Official Series Description


Lab Data Summary

Aggregate lab data for the PEND OREILLE soil series. This aggregation is based on all pedons with a current taxon name of PEND OREILLE, 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 PEND OREILLE 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
4470C0007S1970ID017003Pend Oreille6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.2227783,-116.6152802

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the PEND OREILLE 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 PEND OREILLE 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 PEND OREILLE 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 PEND OREILLE 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 PEND OREILLE 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 PEND OREILLE 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 PEND OREILLE 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 PEND OREILLE, 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 PEND OREILLE 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
Pend Oreille ashy silt loam, 15 to 35 percent slopes136138981528395419id60120021:24000
Pend Oreille ashy silt loam, 5 to 15 percent slopes13593331528385418id60120021:24000
Pend Oreille ashy silt loam, 35 to 65 percent slopes1378233152840541bid60120021:24000
Pend Oreille-Stien, moist complex, 2 to 8 percent slopes19712161529015439id60120021:24000
Pend Oreille-Rock outcrop complex, 15 to 35 percent slopes138486152841541cid60120021:24000
Pend Oreille silt loam, 5 to 45 percent slopes35842581529915466id60419811:24000
Pend Oreille-Rock outcrop complex, 5 to 45 percent slopes37272851529935468id60419811:24000
Pend Oreille-Hoodoo silt loams, 0 to 30 percent slopes3688721529925467id60419811:24000
Pend Oreille-Highfalls complex, 0 to 6 percent slopes2yxtk128431656352yxtkid60419811:24000
Pend Oreille ashy silt loam, 35 to 65 percent slopes7140645333pnj6id60419811:24000
Pend Oreille silt loam, 5 to 45 percent slopes5466236829366835466id6701:24000
Pend Oreille ashy silt loam, 5 to 15 percent slopes5418178729367115418id6701:24000
Pend Oreille ashy silt loam, 15 to 35 percent slopes5419157829367215419id6701:24000
Pend Oreille-Rock outcrop complex, 5 to 45 percent slopes5468140729366725468id6701:24000
Pend Oreille ashy silt loam, 35 to 65 percent slopes541b12962936765541bid6701:24000
Pend Oreille-Hoodoo silt loams, 0 to 30 percent slopes546787629366975467id6701:24000
Pend Oreille-Stien, moist complex, 2 to 8 percent slopes543979829367145439id6701:24000
Pend Oreille-Rock outcrop complex 15 to 35 percent slopes2x6t929730444862x6t9id6701:24000
Pend Oreille ashy silt loam, 5 to 15 percent slopes13548699224rglmmt63419881:24000
Pend Oreille ashy silt loam, 15 to 35 percent slopes1368699225rglnmt63419881:24000

Map of Series Extent

Approximate geographic distribution of the PEND OREILLE 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 .