Official Series Description


Lab Data Summary

Aggregate lab data for the BLACKPIPE soil series. This aggregation is based on all pedons with a current taxon name of BLACKPIPE, 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 BLACKPIPE 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
63A82P082782SD103017Blackpipe7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1116333,-102.1352386
63A84P019382SD103018BLACKPIPE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties44.1269455,-102.2058334
6483P022783SD071002BLACKPIPE7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7972221,-101.5972214
6483P022883SD071003Blackpipe7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties43.7958336,-101.586113

Water Balance

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

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Soil series sharing subgroup-level classification with BLACKPIPE, 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-2012-03-15-14 | Custer and Pennington Counties, Prairie Parts - May 1996

    Pattern of soils and underlying material in the Ottumwa-Razor and the Midway-Razor associations (Soil Survey of Custer and Pennington Counties, Prairie Parts, SD; 1996).

  2. 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).

  3. SD-2012-03-15-55 | Jackson County, Northern Part - July 1987

    Pattern of soils and underlying material in the Weta-Cactusflat and Blackpipe-Wortman associations (Soil Survey of Jackson County, Northern Part, SD; 1987).

Map Units

Map units containing BLACKPIPE 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
Blackpipe silty clay loam, 2 to 6 percent slopesBkB3254354075cwfssd05519921:24000
Blackpipe-Wortman complexBo3190354076cwftsd05519921:24000
Blackpipe silty clay loam, 0 to 2 percent slopesBkA1090354074cwfrsd05519921:24000
Norrest-Blackpipe silt loams, 2 to 5 percent slopesNoB6781353409cvr9sd09519711:20000
Norrest-Blackpipe silt loams, 0 to 2 percent slopesNoA1362353408cvr8sd09519711:20000
Blackpipe soilsBp1156353345cvp7sd09519711:20000
Savo and Blackpipe soils, 2 to 6 percent slopesSkB398933543492tvvysd60019741:24000
Blackpipe silt loam, 6 to 15 percent slopesBlD223953543042y6f3sd60019741:24000
Blackpipe-Savo complex, moist, 2 to 6 percent slopesP038B11500274563530wn0sd60019741:24000
Blackpipe-Shingle complex, 6 to 15 percent slopesBsD104423543052y6f4sd60019741:24000
Midway-Blackpipe complex, 9 to 40 percent slopesMdD9436354331cwq1sd60019741:24000
Blackpipe silt loam, moist, 6 to 15 percent slopesP036D41127334192qt1bsd60019741:24000
Blackpipe-Wortman complex, 0 to 3 percent slopesBoA97002580877cygcsd60620111:24000
Blackpipe clay loam, 2 to 6 percent slopesBlB962225808752t5fhsd60620111:24000
Blackpipe silty clay loam, 2 to 6 percent slopesBkB87852580873cyg7sd60620111:24000
Blackpipe-Norrest complex, 6 to 12 percent slopesBnC54122580876cygbsd60620111:24000
Blackpipe silty clay loam, 0 to 2 percent slopesBkA48842580872cyg6sd60620111:24000
Blackpipe-Wortman complex, 2 to 6 percent slopesBoB372725808782wf36sd60620111:24000
Blackpipe clay loam, 0 to 2 percent slopesBlA204725808742t5ffsd60620111:24000
Savo-Blackpipe silty clay loams, 6 to 15 percent slopesU712D73925829442qt0gsd60620111:24000
Blackpipe-Norrest complex, 6 to 9 percent slopesU060C69425828852kqgzsd60620111:24000
Blackpipe-Wortman silt loams, 3 to 9 percent slopesBwC89332581005cy22sd61120111:24000
Blackpipe-Wortman complex, 6 to 9 percent slopesU070C138925828612wf37sd61120111:24000
Blackpipe-Wortman complex, 2 to 6 percent slopesU070B83825828662wf36sd61120111:24000
Blackpipe-Wortman complex, 2 to 6 percent slopesU070B222723754162wf36sd61220111:20000
Blackpipe-Norrest complex, 6 to 9 percent slopesU060C108823750952kqgzsd61220111:20000
Blackpipe clay loam, 0 to 2 percent slopesU050A45723754152t5ffsd61220111:20000
Blackpipe clay loam, 2 to 6 percent slopesU050B43623750942t5fhsd61220111:20000
Blackpipe-Wortman complex, 6 to 9 percent slopesU070C13523750972wf37sd61220111:20000
Savo-Blackpipe silty clay loams, 6 to 15 percent slopesU712D7625474332qt0gsd61220111:20000

Map of Series Extent

Approximate geographic distribution of the BLACKPIPE 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 .