent

Approximate geographic distribution of the DESCHUTES 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 .