Official Series Description


Lab Data Summary

Aggregate lab data for the BLAIR soil series. This aggregation is based on all pedons with a current taxon name of BLAIR, 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 BLAIR were used in the calculation. Source: KSSL snapshot . Methods used to assemble the KSSL snapshot used by SoilWeb / SDE

Click the image to view it full size.

Pedons used in the lab summary:

MLRALab IDPedon IDTaxonnameCINSSL / NASIS ReportsLink To SoilWeb GMap
11379IL1450081979IL145008Blair1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1816483,-89.3080859
11379IL1450221979IL145022Blair3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0734555,-89.327617
11383IL1210311983IL121031Blair2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8046139,-88.9488639
11384IL1210161984IL121016Blair2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8077472,-89.069625
11384IL1910091984IL191009Blair2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3913778,-88.5828083
11385IL1210221985IL121022Blair2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6478111,-88.9547889
11385IL1210621985IL121062Blair2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6805944,-88.9502194
11386IL1210111986IL121011Blair4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5026889,-88.6996472
11389IL0550051989IL055005Blair3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0708778,-89.0818167
11384P025883IL079020Blair6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1688881,-88.3116684
11386P051685IL121006Blair6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5441666,-89.0519409
11388P048286IL191033Blair7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5338898,-88.6191635
11340A2800S1972IL081003BLAIR6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1319427,-88.7513885
114B78IL1570451978IL157045Blair3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1327682,-89.6292461
114B81IL1330051981IL133005Blair1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2384302,-90.0312285
114B82IL1330041982IL133004Blair1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.3001376,-90.0720688
114B81P0061S1980IL145028Blair6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1633339,-89.4433365
114B81P0037S1980IL157125BLAIR6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.1669426,-89.7133331
115B81IL1330101981IL133010Blair1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2178082,-90.1373902
115B82IL1330021982IL133002Blair1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2239248,-90.1526601
115C69IL0010021969IL001002Blair3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0992182,-91.1345754
115C69IL0010031969IL001003Blair3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.0585492,-91.1501953
n/a84IL1910061984IL191006Blair2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.



Click the image to view it full size.

Sibling Summary

Siblings are those soil series that occur together in map units, in this case with the BLAIR series. Sketches are arranged according to their subgroup-level taxonomic structure. Source: SSURGO snapshot , parsed OSD records and snapshot of SC database .

Click the image to view it full size.

Select annual climate data summaries for the BLAIR series and siblings. 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 BLAIR 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Competing Series

Soil series competing with BLAIR share the same family level classification in Soil Taxonomy. Source: parsed OSD records and snapshot of the SC database .

Click the image to view it full size.

Select annual climate data summaries for the BLAIR 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 BLAIR 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 .

Click the image to view it full size.

Click the image to view it full size.

There are insufficient data to create the 3D mountains figure.

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BLAIR, 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. IL-2010-08-31-01 | Clay County - 1998

    Typical pattern of soils and parent material in the Bluford-Hickory-Ava association (Soil Survey of Clay County, Illinois; 1998).

  2. IL-2010-08-31-03 | Clinton County - 2002

    Typical pattern of soils and parent material in the Hoyleton-Darmstadt-Cisne association (Soil Survey of Clinton County, Illinois; 2002).

  3. IL-2010-08-31-05 | Clinton County - 2002

    Typical pattern of soils and parent material in the Bluford-Hickory-Blair association (Soil Survey of Clinton County, Illinois; 2002).

  4. IL-2010-08-31-06 | Clinton County - 2002

    Typical pattern of soils and parent material in the Blair-Muren-Iva association (Soil Survey of Clinton County, Illinois; 2002).

  5. IL-2010-09-01-06 | Edgar County - 2002

    Typical pattern of soils and parent material in the Weir-Stoy-Hickory association (Soil Survey of Edgar County, Illinois; 2002).

  6. IL-2010-09-01-10 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Hoyleton-Cisne association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  7. IL-2010-09-01-11 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Bluford-Wynoose association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  8. IL-2010-09-01-13 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Ava-Bluford-Plumfield association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  9. IL-2010-09-01-14 | Franklin and Jefferson Counties - 2003

    Typical pattern of soils and parent material in the Grantsburg-Zanesville association (Soil Survey of Franklin and Jefferson Counties, Illinois; 2003).

  10. IL-2010-09-01-77 | Washington County - 1998

    Typical pattern of soils and parent material in the Bluford-Hoyleton-Wynoose association (Soil Survey of Washington County, Illinois; 1998).

  11. IL-2010-09-01-78 | Washington County - 1998

    Typical pattern of soils and parent material in the Marine-Rushville-Muren association (Soil Survey of Washington County, Illinois; 1998).

  12. IL-2010-09-01-80 | Washington County - 1998

    Typical pattern of soils and parent material in the Bluford-Hickory-Blair association (Soil Survey of Washington County, Illinois; 1998).

  13. IL-2010-09-09-01 | Wayne County -

    Typical pattern of soils and parent material in the Bluford-Wynoose association (Soil Survey of Wayne County, Illinois).

  14. IL-2010-09-09-02 | Wayne County -

    Typical pattern of soils and parent material in the Ava-Blair-Hickory association (Soil Survey of Wayne County, Illinois).

