Official Series Description


Lab Data Summary

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

There are insufficient data to create the lab data summary figure.


Water Balance

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

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Competing Series

Soil series competing with BEADLE 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 BEADLE 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 BEADLE 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 BEADLE, 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. SD-2012-03-15-57 | Jerauld County - September 1994

    Pattern of soils and parent material in the Homme-Peno association (Soil Survey of Jerauld County, SD; 1994).

  2. SD-2012-03-15-68 | Lake County - December 1973

    Relationship of soils to topography and the underlying materials in the Egan-Wentworth association (Soil Survey of Lake County, SD; 1973).

Map Units

Map units containing BEADLE 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
Beadle-Jerauld-Dudley complex, 0 to 6 percent slopesBgB1352533336992yyg6sd00319791:20000
Beadle-Dudley complex, 0 to 2 percent slopesBdA40063548282yyg0sd00319791:20000
Beadle-Stickney complex, 1 to 6 percent slopesBaB7723548272yyg3sd00319791:20000
Beadle-Dudley complex, 0 to 2 percent slopesBdA547353545492yyg0sd00519761:20000
Beadle-Stickney complex, 1 to 6 percent slopesBaB202993545472yyg3sd00519761:20000
Beadle-Stickney complex, 0 to 2 percent slopesBaA147423545462yyg2sd00519761:20000
Beadle loam, 6 to 9 percent slopesBaC29623545482yyg7sd00519761:20000
Beadle-Jerauld-Dudley complex, 0 to 6 percent slopesBgB116533336762yyg6sd00519761:20000
Eakin-Beadle complex, 2 to 6 percent slopesEbB68623550182yyg5sd02319801:20000
Beadle-Jerauld complex, 0 to 6 percent slopesBcB516335500430t1csd02319801:20000
Beadle-Eakin complex, 6 to 9 percent slopesBbC26793550032yyg8sd02319801:20000
Beadle-Dudley complex, 0 to 2 percent slopesBfA9144176922yyg0sd02519921:20000
Beadle-Stickney complex, 1 to 6 percent slopesBeB4544176902yyg3sd02519921:20000
Beadle loam, 6 to 9 percent slopesBeC294176912yyg7sd02519921:20000
Beadle-Dudley complex, 0 to 2 percent slopesBaA39733528992yyg0sd03519661:20000
Beadle-Stickney complex, 1 to 6 percent slopesBaB1033548772yyg3sd04319791:20000
Beadle-Jerauld-Dudley complex, 0 to 6 percent slopesBgB80703564052yyg6sd07319871:20000
Beadle-Lane complex, 1 to 6 percent slopesBlB242835640630sqqsd07319871:20000
Beadle-Dudley complex, 0 to 2 percent slopesBdA1943564032yyg0sd07319871:20000
Beadle-Dudley complex, 0 to 2 percent slopesBeA46494174562yyg0sd07719921:20000
Beadle-Stickney complex, 1 to 6 percent slopesBdB8594174542yyg3sd07719921:20000
Beadle loam, 6 to 9 percent slopesBdC774174552yyg7sd07719921:20000
Egan-Beadle complex, 2 to 6 percent slopesEbB29143416488fzd3sd07919671:20000
Egan-Beadle complex, 6 to 9 percent slopesEbC9861416489fzd4sd07919671:20000
Beadle clay loam, 2 to 6 percent slopesBdB1266416472fzclsd07919671:20000
Egan-Beadle complex, 0 to 2 percent slopesEbA803416487fzd2sd07919671:20000
Beadle clay loam, 0 to 2 percent slopesBdA376416471fzcksd07919671:20000
Beadle clay loam, 6 to 9 percent slopesBdC330416473fzcmsd07919671:20000
Beadle-Stickney complex, 0 to 2 percent slopesBeA255813565622yyg2sd11519971:24000
Beadle-Dudley complex, 0 to 2 percent slopesBdA89763565612yyg0sd11519971:24000
Beadle-Stickney complex, 0 to 2 percent slopes, very stonyBfA28523565642yyjxsd11519971:24000
Beadle-Stickney complex, 1 to 6 percent slopesBeB7763565632yyg3sd11519971:24000
Beadle-Stickney complex, 1 to 6 percent slopes, very stonyBfB5233565652yyjysd11519971:24000
Beadle loam, 6 to 9 percent slopesBaC1713565602yyg7sd11519971:24000
Beadle-Jerauld complex, 0 to 6 percent slopesBgB1099735548430t1csd60319831:20000
Eakin-Beadle complex, 2 to 6 percent slopesBeB51273554822yyg5sd60319831:20000
Beadle-Eakin complex, 6 to 9 percent slopesBeC12733554832yyg8sd60319831:20000

Map of Series Extent

Approximate geographic distribution of the BEADLE 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 .