Official Series Description


Lab Data Summary

Aggregate lab data for the BULLOCK soil series. This aggregation is based on all pedons with a current taxon name of BULLOCK, 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 BULLOCK 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
5440A2542S1976SD093016Bullock3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.0201378,-102.0856934
58A83P071480MT087496Bullock7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties46.648056,-106.4925003
58D78P053978SD063037Bullock8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3477783,-103.9947205
58D78P054378SD063041Bullock8Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties45.3444443,-103.9777756

Water Balance

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

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

Soil series sharing subgroup-level classification with BULLOCK, 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-2012-03-15-10 | Corson County - July 1995

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

  2. SD-2012-03-15-48 | Harding County - December 1988

    Pattern of soils and parent material in the Hanly-Korchea-Glendive and Bullock-Parchin associations (Soil Survey of Harding County, SD; 1988).

  3. SD-2012-03-15-49 | Harding County - December 1988

    Pattern of soils and parent material in the Cabbart-Rock outcrop-Delridge association (Soil Survey of Harding County, SD; 1988).

  4. SD-2012-03-15-73 | Meade County, Northern Part - January 1986

    Pattern of soils and parent material in the Assinniboine-Blackhall-Twilight association (Soil Survey of Meade County, Northern Part, SD; 1986).

  5. SD-2012-03-15-75 | Meade County, Northern Part - January 1986

    Pattern of soils and parent material in the Bullock-Parchin association (Soil Survey of Meade County, Northern Part, SD; 1986).

  6. SD-2012-03-16-07 | Ziebach County - March 1990

    Pattern of soils and parent material in the Bullock-Vebar-Parchin association (Soil Survey of Ziebach County, SD; 1990).

Map Units

Map units containing BULLOCK 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
Parchin-Bullock complex, 2 to 8 percent slopes121C15852342853chrsmt01119921:24000
Archin-Davidell-Bullock complex, 2 to 8 percent slopes192C34583433312yk0smt01719951:24000
Cabbart-Bullock, eroded complex, 2 to 25 percent slopes994E378343836cjshmt01719951:24000
Bullock, eroded-Ralore clay loams, 2 to 15 percent slopes914D108343743cjphmt01719951:24000
Parchin-Bullock complex, 2 to 8 percent slopes121C5737342074cgynmt02519911:24000
Bonfri-Bullock, eroded-Cabbart complex, 4 to 25 percent slopes13E20283428022yk11mt03320021:24000
Bullock, thin surface-Rominell complex, 2 to 8 percent slopes323C1415342777chpbmt03320021:24000
Bullock loam, 2 to 8 percent slopes27C122513697pl21mt62420211:24000
Bullock, eroded-Rominell complex, 2 to 8 percent slopes4325575348074cp66mt64919851:24000
Bullock, eroded-Rallod, warm, clay loams, 2 to 15 percent slopes4214357348073cp65mt64919851:24000
Bonfri-Marmarth-Bullock fine sandy loams, 1 to 4 percent slopes3591053480652yk16mt64919851:24000
Bonfri-Bullock, eroded-Cabbart complex, 4 to 25 percent slopes3390193480632yk11mt64919851:24000
Bullock loam, 2 to 8 percent slopes27C771642972pl21mt66620081:24000
Rhame-Bullock-Kremlin complex, 9 to 35 percent slopesL2307F3827584932qxjhnd02519811:20000
Rhame-Bullock-Kremlin complex, 9 to 35 percent slopesL2307F236227151472qxjhnd05320031:24000
Bullock-Parchin fine sandy loams, 0 to 9 percent slopesBrB62710356142cylgsd03119861:24000
Bullock-Slickspots-Rock outcrop complex, 0 to 40 percent slopesBvE24701356145cylksd03119861:24000
Bullock-Parchin-Slickspots complex, 0 to 9 percent slopesBsB22200356143cylhsd03119861:24000
Bullock fine sandy loam, 0 to 6 percent slopesBnA9144356141cylfsd03119861:24000
Bullock-Slickspots complex, 0 to 6 percent slopesBuB9013356144cyljsd03119861:24000
Bullock-Telfer-Parchin complex, 0 to 9 percent slopesBzB5840356146cyllsd03119861:24000
Evridge-Bullock fine sandy loams, 0 to 6 percent slopesEwB5655356157cylysd03119861:24000
Parchin-Bullock-Cabba complex, 6 to 30 percent slopesPdD2528356187cymxsd03119861:24000
Parchin-Bullock-Slickspots complex, 2 to 9 percent slopesArB6338354174cwjzsd04119721:24000
Parchin-Bullock fine sandy loams, 2 to 9 percent slopesPbB1433253557722wf3rsd06319841:24000
Bullock-Cabbart complex, 6 to 25 percent slopesBoD1073393557222wf31sd06319841:24000
Bullock-Parchin-Slickspots complex, 2 to 9 percent slopesBpB726003557232wf3qsd06319841:24000
Archin-Bullock fine sandy loams, 0 to 4 percent slopesAkA401713557122y6djsd06319841:24000
Bullock-Slickspots complex, 0 to 4 percent slopesBsA18192355724cy4zsd06319841:24000
Trey-Parchin-Bullock complex, 2 to 9 percent slopesTvB11634355802cy7hsd06319841:24000
Bullock-Assinniboine fine sandy loams, 0 to 4 percent slopesBnA2198355721cy4wsd06319841:24000
Bullock fine sandy loam, 6 to 20 percent slopes, extremely stonyBkF1967355720cy4vsd06319841:24000
Bullock-Slickspots complex, 0 to 15 percent slopesAbC83258354608cwzzsd10519771:24000
Bullock-Parchin loams, 0 to 9 percent slopesAaB77258354607cwzysd10519771:24000
Bullock-Vanda-Rock Outcrop complex, 2 to 25 percent slopesBuD170143546542zzvqsd10519771:24000
Bullock-Trembles-Slickspots complex, channeledAc16821354609cx00sd10519771:24000
Bullock-Parchin fine sandy loams, 0 to 9 percent slopesBpB38900355828cy8bsd13719851:24000
Cohagen-Vebar-Bullock fine sandy loams, 6 to 25 percent slopesCrD22745355834cy8jsd13719851:24000
Bullock-Slickspots-Parchin complex, 2 to 25 percent slopesBsC13402355829cy8csd13719851:24000
Parchin-Bullock fine sandy loams, 1 to 6 percent slopesPbB10615355860cy9csd13719851:24000
Bullock-Parchin fine sandy loams, 0 to 4 percent slopesBpB94211355426cxvcsd60119831:24000
Parchin-Bullock fine sandy loams, 2 to 6 percent slopesPbB43920355456cxwbsd60119831:24000
Bullock-Slickspots complex, 0 to 4 percent slopesBsB13603355427cxvdsd60119831:24000
Bullock-Lardell-Blackhall fine sandy loams, 2 to 40 percent slopesBoE9966355425cxvbsd60119831:24000
Rock outcrop-Cabbart-Bullock complex, 15 to 40 percent slopesRoE5286355461cxwhsd60119831:24000
Abston-Bullock complex, 5 to 25 percent slopes1017082501616jtz5wy60119911:24000

Map of Series Extent

Approximate geographic distribution of the BULLOCK 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 .