Official Series Description


Lab Data Summary

Aggregate lab data for the BADRIVER soil series. This aggregation is based on all pedons with a current taxon name of BADRIVER, 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 BADRIVER 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
9291P0368S1990WI003001BADRIVER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5288887,-90.8252792
9291P0369S1990WI003002BADRIVER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.457222,-90.8230591
9291P0370S1990WI003003BADRIVER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.6133347,-90.7322235
9291P0371S1990WI003004BADRIVER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.5280571,-90.7330551
9291P0386S1990WI031002BADRIVER6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.7283325,-91.5736084

Water Balance

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

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

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Competing Series

Soil series competing with BADRIVER 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 BADRIVER 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 BADRIVER 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 hills figure.

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

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

Click the image to view it full size.

Soil series sharing subgroup-level classification with BADRIVER, 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. MI-2010-09-10-21 | Ontonagon County -

    Typical pattern of soils and parent material in the Sanborg-Badriver-Carp Lake association (Soil Survey of Ontonagon County, Michigan).

Map Units

Map units containing BADRIVER 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
Badriver-Sanborg complex, 0 to 4 percent slopes8164B1078716748541t6tkmi13120071:24000
Badriver silt loam, 0 to 4 percent slopes8159A361316748491t6tdmi13120071:24000
Normanna, clayey substratum-Badriver, colluvial mantle complex, 3 to 18 percent slopes, very rockyC1071D641227745452t217mn03120131:24000
Badriver, colluvial mantle complex, 0 to 8 percent slopes, very rockyC1070B477227747192t216mn03120131:24000
Sanborg-Badriver complex, 3 to 18 percent slopesC1-41D446127746212rn0lmn03120131:24000
Badriver complex, 0 to 8 percent slopesC1-40B310227745232rn0kmn03120131:24000
Badriver complex, 0 to 3 percent slopesC1-20A262527746792rn0gmn03120131:24000
Palmers, depressional-Badriver complex, 0 to 1 percent slopesC1-10A116227746502rn0fmn03120131:24000
Badriver complex, 0 to 8 percent slopes, very rockyC3-40B96927746692t219mn03120131:24000
Sanborg-Badriver complex, 1 to 18 percent slopes, very rockyC3-41D68127745762t21bmn03120131:24000
Badriver complex, 0 to 3 percent slopes, very rockyC3-20A23927746382t218mn03120131:24000
Badriver-Fluvaquents, frequently flooded complex, 0 to 8 percent slopesE2-20B21227746522t571mn03120131:24000
Badriver-Rock outcrop-Fluvaquents, frequently flooded complex, 0 to 8 percent slopesE1-26B14627747262rn1jmn03120131:24000
Badriver complex, 0 to 3 percent slopesC1-20A330627421532rn0gmn07520131:24000
Badriver complex, 0 to 8 percent slopesC1-40B285927421542rn0kmn07520131:24000
Sanborg-Badriver complex, 3 to 18 percent slopesC1-41D91827421552rn0lmn07520131:24000
Palmers, depressional-Badriver complex, 0 to 1 percent slopesC1-10A85827421522rn0fmn07520131:24000
Sanborg-Badriver complex, 1 to 18 percent slopes, very rockyC3-41D58727421742t21bmn07520131:24000
Badriver complex, 0 to 8 percent slopes, very rockyC3-40B40927421732t219mn07520131:24000
Normanna, clayey substratum-Badriver, colluvial mantle complex, 3 to 18 percent slopes, very rockyC1071D24227421722t217mn07520131:24000
Badriver-Fluvaquents, frequently flooded complex, 0 to 8 percent slopesE2-20B15727421982t571mn07520131:24000
Badriver complex, 0 to 8 percent slopesE15B1216114614817gnjmn61520071:24000
Sanborg-Badriver complex, 3 to 18 percent slopesE22D722114614717gnhmn61520071:24000
Badriver complex, 0 to 3 percent slopesE15A679114614917gnkmn61520071:24000
Sanborg-Badriver complex, 0 to 6 percent slopes580B6986314444491kh24wi00320061:12000
Pickford-Badriver complex, 0 to 3 percent slopes548A2602514444411kh1wwi00320061:12000
Sanborg-Badriver complex, 0 to 6 percent slopes580B31733433663gk84wi00720051:12000
Pickford-Badriver complex, 0 to 3 percent slopes548A2045433629gk71wi00720051:12000
Badriver clay loam, 0 to 3 percent slopes348A77433461gk1mwi00720051:12000

Map of Series Extent

Approximate geographic distribution of the BADRIVER 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 .