Official Series Description


Lab Data Summary

Aggregate lab data for the BRYCE soil series. This aggregation is based on all pedons with a current taxon name of BRYCE, 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 BRYCE 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
11040IL0750021940IL075002Bryce4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5169519,-87.877205
11076IL0190071976IL019007Bryce1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3988083,-87.9552056
110BE80471980IN007047Bryce3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6786,-87.5269611
11040A278577IL075004aBryce7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.5022492,-88.0297516
11082P021580IL075001aBryce5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8022462,-87.6358498
11040A2781S1977IL075006Bryce7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6438889,-87.8730556
n/a40IL0750051940IL075005Bryce3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

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

Click the image to view it full size.

Competing Series

Soil series competing with BRYCE 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 BRYCE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BRYCE 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.

There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BRYCE, 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. IL-2010-09-01-37 | Livingston County - 1996

    Typical pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Livingston County, Illinois; 1996).

  2. IL-2011-08-04-10 | Ford County - 1990

    Typical pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Ford County, Illinois; 1990).

  3. IL-2011-08-04-39 | Kankakee County - 1991

    Typical pattern of soils in Bryce-Mokena-Frankfort association (Soil Survey of Kankakee County, Illinois; 1991).

  4. IL-2011-08-04-50 | Livingston County - 1996

    Typical pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Livingston County, Illinois; 1996).

  5. IN-2012-01-19-03 | Benton County - 1989

    Pattern of soils and parent material in the Bryce-Swygert association (Soil Survey of Benton County, Indiana; 1989).

Map Units

Map units containing BRYCE 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
Bryce silty clay, 0 to 2 percent slopes235A16212429792t6zpil01919991:12000
Bryce silty clay, 0 to 2 percent slopes235A428021087322t6zpil03120081:12000
Frankfort-Bryce complex, 1 to 6 percent slopes925B346923945292lcpwil03120081:12000
Bryce silty clay, 0 to 2 percent slopes235A455731983432t6zpil05320011:12000
Bryce silty clay, 0 to 2 percent slopes235A509911440062t6zpil06320051:12000
Bryce, shale substratum-Calamine silty clays, 0 to 2 percent slopes553A405815902881qctmil06320051:12000
Bryce silty clay, 0 to 2 percent slopes235A986071755652t6zpil07519801:15840
Bryce silty clay, 0 to 2 percent slopes235A24169804502t6zpil09120031:12000
Bryce silty clay, 0 to 2 percent slopes235A89206387682t6zpil09320071:12000
Bryce silty clay, 0 to 2 percent slopes235A1420610299242t6zpil09920061:12000
Bryce silty clay, 0 to 2 percent slopes235A803871769472t6zpil10519911:15840
Bryce silty clay, 0 to 2 percent slopes235A1446016131802t6zpil18320061:12000
Bryce silty clay, 0 to 2 percent slopes235A84292623292t6zpil19720021:12000
Bryce silty clay, 0 to 2 percent slopesBt15711645352t6zpin00719851:15840
Bryce silty clay, 0 to 2 percent slopesBy12471635202t6zpin11119901:15840

Map of Series Extent

Approximate geographic distribution of the BRYCE 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 .