Official Series Description


Lab Data Summary

Aggregate lab data for the ROSSBURG soil series. This aggregation is based on all pedons with a current taxon name of ROSSBURG, 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 ROSSBURG 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
108A85IL1830271985IL183027Rossburg2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0790972,-87.5766139
n/a92P0246S1991OH131104Rossburg6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

There are insufficient data to create the 3D terrace figure.

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Soil series sharing subgroup-level classification with ROSSBURG, 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 ROSSBURG 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
Rossburg silt loam, 0 to 2 percent slopes, frequently flooded3473A98224299584vkil01919991:12000
Rossburg loam, 0 to 2 percent slopes, occasionally flooded8473A112616132061r4nxil18320061:12000
Rossburg silt loam, 0 to 2 percent slopes, frequently flooded3473A516133461r4tfil18320061:12000
Rossburg silt loam, 0 to 2 percent slopes, frequently flooded, brief durationRtxAH61942073156yqlin00520021:12000
Rossburg silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationRtxAK232073146yqkin00520021:12000
Rossburg and Landes soils, 0 to 2 percent slopes, frequently flooded, brief durationRtuAH2687697272rdknin01120031:12000
Rossburg silt loam, 0 to 2 percent slopes, occasionally flooded, brief durationRtxAK1151242433848fin04519991:12000
Rossburg silt loam, 0 to 2 percent slopes, frequently flooded, brief durationRtxAH472620337nthwin07119851:15840
Rossburg silt loam, moderately wet, sandy substratum, 0 to 1 percent slopes, occasionally floodedRoA9815899781qchmoh01719771:15840
Rossburg silt loam, 0 to 2 percent slopes, rarely floodedRsA2631720115rzroh02719991:12000
Rossburg silt loam, 0 to 2 percent slopes, occasionally floodedRoA14641720825s21oh04119971:12000
Rossburg-Sloan complex, 0 to 2 percent slopes, occasionally floodedRsA6211720835s22oh04119971:12000
Rossburg silt loam, occasionally floodedRt2281723035s95oh04519981:12000
Rossburg silt loam, 0 to 2 percent slopes, occasionally floodedRtA917644447pmlmoh06319971:12000
Rossburg silt loam, 0 to 2 percent slopes, occasionally floodedRo414004581j092oh10119841:15840
Rossburg silt loam, moderately wet, sandy substratum, 0 to 1 percent slopes, occasionally floodedRpA115901191qcn5oh11319691:15840
Rossburg silt loam, occasionally floodedRt111124459986j9oh12519931:12000
Rossburg silt loam, moderately wet, sandy substratum, 0 to 1 percent slopes, occasionally floodedRpA529521086872f6oh13520051:12000
Rossburg silt loam, occasionally floodedRw3315291631nb6voh13719711:20000
Rossburg silt loam, rarely floodedRo28561709525qwloh14119971:15840
Rossburg silt loam, occasionally floodedRs23621695795pg9oh14319831:15840
Rossburg silty clay loam, occasionally floodedRo550537294l132oh14519841:15840
Rossburg silt loam, occasionally floodedRw9015921931qft2oh14719781:15840
Rossburg-Sloan complex, 0 to 2 percent slopes, occasionally floodedRrA2114061201j65qoh15919701:15840
Rossburg silt loam, 0 to 2 percent slopes, occasionally floodedRpA214061191j65poh15919701:15840
Rossburg silt loam, 0 to 2 percent slopes, frequently floodedRsA391683295n4zoh17320001:12000

Map of Series Extent

Approximate geographic distribution of the ROSSBURG 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 .