Official Series Description


Lab Data Summary

Aggregate lab data for the BLACKHAWK soil series. This aggregation is based on all pedons with a current taxon name of BLACKHAWK, 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 BLACKHAWK 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
2440A3186S1956NV027014BLACKHAWK5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6832275,-117.7009659
2440A3188S1966NV027001Blackhawk5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.685173,-117.6592941
2440A3187S1966NV027002BLACKHAWK5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.6829491,-117.6820755

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLACKHAWK 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 BLACKHAWK 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 BLACKHAWK 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 BLACKHAWK 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 BLACKHAWK 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 BLACKHAWK 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 BLACKHAWK 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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Soil series sharing subgroup-level classification with BLACKHAWK, 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

No block diagrams are available.

Map Units

Map units containing BLACKHAWK 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
McConnel-Blackhawk complexMh2915476113hzfhnv61219681:24000
Rad-Blackhawk complexRd1570476147hzglnv61219681:24000
Golconda-Blackhawk association41122425193812qj9fnv61219681:24000
Blackhawk-Trocken association1584930474689hxyknv76019941:24000
Ricert-Blackhawk-Orovada association12896140479056j2hfnv76819851:63360
Eastwell-Blackhawk-Pineval association3603785479238j2p9nv76819851:63360
Blackhawk very fine sandy loam, 2 to 8 percent slopes2201335479117j2kdnv76819851:63360
Blackhawk-Tenabo-Desatoya variant association2211295479118j2kfnv76819851:63360
Blackhawk silt loam, 0 to 2 percent slopes15118373475224hyhtnv76919861:24000
Eastwell-Shabliss-Blackhawk association15504725475228hyhynv76919861:24000
Golconda-Blackhawk association4112895479671j348nv77519851:24000
Blackhawk very fine sandy loam, 2 to 8 percent slopes2201290479535j2zwnv77519851:24000
Blackhawk-Golconda-Orovada association15423016475564hyvsnv77719931:24000
Bliss-Blackhawk-Adelaide association16712848475600hywynv77719931:24000
Davey-Blackhawk association20411670475626hyxsnv77719931:24000
Blackhawk-Clurde association1564723475568hyvxnv77719931:24000
Blackhawk silt loam, 2 to 8 percent slopes1524551475556hyvjnv77719931:24000
Blackhawk-Trocken association1584130475577hyw6nv77719931:24000
Blackhawk-Broyles association1572367475572hyw1nv77719931:24000
Blackhawk loamy fine sand, 0 to 2 percent slopes 1/1552126475566hyvvnv77719931:24000
Blackhawk silt loam, 0 to 2 percent slopes 1/1511209475555hyvhnv77719931:24000

Map of Series Extent

Approximate geographic distribution of the BLACKHAWK 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 .