Official Series Description


Lab Data Summary

Aggregate lab data for the REDBY soil series. This aggregation is based on all pedons with a current taxon name of REDBY, 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 REDBY were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
56UMN1197S1970MN0691197Redby3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7627792,-96.492981
56UMN1518S1972MN0691518Redby2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties48.7454987,-96.5663147

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the REDBY series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the REDBY series and siblings. 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 REDBY 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with REDBY share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the REDBY 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 REDBY 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 .

Click the image to view it full size.

Click the image to view it full size.

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with REDBY, 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. MN-2010-09-10-07 | Roseau County -

    Pattern of soils and underlying material in the Redby-Hiwood-Cormant association (Soil Survey of Roseau County, Minnesota).

Map Units

Map units containing REDBY 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
Redby loamy fine sand, stratified substratum7951903432967gjjpmn00119961:20000
Redby loamy fine sand, 0 to 3 percent slopes116243453975902x14nmn00719911:24000
Cormant-Redby complex, 0 to 2 percent slopes1206146826036602qkjxmn00719911:24000
Redby loamy fine sand, dense till, 0 to 2 percent slopesI90A802798052307d8mn00719911:24000
Guida-Zimmerman-Redby complex, 0 to 8 percent slopesB253B2480231151412z32lmn02119931:20000
Redby-Deford-Hiwood complex, 0 to 3 percent slopesB252A1144131151422z32mmn02119931:20000
Redby loamy fine sand, 0 to 3 percent slopes116107218573422x14nmn02119931:20000
Guida-Zimmerman-Redby complex, 0 to 8 percent slopesB253B2054831151442z32lmn06119821:24000
Redby-Deford-Hiwood complex, 0 to 3 percent slopesB252A1007831151452z32mmn06119821:24000
Redby loamy fine sand, 0 to 3 percent slopes116518831846392x14nmn06119821:24000
Redby loamy fine sand, dense till, 0 to 2 percent slopesI90A165542798837307d8mn06920071:12000
Redby loamy fine sand, 0 to 3 percent slopes116300283988572x14nmn07719891:24000
Redby loamy fine sand, 0 to 3 percent slopes11633383571012x14nmn08919941:20000
Redby loamy fine sand, dense till, 0 to 2 percent slopesI90A11812798969307d8mn08919941:20000
Redby loamy fine sand, 0 to 3 percent slopes116208603947822x14nmn13519991:24000
Redby-Hiwood-Leafriver complex, 0 to 6 percent slopes1274B16072394798f7tfmn13519991:24000
Cormant-Redby complex, 0 to 2 percent slopes120614926394794f7t9mn13519991:24000
Redby loamy fine sand, dense till, 0 to 2 percent slopesI90A38762799853307d8mn13519991:24000
Soderville-Redby complex, 0 to 3 percent slopesB248A196029437942dv53mn62520151:24000
Redby-Cormant complex, 0 to 3 percent slopesB250A96229437962dv55mn62520151:24000

Map of Series Extent

Approximate geographic distribution of the REDBY 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 .