Official Series Description


Lab Data Summary

Aggregate lab data for the DOUGVILLE soil series. This aggregation is based on all pedons with a current taxon name of DOUGVILLE, 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 DOUGVILLE 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
887P050187WA017002Dougville6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.7180557,-120.0999985
889P021989WA017016Dougville5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8083344,-119.9083328
890P101490WA017006Dougville7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.8083344,-119.9080582

Water Balance

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

Click the image to view it full size.

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.

Soil series sharing subgroup-level classification with DOUGVILLE, 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-2010-11-05-03 | Douglas County - 2008

    Cross-section view of soils that formed in residuum and colluvium or loess and volcanic ash over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; 2008).

  2. WA-2012-05-11-44 | Douglas County - May 2008

    Cross-section of soils that formed in residuum and colluvium or loess and volcanic ash over older loess over basalt and receive 12 to 15 inches of precipitation (Soil Survey of Douglas County, Washington; May 2008).

Map Units

Map units containing DOUGVILLE 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
Dougville-Norax-Nemire complex, 0 to 25 percent slopes1385417699441rgtmwa01719981:12000
Dougville ashy fine sandy loam, 0 to 8 percent slopes1293153699637rh0ywa01719981:12000
Dougville-Farmer complex, 8 to 15 percent slopes1362089700668rj36wa01719981:12000
Norax-Dutchenry-Dougville complex, 8 to 15 percent slopes2512034700292rhq2wa01719981:12000
Dougville ashy fine sandy loam, cemented substratum, 0 to 8 percent slopes1321874700287rhpxwa01719981:12000
Norax-Dutchenry-Dougville complex, 15 to 30 percent slopes2521812700294rhq4wa01719981:12000
Cheviot-Ralls-Dougville complex, 8 to 15 percent slopes991347699387rgrwwa01719981:12000
Dougville-Farmer-Dutchenry complex, 15 to 30 percent slopes1371012700671rj39wa01719981:12000
Badge-Dougville complex, 8 to 30 percent slopes38856699462rgv9wa01719981:12000
Dougville ashy fine sandy loam, cemented substratum, 8 to 15 percent slopes133761700288rhpywa01719981:12000
Dougville ashy fine sandy loam, 8 to 15 percent slopes130626699638rh0zwa01719981:12000
Norax-Dutchenry-Dougville complex, 3 to 8 percent slopes250532700291rhq1wa01719981:12000
Dougville-Badge complex, 30 to 65 percent slopes135434699458rgv5wa01719981:12000
Beca-Dougville-Slickear complex, 15 to 40 percent slopes52375699243rgm7wa01719981:12000
Dougville ashy fine sandy loam, 15 to 30 percent slopes131152699639rh10wa01719981:12000
Dougville ashy fine sandy loam, cemented substratum, 15 to 30 percent slopes13480700289rhpzwa01719981:12000

Map of Series Extent

Approximate geographic distribution of the DOUGVILLE 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 .