Official Series Description


Lab Data Summary

Aggregate lab data for the BRONSON soil series. This aggregation is based on all pedons with a current taxon name of BRONSON, 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 BRONSON 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
111C94P0314S1993IN039017BRONSON6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6549988,-85.6955566
9893P0411S1993IN039004Bronson6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.6361122,-85.9491653
n/aAL-0321954-OH003-032Bronson3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aGN-0041954-OH057-004Bronson2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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 BRONSON, 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. IN-2010-09-02-06 | Pulaski County - 2003

    Typical pattern of soils and underlying material in the Strole-Rensselaer-Milford association (Soil Survey of Pulaski County, Indiana; 2003).

  2. IN-2010-09-02-07 | Pulaski County - 2003

    Typical pattern of soils and underlying material in the Whitepost-Headlee-Whiskerville association (Soil Survey of Pulaski County, Indiana; 2003).

  3. IN-2010-09-24-02 | Elkhart County -

    Typical pattern of soils and underlying material in the Bristol-Vistula-Bronson association (Soil Survey of Elkhart County, Indiana).

  4. IN-2010-09-24-06 | Elkhart County -

    Typical pattern of soils and underlying material in the Bainter-Bristol-Brady association (Soil Survey of Elkhart County, Indiana).

  5. IN-2010-09-24-07 | Elkhart County -

    Typical pattern of soils and underlying material in the Desker-Matherton association (Soil Survey of Elkhart County, Indiana).

  6. IN-2012-01-19-41 | Pulaski County - January 1968

    Topographical relationships between a few of the major soils in the county (Soil Survey of Pulaski County, Indiana; 1968).

Map Units

Map units containing BRONSON 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
Bronson sandy loam, 0 to 1 percent slopesBufA39751653295k16in03919971:12000
Urban land-Bronson complex, 0 to 1 percent slopesUdrA7801655015k6rin03919971:12000
Bronson sandy loam, 0 to 2 percent slopesBrA43711608565dcxin08519851:20000
Bronson sandy loam, 0 to 3 percent slopesBxA244427259494ncin08719781:20000
Bronson sandy loam, 0 to 1 percent slopesBufA416124819332p9ncin09919781:15840
Urban land-Bronson complex, 0 to 1 percent slopesUdrA824855062pfcmin09919781:15840
Whiskerville-Bronson fine sandy loams, 0 to 1 percent slopesWmgA170018498866hcin13120011:12000
Winamac-Bronson fine sandy loams, 0 to 1 percent slopesWpaA157218498366h6in13120011:12000
Bronson fine sandy loam, 1 to 4 percent slopesBupB19018500166hsin13120011:12000
Bronson sandy loam, 0 to 3 percent slopes21A236918696668k5mi02319841:15840
Bronson sandy loam, 0 to 6 percent slopes14B78601886786bbdmi02519931:15840
Bronson loamy sand, 0 to 3 percent slopes20A240718691868hmmi02719881:15840
Brady-Bronson sandy loams, 0 to 3 percent slopesBrA431218622267s5mi04519741:15840
Bronson sandy loam, 0 to 3 percent slopesBrA96818705768n3mi07719781:15840
Bronson sandy loam, 0 to 3 percent slopesBnA30201884446b2vmi09119571:20000
Bronson sandy loam, 3 to 7 percent slopesBnB13081884456b2wmi09119571:20000
Bronson loamy sand, 0 to 2 percent slopesBwA2878187547694xmi09319681:20000
Bronson sandy loam, 0 to 3 percent slopes20A681818627467tvmi14919801:15840
Bronson sandy loam, 0 to 3 percent slopes24A444718631067w0mi15919841:15840
Bronson sandy loam, 1 to 6 percent slopesBrB10841684315n88oh03919811:15840
Bronson sandy loam, 1 to 6 percent slopesBtB1714140401jgf6oh17119751:15840

Map of Series Extent

Approximate geographic distribution of the BRONSON 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 .