Official Series Description


Lab Data Summary

Aggregate lab data for the DUPEE soil series. This aggregation is based on all pedons with a current taxon name of DUPEE, 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 DUPEE 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
206N1053S2006OR071013Dupee7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3621407,-123.096138

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the DUPEE 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 DUPEE 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 DUPEE 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 DUPEE 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 flats position figure.

Competing Series

Soil series competing with DUPEE 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 DUPEE 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 DUPEE 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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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with DUPEE, 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. OR-2012-05-10-22 | Yamhill County - January 1974

    Pattern of soils of association 7 on terraces and low foothills of the Coast Range (Soil Survey of Yamhill County, Oregon; January 1974).

Map Units

Map units containing DUPEE 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
Dupee silt loam, 3 to 12 percent slopes612895854142vw9or00320041:24000
Wellsdale-Willakenzie-Dupee complex, 2 to 12 percent slopes1612280610192ngymor00320041:24000
Jory-Dupee complex, 2 to 12 percent slopes97918854232vwlor00320041:24000
Goodin-Dupee-Chehulpum complex, 12 to 20 percent slopes73666610186ngyfor00320041:24000
Wellsdale-Willakenzie-Dupee complex, 12 to 20 percent north slopes162661610193ngynor00320041:24000
Goodin-Dupee-Chehulpum complex, 2 to 12 percent slopes72423610185ngydor00320041:24000
Dupee silt loam, 12 to 20 percent slopes6252853202vs8or00320041:24000
Dupee silt loam, 3 to 12 percent slopes27C47446232622vjor05319771:20000
Dupee silt loam, 12 to 20 percent slopes27D11316232722vkor05319771:20000
Wellsdale-Willakenzie-Dupee complex, 2 to 12 percent slopes2760C19314045861j4l7or05319771:20000
Wellsdale-Willakenzie-Dupee complex, 12 to 20 percent north slopes2760D1314045871j4l8or05319771:20000
Wellsdale-Willakenzie-Dupee complex, 2 to 12 percent slopes2760C188427113611j8c2or07119671:24000
Goodin-Dupee-Chehulpum complex, 2 to 12 percent slopes, eroded2765C108027113921j8c8or07119671:24000
Dupee silt loam, moderately well drained, 2 to 12 percent slopes2772C81327314421j8cnor07119671:24000
Goodin-Dupee-Chehulpum complex, 12 to 20 percent slopes, eroded2765D80327113071j8c9or07119671:24000
Wellsdale-Willakenzie-Dupee complex, 12 to 20 percent north slopes2760D72327114231j8c3or07119671:24000
Dupee silt loam, moderately well drained, 12 to 20 percent slopes2772D52727112661j8cpor07119671:24000
Wellsdale-Dupee complex, 2 to 12 percent slopes2811C51027113122q3ksor07119671:24000
Wellsdale-Dupee complex, hummocky, 2 to 20 percent slopes2810D37427112722p8wfor07119671:24000
Wellsdale-Dupee complex, 12 to 20 percent slopes2811D24727114252q3ktor07119671:24000
Dupee silt loam, somewhat poorly drained, 12 to 20 percent slopes2703D23227113401j8bdor07119671:24000
Dupee silt loam, somewhat poorly drained, 3 to 12 percent slopes2703C22627114161j8bcor07119671:24000
Dupee silt loam, moderately well drained, 20 to 30 percent slopes2772E4827113442p8twor07119671:24000
Dupee silt loam, somewhat poorly drained, 20 to 30 percent slopes2703E1327113981j8bfor07119671:24000
Dupee silt loam, 3 to 20 percent slopes45C22081626822370or63719811:20000
Dupee silt loam, 12 to 20 percent slopes2703D614215291jq6sor63719811:20000
Dupee silt loam, 3 to 20 percent slopes36D41006430224x8or63919831:20000
Oakland-Dupee complex, 12 to 30 percent slopes173E427766474275bor64919941:24000
Dupee silty clay loam, 3 to 12 percent slopes75C38426705127ryor64919941:24000
Dupee silty clay loam, 12 to 30 percent slopes75E34396705227rzor64919941:24000

Map of Series Extent

Approximate geographic distribution of the DUPEE 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 .