  15. IL-2011-08-04-77 | Monroe County - 1987

    Typical pattern of soils and parent material in the Blair-Marine association (Soil Survey of Monroe County, Illinois; 1987).

  16. IL-2011-08-04-87 | Perry County - 1988

    Typical pattern of soils and parent material in the Hoyleton-Cisne association (Soil Survey of Perry County, Illinois; 1988).

  17. IL-2011-08-04-88 | Perry County - 1988

    Typical pattern of soils and parent material in the Hosmer-Hickory-Blair association (Soil Survey of Perry County, Illinois; 1988).

  18. IL-2011-08-05-02 | Washington County - 1998

    Typical pattern of soils and parent material in the Marine-Rushville-Muren association (Soil Survey of Washington County, Illinois; 1998).

  19. IL-2011-08-05-03 | Washington County - 1998

    Typical pattern of soils and parent material in the Bluford-Hoyleton-Wynoose association (Soil Survey of Washington County, Illinois; 1998).

  20. IL-2011-08-05-05 | Washington County - 1998

    Typical pattern of soils and parent material in the Bluford-Hickory-Blair association (Soil Survey of Washington County, Illinois; 1998).

Map Units

Map units containing BLAIR 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
Blair-Atlas silty clay loams, 5 to 10 percent slopes, severely eroded927C3313716074721qypyil02320061:12000
Blair-Atlas silt loams, 5 to 10 percent slopes, eroded927C2303216074701qypwil02320061:12000
Blair-Grantfork complex, 5 to 10 percent slopes, eroded934C21545210919928sspil02519931:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C265051746652t963il02719921:15840
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C359451746662t964il02719921:15840
Blair-Grantfork complex, 5 to 10 percent slopes, eroded934C252851746885vs3il02719921:15840
Blair silty clay loam, 10 to 18 percent slopes, severely eroded5D318101746672t967il02719921:15840
Blair-Grantfork complex, 2 to 5 percent slopes, eroded934B25551746875vs2il02719921:15840
Ava-Blair complex, 2 to 7 percent slopes, eroded844B2134251748645vysil03519921:15840
Blair silt loam, 2 to 5 percent slopes, eroded5B26391748445vy4il03519921:15840
Blair-Atlas complex, 5 to 10 percent slopes, eroded927C22651748785vz7il03519921:15840
Blair silt loam, 2 to 5 percent slopes, severely eroded5B32151748455vy5il03519921:15840
Blair silt loam, 5 to 10 percent slopes, eroded5C213258435282t963il04519971:12000
Blair soils, 7 to 12 percent slopes, severely eroded5D331451754845wlsil04719671:15840
Blair silt loam, 7 to 12 percent slopes, eroded5D230411754835wlril04719671:15840
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C3113808070952t964il05520051:12000
Blair-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded927D32579807190w2ydil05520051:12000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C31994915404512t964il08120051:12000
Blair-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded927D3490015404971nq0gil08120051:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C22515405062t963il08120051:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C223631767462t963il10119521:42240
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C33851767472t964il10119521:42240
Blair silty clay loam, 7 to 15 percent slopes, severely eroded5D31691767495xxlil10119521:42240
Blair silt loam, 7 to 15 percent slopes, eroded5D21301767485xxkil10119521:42240
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C39520239102t964il12120081:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C2109517211562t963il13520071:12000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C336117211602t964il13520071:12000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C31155914036892t964il14520051:12000
Blair silty clay loam, 10 to 18 percent slopes, severely eroded5D3839714036852t967il14520051:12000
Blair silt loam, 10 to 18 percent slopes5D278114036882t965il14520051:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C222962004452t963il15720011:12000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C320262004462t964il15720011:12000
Blair-Grantfork silt loams, 10 to 18 percent slopes, severely eroded934D313012005406qp1il15720011:12000
Blair silty clay loam, 10 to 18 percent slopes, severely eroded5D37842004482t967il15720011:12000
Blair silt loam, 10 to 18 percent slopes, eroded5D23312004472t966il15720011:12000
Blair-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded927D32062005246qnjil15720011:12000
Blair soils, 7 to 12 percent slopes, severely eroded5D3391020268052611til15919671:12000
Blair silt loam, 7 to 12 percent slopes, eroded5D2311420268042611sil15919671:12000
Blair silty clay loam, 10 to 18 percent slopes, severely eroded5D33151830922t967il16319971:12000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C33031830912t964il16319971:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C22161830902t963il16319971:12000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C310461797022t964il18519621:20000
Blair silt loam, 5 to 10 percent slopes, eroded5C21701797012t963il18519621:20000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C31530915288972t964il18920061:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C2934815288982t963il18920061:12000
Blair silty clay loam, 10 to 18 percent slopes, severely eroded5D3333715288952t967il18920061:12000
Blair silt loam, 10 to 18 percent slopes5D90615288962t965il18920061:12000
Blair-Grantfork silt loams, 10 to 18 percent slopes, severely eroded934D343715289751nb0sil18920061:12000
Blair silt loam, 5 to 10 percent slopes, eroded5C2628319063582t963il19120081:12000
Blair silty clay loam, 5 to 10 percent slopes, severely eroded5C378514780362t964il19920071:12000
Blair-Atlas silty clay loams, 10 to 18 percent slopes, severely eroded927D35190286721w2til19920071:12000

Map of Series Extent

Approximate geographic distribution of the BLAIR 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 .