Official Series Description


Lab Data Summary

Aggregate lab data for the BLAINCREEK soil series. This aggregation is based on all pedons with a current taxon name of BLAINCREEK, 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 BLAINCREEK 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
4692P049991MT049003Blaincreek6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties47.0582314,-112.1117249

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLAINCREEK 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 BLAINCREEK 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 BLAINCREEK 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 BLAINCREEK 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 flats position figure.

Competing Series

Soil series competing with BLAINCREEK 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 BLAINCREEK 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 BLAINCREEK 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 flats position figure.

Soil series sharing subgroup-level classification with BLAINCREEK, 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 BLAINCREEK 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
Tolbert-Blaincreek complex, 2 to 15 percent slopes439D537415547756sdmt62219971:24000
Tolbert-Blaincreek-Adel complex, 15 to 45 percent slopes439E452115547856sfmt62219971:24000
Blaincreek-Tolbert complex, 40 to 70 percent slopes439G32415547956sgmt62219971:24000
Blaincreek-Sawicki complex, 4 to 15 percent slopes750C159924952812psp3mt62420211:24000
Blaincreek-Sawicki complex, 0 to 4 percent slopes750B57125264212qlxfmt62420211:24000
Blaincreek, very stony-Tolbert, extremely stony-Sawicki, stony complex, 15 to 35 percent slopes703E19124874122phc3mt62420211:24000
Blaincreek-Castner complex, 2 to 15 percent slopes561D4125232264z1tmt62420211:24000
Tolbert, very stony-Rock outcrop-Blaincreek, very stony, complex, 35 to 60 percent slopes1675F216215068251sqmt62719981:24000
Tolbert, very stony-Blaincreek, stony-Rock outcrop complex, 8 to 35 percent slopes1675E210815068151spmt62719981:24000
Sawicki, very stony-Blaincreek, very stony-Tolbert, bouldery, complex, 15 to 45 percent slopes1658E115315066951s9mt62719981:24000
Sawicki, stony-Blaincreek-Tolbert, very stony, complex, 15 to 45 percent slopes1654E78015066451s4mt62719981:24000
Blaincreek, very stony-Sawicki, very stony-Tolbert, very bouldery, complex, 35 to 70 percent slopes1451F69115062051qqmt62719981:24000
Tolbert-Blaincreek complex, 8 to 35 percent slopes1672E49515068051snmt62719981:24000
Tolbert-Blaincreek complex, 8 to 35 percent slopes, warm1671E42815067951smmt62719981:24000
Sawicki, stony-Blaincreek, very stony, complex, 4 to 15 percent slopes1658D6115066851s8mt62719981:24000
Castner-Blaincreek-Rock outcrop complex, 4 to 35 percent slopes160D50651477104ypvmt63019911:24000
Blaincreek-Castner gravelly loams, 4 to 25 percent slopes260D38241477594yrfmt63019911:24000
Whitlash, rubbly-Blaincreek, very bouldery-Rock outcrop complex, 15 to 35 percent slopes350E143823928052l9x8mt6321:24000
Blaincreek, very stony-Tolbert, extremely stony-Sawicki, stony complex, 15 to 35 percent slopes703E66025124452phc3mt6321:24000
Sawicki, extremely stony-Blaincreek, very stony complex, 15 to 35 percent slopes140E45923927752l9w9mt6321:24000
Sixteenmile-Blaincreek-Brickner complex, 2 to 8 percent slopes371C15123928092l9xdmt6321:24000
Tolbert, very stony-Blaincreek, stony-Rock outcrop complex, 8 to 35 percent slopes1675E21717030731v55vmt63520061:24000
Whitlash, rubbly-Blaincreek, very bouldery-Rock outcrop, complex, 15 to 35 percent slopes350E10461637794pdp0mt63720141:24000
Sixteenmile-Blaincreek-Brickner complex, 2 to 8 percent slopes371C625913833671hfhrmt63720141:24000
Blaincreek-Castner complex, 2 to 15 percent slopes561D26791480504z1tmt63720141:24000
Sawicki, extremely stony-Blaincreek, very bouldery complex, 15 to 35 percent slopes140E2599637158pd0hmt63720141:24000
Blaincreek, stony-Braziel-Tolbert, very stony complex, 4 to 15 percent slopes388D175824947422prr3mt63720141:24000
Winspect, very bouldery-Blaincreek, very stony-Tolbert, very stony complex, 8 to 35 percent slopes50E1722639209pg4nmt63720141:24000
Shanley-Blaincreek, stony complex, 4 to 15 percent slopes140D969637148pd05mt63720141:24000
Blaincreek, stony-Braziel-Shanley complex, 15 to 35 percent slopes388E26724947432prr4mt63720141:24000
Tolbert-Blaincreek complex, 2 to 15 percent slopes439D24249352656sdmt63720141:24000
Blaincreek-Wheelbarrow complex, 4 to 15 percent slopes531D424633723p8fpmt64520131:12000
Tolbert-Shawmut-Blaincreek complex, very stony, 15 to 60 percent slopes8608F37471567725845mt6691:24000
Blaincreek, stony-Cabba, stony-Castner, stony-Meagher, extremely stony-Vershal, stony complex, 25 to 60 percent slopes5616F99315648157tsmt6691:24000
Tolbert, stony-Blaincreek, stony-Bowery complex, cool, 35 to 60 percent slopes802F2211017171134fzmt6691:24000
Fughes, extremely stony-Blaincreek, very stony families, complex, 25 to 60 percent slopes1453447791185vk93ut6511:24000

Map of Series Extent

Approximate geographic distribution of the BLAINCREEK 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 .