Official Series Description


Lab Data Summary

Aggregate lab data for the ROCKWELL soil series. This aggregation is based on all pedons with a current taxon name of ROCKWELL, 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 ROCKWELL 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
5640A174167MN167003Rockwell6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.2016678,-96.4130554
56UMN2421S1977MN0272421Rockwell2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0903625,-96.3208313
56UMN2665S1978MN1132665Rockwell2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.0357628,-96.4586334

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the ROCKWELL 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 ROCKWELL 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 ROCKWELL 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 ROCKWELL 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 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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Competing Series

Soil series competing with ROCKWELL 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 ROCKWELL 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 ROCKWELL 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 ROCKWELL, 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 ROCKWELL 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
Rockwell loam632394397546fbp2mn00519941:20000
Rockwell fine sandy loam, 0 to 1 percent slopesI171A74027980552l6xhmn00719911:24000
Rockwell fine sandy loam439474397632fbrvmn00719911:24000
Rockwell loam, 0 to 1 percent slopesI699A350227981342sw8hmn02719801:20000
Rockwell loam, very poorly drained, 0 to 1 percent slopesI700A24927981352sw8jmn02719801:20000
Rockwell and Kratka soils, 0 to 1 percent slopesI823A427981332sw8gmn02719801:20000
Rockwell loam, 0 to 1 percent slopesI699A113827981722sw8hmn02919931:20000
Rockwell loam, 0 to 1 percent slopesI699A383827982132sw8hmn05119741:20000
Rockwell-Vallers complex, 0 to 1 percent slopesI701A131627982142sw8kmn05119741:20000
Rockwell loam632276399243fdftmn08719921:20000
Rockwell fine sandy loam, 0 to 1 percent slopesI171A7227990032l6xhmn08919941:20000
Rockwell fine sandy loam, 0 to 1 percent slopesI171A1198427990812l6xhmn10719701:20000
Rockwell and Kratka soils, 0 to 1 percent slopesI823A213427991142sw8gmn10719701:20000
Rockwell loam, 0 to 1 percent slopesI699A23627991152sw8hmn10719701:20000
Rockwell loam, 0 to 1 percent slopesI699A357727991592sw8hmn11119961:20000
Rockwell loam63552435880gmknmn11119961:20000
Rockwell fine sandy loam, 0 to 1 percent slopesI171A627997072l6xhmn11919961:20000
Grimstad-Rockwell fine sandy loamsGr10428343gcqjmn14919661:15840
Rockwell loam, 0 to 2 percent slopesJ4A2355434758gldgmn15120001:12000
Rockwell loam, 0 to 1 percent slopesI699A330628004592sw8hmn16719851:20000
Rockwell loam, very poorly drained, 0 to 1 percent slopesI700A18528004602sw8jmn16719851:20000
Rockwell fine sandy loam, 0 to 1 percent slopesI171A157926425752l6xhnd03519801:20000
Rockwell fine sandy loam, 0 to 1 percent slopesI171A75926424852l6xhnd09719741:20000
Rockwell fine sandy loam, 0 to 1 percent slopesI171A336326428862l6xhnd09919671:20000

Map of Series Extent

Approximate geographic distribution of the ROCKWELL 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 .