Official Series Description


Lab Data Summary

Aggregate lab data for the PILCHUCK soil series. This aggregation is based on all pedons with a current taxon name of PILCHUCK, 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 PILCHUCK 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
206N0235S2005OR071007Pilchuck6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.1336937,-123.0278625

Water Balance

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

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Competing Series

Soil series competing with PILCHUCK 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 PILCHUCK 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 PILCHUCK 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.

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 PILCHUCK, 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 PILCHUCK 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
Pilchuck fine sandy loam, 0 to 3 percent slopes132613852922vrcor00320041:24000
Pilchuck-Urban land complex, 0 to 3 percent slopes33A516461809229vor05119771:20000
Pilchuck sand31154961807229sor05119771:20000
Pilchuck sand, protected3232861808229tor05119771:20000
Pilchuck fine sandy loam581846239222xnor05319771:20000
Pilchuck fine sandy loam, 0 to 3 percent slopes2010A14427113772dglcor07119671:24000
Pilchuck fine sand, 0 to 8 percent slopesPhB1900720522dz8wa01119721:20000
Pilchuck loamy fine sand, 0 to 8 percent slopes1604025722042f45wa01519941:24000
Pilchuck loamy fine sandPc267113894431hmtrwa63319691:24000
Pilchuck fine sandy loamPk43813894441hmtswa63319691:24000
Pilchuck loamy fine sand, 0 to 3 percent slopes1872837739902gzswa63419861:24000
Pilchuck loamy fine sand, 0 to 3 percent slopes187A2115539817s8xwa64119801:24000
Pilchuck gravelly loamy sand, 0 to 3 percent slopesPa426746042hmlwa64519531:31680
Pilchuck loamy sand, 0 to 3 percent slopesPb290746052hmmwa64519531:31680
Pilchuck sand, shallow, 0 to 3 percent slopesPc175746062hmnwa64519531:31680
Pilchuck fine sand29A4886746852hq6wa65319741:24000
Puyallup-Pilchuck complex, 0 to 12 percent slopes30717132420592zl8lwa65319741:24000
Pilchuck loamy sand1047850747322hrqwa65719811:24000
Pilchuck variant fine sandy loam105510747332hrrwa65719811:24000
Pilchuck very fine sandy loam8269913856081hhv1wa65919871:24000
Pilchuck loamy sand507840749372hzbwa66119791:24000
Pilchuck loamy sand84146624546982nd9twa66719831:24000
Pilchuck loamy fine sand, 0 to 3 percent slopes1192465749972j18wa67319831:24000
Puyallup-Pilchuck complex, 0 to 12 percent slopes30712232270642zl8lwa77620211:24000
Pilchuck loamy sand, 0 to 3 percent slopes8477525085062ppldwa77720121:24000

Map of Series Extent

Approximate geographic distribution of the PILCHUCK 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 .