Official Series Description


Lab Data Summary

Aggregate lab data for the BULLCREEK soil series. This aggregation is based on all pedons with a current taxon name of BULLCREEK, 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 BULLCREEK 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
63A94P057794SD117002Bullcreek8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.2075005,-100.7300034
63B83P056182SD085004Bullcreek8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7019463,-99.8191681
63B14N0303S2013SD017001Bullcreek8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.00447,-99.0856983

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BULLCREEK 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 BULLCREEK 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 BULLCREEK 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 BULLCREEK 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 BULLCREEK 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 BULLCREEK 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 BULLCREEK 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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Click the image to view it full size.

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

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

Soil series sharing subgroup-level classification with BULLCREEK, 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-2012-03-15-06 | Corson County - July 1995

    Pattern of soils and parent material in the Sansarc-Dupree-Opal association (Soil Survey of Corson County, SD; 1995).

  2. SD-2012-03-15-38 | Haakon County - 1998

    Typical pattern of soils and parent material in the Bankard-Craft-Wendte, Ree, and Samsil-Pierre associations (Soil Survey of Haakon County, SD; 1998).

  3. SD-2012-03-15-41 | Haakon County - 1998

    Typical pattern of soils and parent material in the Ottumwa-Lakoma-Kolls and Ottumwa-Lakoma associations (Soil Survey of Haakon County, SD; 1998).

  4. SD-2012-03-15-42 | Haakon County - 1998

    Typical pattern of soils and parent material in the Ottumwa-Kirley and Ottumwa-Razor-Midway associations (Soil Survey of Haakon County, SD; 1998).

  5. SD-2012-03-15-52 | Hyde County - 1998

    Typical pattern of soils and parent material in the Sansarc-Opal association (Soil Survey of Hyde County, SD; 1998).

  6. SD-2012-03-15-60 | Jones County - 1999

    Typical pattern of soils and parent material in the Promise-Kirley and Promise associations (Soil Survey of Jones County, SD; 1999).

  7. SD-2012-03-15-61 | Jones County - 1999

    Typical pattern of soils and parent material in the Okaton-Lakoma association (Soil Survey of Jones County, SD; 1999).

  8. SD-2012-03-15-71 | Lyman County - May 1987

    Pattern of soils and parent material in the Sansarc-Opal and Munjor-Hilmoe-Bigbend associations (Soil Survey of Lyman County, SD; 1987).

Map Units

Map units containing BULLCREEK 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
Bullcreek-Slickspots complex, 0 to 6 percent slopesBmA93823561402wfqfsd03119861:24000
Bullcreek clay, 0 to 6 percent slopesBlA54483561392wfqdsd03119861:24000
Bullcreek-Slickspots complex, 0 to 6 percent slopesBx1574829126112wfqfsd04119721:24000
Bullcreek clay, 0 to 6 percent slopesBu1241529126102wfqdsd04119721:24000
Bullcreek clay, 0 to 6 percent slopesBu115233540772wfqdsd05519921:24000
Bullcreek-Slickspots complex, 0 to 6 percent slopesBx20663540792wfqfsd05519921:24000
Bullcreek-Slickspots complex, 0 to 6 percent slopesBx193929126222wfqfsd06519701:20000
Bullcreek clay, 0 to 6 percent slopesBu161129126212wfqdsd06519701:20000
Peno-Bullcreek complex, 3 to 15 percent slopesPnD913353317cvnbsd06519701:20000
Bullcreek clay, 0 to 6 percent slopesBuA8403537842wfqdsd06919921:20000
Artesian-Bullcreek complexAt954356400cyvssd07319871:20000
Okaton-Wendte-Bullcreek complex, 0 to 45 percent slopesOkE21701353658cw0bsd07519911:24000
Bullcreek clay, 0 to 6 percent slopesBu134863536222wfqdsd07519911:24000
Herdcamp-Bullcreek complexHb6155353627cvzbsd07519911:24000
Bullcreek-Slickspots complex, 0 to 6 percent slopesBx29243536232wfqfsd07519911:24000
Promise-Bullcreek claysPsA2859353671cw0rsd07519911:24000
Promise-Bullcreek-Kolls complexPtA358353672cw0ssd07519911:24000
Bullcreek clay, 0 to 6 percent slopesBuA203683555632wfqdsd08519841:20000
Bullcreek-Slickspots complex, 0 to 6 percent slopesBxA16383555642wfqfsd08519841:20000
Bullcreek clay, 0 to 6 percent slopesBu2943329330392wfqdsd11719771:24000
Bullcreek-Slickspots complex, 0 to 6 percent slopesBx1280629330402wfqfsd11719771:24000
Chantier-Bullcreek clays, 2 to 9 percent slopesCwB4069353470cvt8sd11719771:24000
Okaton-Wendte-Bullcreek complex, 0 to 45 percent slopesOfE46110159571335tsd11719771:24000
Bullcreek clay, 0 to 6 percent slopesBu1045429330442wfqdsd12319751:20000
Bullcreek clay, 0 to 6 percent slopesBu171129330472wfqdsd12919751:20000
Bullcreek clay, 0 to 6 percent slopesBu84033554882wfqdsd60319831:20000

Map of Series Extent

Approximate geographic distribution of the BULLCREEK 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 .