Official Series Description


Lab Data Summary

Aggregate lab data for the DOUDS soil series. This aggregation is based on all pedons with a current taxon name of DOUDS, 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 DOUDS 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
10992P0593S1992IA177001Douds7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.896946,-91.7763901

Water Balance

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

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Competing Series

Soil series competing with DOUDS 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 DOUDS 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 DOUDS 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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Click the image to view it full size.

Soil series sharing subgroup-level classification with DOUDS, 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. IA-2011-06-01-08 | Louisa County - 1980

    Pattern of soils and parent material in the Downs-Fayette association (Soil Survey of Louisa County, Iowa; 1980).

Map Units

Map units containing DOUDS 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
Douds-Galland loams, 14 to 18 percent slopes, moderately eroded994E21644404751fl5hia05119881:15840
Douds loam, heavy loess, 9 to 14 percent slopes, moderately eroded58D22324047192wjg8ia05119881:15840
Douds-Galland complex, 9 to 18 percent slopes, moderately eroded994E23004404855fl8via05319861:15840
Douds loam, heavy loess, 14 to 18 percent slopes, moderately eroded58E29224048282wjg7ia05319861:15840
Douds-Galland loams, 9 to 18 percent slopes994E731404854fl8tia05319861:15840
Douds loam, heavy loess, 14 to 18 percent slopes58E3434048272wjg9ia05319861:15840
Douds loam, 14 to 18 percent slopes58E363405268flq5ia05719801:15840
Douds loam, 18 to 40 percent slopes58F524406878fnd3ia08719821:15840
Douds loam, heavy loess, 14 to 18 percent slopes58E2644068772wjg9ia08719821:15840
Galland-Douds complex, 14 to 18 percent slopes, moderately erode994E2875407920fpgqia10119921:15840
Galland-Douds loams, heavy loess, 9 to 14 percent slopes, moderately erodedS994D253929834422wjfmia10119921:15840
Galland-Douds complex, 9 to 14 percent slopes, moderately eroded994D2221407919fpgpia10119921:15840
Galland-Douds complex, 9 to 14 percent slopes, moderately eroded994D2283447258h0dpia10719981:12000
Galland-Douds complex, 14 to 18 percent slopes, moderately eroded994E290447259h0dqia10719981:12000
Douds loam, heavy loess, 14 to 18 percent slopes, moderately eroded58E230414084852wjg7ia11119761:15840
Douds-Alvin-Tell Complex, 18 to 60 percent slopesS154G1803408432fq07ia11119761:15840
Douds loam, heavy loess, 9 to 14 percent slopes, moderately eroded58D211674084842wjg8ia11119761:15840
Douds-Lindley loams, 25 to 40 percent slopes1058G2786408704fq90ia11519841:15840
Douds-Lindley loams, 18 to 25 percent slopes1058F480408703fq8zia11519841:15840
Douds-Lindley loams, 14 to 18 percent slopes1058E290408702fq8yia11519841:15840
Douds loam, heavy loess, 9 to 14 percent slopes, moderately eroded58D219414097992wjg8ia13519821:15840
Douds loam, heavy loess, 14 to 18 percent slopes, moderately eroded58E217184098002wjg7ia13519821:15840
Lindley-Douds-Orwood silt loams, 18 to 40 percent slopes680G3812410021frnhia13919861:15840
Galland-Douds loams, heavy loess, 9 to 14 percent slopes, moderately eroded994D215064131972wjfmia17719941:12000
Galland-Douds complex, 14 to 18 percent slopes, moderately eroded994E21413413198fvyzia17719941:12000
Douds loam, heavy loess, 9 to 14 percent slopes, moderately eroded58D210424131292wjg8ia17719941:12000
Douds loam, heavy loess, 14 to 18 percent slopes, moderately eroded58E210144131302wjg7ia17719941:12000
Douds loam, 25 to 40 percent slopes58G942413132fvwvia17719941:12000
Douds loam, 18 to 25 percent slopes, moderately eroded58F2202413131fvwtia17719941:12000
Douds loam, 9 to 14 percent slopes58D12413128fvwqia17719941:12000
Douds loam, heavy loess, 14 to 18 percent slopes, moderately eroded58E26534118262wjg7ia17919781:15840
Douds soils, 18 to 40 percent slopes58G367411827ftjria17919781:15840
Douds loam, 9 to 14 percent slopes, moderately eroded58D2360411824ftjnia17919781:15840
Douds loam, heavy loess, 14 to 18 percent slopes58E3574118252wjg9ia17919781:15840
Galland-Douds clay loams, 9 to 14 percent slopes, severely eroded994D3446412125ftvcia18319831:15840
Douds loam, 9 to 14 percent slopes, moderately eroded58D2237412076ftssia18319831:15840
Douds loam, 14 to 18 percent slopes, moderately eroded58E2164412077ftstia18319831:15840

Map of Series Extent

Approximate geographic distribution of the DOUDS 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 .