Official Series Description


Lab Data Summary

Aggregate lab data for the BLACKHALL soil series. This aggregation is based on all pedons with a current taxon name of BLACKHALL, 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 BLACKHALL 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 BLACKHALL 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 BLACKHALL 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 BLACKHALL 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 BLACKHALL 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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Competing Series

Soil series competing with BLACKHALL 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 BLACKHALL 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 BLACKHALL 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 BLACKHALL, 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-2012-03-15-73 | 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).

  2. 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).

  3. WY-2012-03-23-01 | Fremont County, East Part and Dubois Area - July 1993

    Soils and their landscape positions as they relate to parent material, precipitation zones, and temperature regimes (Soil Survey of Fremont County, East Part and Dubois Area, WY; 1993).

Map Units

Map units containing BLACKHALL 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
Twilight-Blackhall-Rock outcrop complex, 4 to 25 percent slopes8011903344752ckr1mt06919891:24000
Blackhall-Rock outcrop-Twilight complex, 8 to 45 percent slopes105021344670ckndmt06919891:24000
Busby-Blackhall fine sandy loams, 8 to 15 percent slopes123231344677cknmmt06919891:24000
Blackhall-Rock outcrop complex, 15 to 45 percent slopes18141541464394xcvmt63619831:24000
Twilight-Blackhall fine sandy loams, 6 to 18 percent slopesThD11770353251cvl6sd01919701:24000
Twilight-Blackhall fine sandy loams, 9 to 25 percent slopesTxE789583558042wf3nsd06319841:24000
Blackhall-Cabbart complex, 15 to 40 percent slopesBhE29751354618cx09sd10519771:24000
Blackhall-Twilight fine sandy loams, 9 to 40 percent slopesBmE45297355424cxv9sd60119831:24000
Blackhall-Rock outcrop complex, 15 to 40 percent slopesBlE19324355423cxv8sd60119831:24000
Bullock-Lardell-Blackhall fine sandy loams, 2 to 40 percent slopesBoE9966355425cxvbsd60119831:24000
Blackhall-Satanka-Rock outcrop complex, 5 to 20 percent slopes110511044603hppwy03119981:24000
Blackhall-Satanka-Rock outcrop complex, 5 to 20 percent slopes11415834501640jtzywy60119911:24000
Blackhall-Browtine, moist, complex, 15 to 45 percent slopes1133943501638jtzwwy60119911:24000
McFadden-Edlin-Blackhall complex, 5 to 40 percent slopes21933613502329jvq5wy62519851:24000
Rawlins-McFadden-Blackhall complex, 2 to 20 percent slopes2414963502367jvrdwy62519851:24000
Carmody-Blackhall complex, 6 to 45 percent slopes -- Draft47215258353s1wy6291:24000
Blackhall-Diamondville-Wilde-like complex, 15 to 60 percent slopes -- Draft550625515042qttdwy6291:24000
Cushool-Worfman-Blackhall sandy loams, 6 to 30 percent slopes -- draft3466283723781032ktm0wy6301:24000
McFadden-Blackhall-Edlin sandy loams, 5 to 50 percent slopes -- draft3175681123764642krx4wy6301:24000
McFadden-Blackhall sandy loams, 2 to 15 percent slopes -- draft3163469723781002ktlxwy6301:24000
Blazon-Blackhall complex, 10 to 40 percent slopes -- draft3793400124379932mtxywy6301:24000
Grieves-Blackhall association, 3 to 30 percent slopes -- draft3121950723775232kt09wy6301:24000
Blackhall-Rentsac complex, 10 to 40 percent slopes -- draft3761909023782442ktrkwy6301:24000
Blackhall-Rentsac complex, 0 to 15 percent slopes -- draft3501714223785502kv2fwy6301:24000
Blackhall-Carmody-Rock outcrop complex, 3 to 50 percent slopes -- draft3031413623778622ktc7wy6301:24000
McFadden-Brownsto-Blackhall complex, 6 to 20 percent slopes -- draft320819223778722ktckwy6301:24000
Carmody-Blackhall sandy loams, 2 to 15 percent slopes -- draft410539324210182m88cwy6301:24000
Blackhall-Seaverson-Rock outcrop, 5 to 40 percent slopes -- draft364503223939092lc1wwy6301:24000
Blackhall-Cragosen-Brownsto complex, 3 to 50 percent slopes -- draft366437723939112lc1ywy6301:24000
Blackhall-Satanka-Rock outcrop complex, 5 to 20 percent slopes -- draft45055325730302x8phwy6301:24000
Sweetlette-Blackhall complex, 1 to 6 percent slopes5334427825145452qcskwy6351:24000
Redcreek-Blackhall-Rock outcrop complex, 6 to 35 percent slopes1683683504027jxgywy63819901:24000
Blackhall-Kappes-Rentsac complex, 0 to 8 percent slopes1032211503938jxd2wy63819901:24000
Blackhall-Rentsac complex, 6 to 25 percent slopes1041985503939jxd3wy63819901:24000
Spool-Rock outcrop-Blackhall complex, 15 to 50 percent slopes1831236504047jxhlwy63819901:24000
Blackhall-Rock outcrop complex, 5 to 45 percent slopes0485127415757158yywy6471:24000
Blackhall-Carmody association, 5 to 45 percent slopes0232543515754258y0wy6471:24000
Blackhall-Carmody association2141841590595bhywy67719751:24000
Blackhall-Carmody association, hilly59966190154821tq8wy67719751:24000
Rock outcrop-Blackhall complex, hilly56415190157421tr3wy67719751:24000
Blackhall-Carmody association, hilly11760449502982jwd7wy71319861:24000
Rock outcrop-Blackhall complex, hilly19612993503061jwgswy71319861:24000
Blackhall-Rock outcrop complex, steep11610460502981jwd6wy71319861:24000
Cushool-Worfman-Blackhall sandy loams, 6 to 30 percent slopes -- draft734690525724432ktm0wy7371:24000
Rock outcrop-Blackhall complex, 20 to 50 percent slopes -- draft253186327716352t6c8wy7371:24000
Blackhall-Blazon-Poposhia complex, 3 to 30 percent slopes -- draft590832572292jx2swy7371:24000

Map of Series Extent

Approximate geographic distribution of the BLACKHALL 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 .