Official Series Description


Lab Data Summary

Aggregate lab data for the BIRKBECK soil series. This aggregation is based on all pedons with a current taxon name of BIRKBECK, 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 BIRKBECK 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
108A90P04791990IL203004Birkbeck4Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7813873,-89.3991699
108A40A1989S1961IL099001Birkbeck6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4399986,-89.0805588
108A82P0045S1980IL115035Birkbeck6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9066658,-88.8324966
108B78IL1030051978IL103005Birkbeck1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.8380192,-89.5247331
111DMY80251980IN107025Birkbeck2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.9474361,-86.9944694
115C94P06761994IL123038Birkbeck7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.0908546,-89.3345184
n/aCT-S091953-OH027-S09Birkbeck3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCT-0191954-OH027-019Birkbeck2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCT-s441955-OH027-S44Birkbeck3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aCT-0521956-OH027-052Birkbeck3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aPB-0091957-OH135-009Birkbeck2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aWA-0241959-OH165-024Birkbeck3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aGN-0211970-OH057-021Birkbeck3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aGN-0301988-OH057-030Birkbeck3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

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

Click the image to view it full size.

Click the image to view it full size.

Soil series sharing subgroup-level classification with BIRKBECK, 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-2010-09-01-43 | Marshall County - 2002

    Typical pattern of soils and parent material in the Hennepin-Birkbeck-Senachwine association (Soil Survey of Marshall County, Illinois; 2002).

  2. IL-2010-09-01-44 | Marshall County - 2002

    Typical pattern of soils and parent material in the Rozetta-Keomah association (Soil Survey of Marshall County, Illinois; 2002).

  3. IL-2010-09-01-57 | McLean County - 1998

    Typical pattern of soils and parent material in the Strawn-Mayville-Birkbeck association (Soil Survey of McLean County, Illinois; 1998).

  4. IL-2010-09-01-83 | Woodford County - 1999

    Typical pattern of soils and parent material in the Keomah-Rozetta association (Soil Survey of Woodford County, Illinois; 1999).

  5. IL-2010-09-01-84 | Woodford County - 1999

    Typical pattern of soils and parent material in the Miami-Birkbeck-Hennepin association (Soil Survey of Woodford County, Illinois; 1999).

  6. IL-2011-08-04-04 | De Witt County - 1991

    Typical pattern of soils and parent material in the Miami association (Soil Survey of De Witt County, Illinois; 1991).

  7. IL-2011-08-04-05 | De Witt County - 1991

    Typical pattern of soils and parent material in the Birkbeck-Russell-Keomah association (Soil Survey of De Witt County, Illinois; 1991).

  8. IL-2011-08-04-55 | Macon County - 1990

    Typical landscape pattern of soils and parent materials in the Miami-Birkbeck-Russell association (Soil Survey of Macon County, Illinois; 1990).

  9. IN-2012-01-19-17 | Fountain County - 1966

    Major soil series in the county in relation to their topography and underlying material (Soil Survey of Fountain County, Indiana; 1966).

Map Units

Map units containing BIRKBECK 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
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C2377018627222sssdil01120071:12000
Birkbeck silt loam, 2 to 5 percent slopes233B285418627212sssbil01120071:12000
Birkbeck silt loam, 10 to 18 percent slopes, eroded233D246018627232sssfil01120071:12000
Birkbeck silt loam, 2 to 5 percent slopes233B26682429812sssbil01919991:12000
Birkbeck silt loam, 0 to 2 percent slopes233A8851838902sss9il03719981:12000
Birkbeck silt loam, 2 to 5 percent slopes233B3761838912sssbil03719981:12000
Birkbeck silt loam, 2 to 5 percent slopes233B1784215313962sssbil03920051:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C2205615314202sssdil03920051:12000
Birkbeck silt loam, 2 to 5 percent slopes233B52810194182sssbil04120041:12000
Birkbeck silt loam, 2 to 5 percent slopes233B11631988222sssbil08920001:12000
Birkbeck silt loam, 0 to 2 percent slopes233A5221988212sss9il08920001:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C22761988232sssdil08920001:12000
Birkbeck silt loam, 0 to 2 percent slopes233A4317182562sss9il09320071:12000
Birkbeck silt loam, 2 to 5 percent slopes233B542910299232sssbil09920061:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C2445814261412sssdil09920061:12000
Birkbeck silt loam, 0 to 2 percent slopes233A2932634322sss9il09920061:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C226729213332sssdil10320041:12000
Birkbeck silt loam, 2 to 5 percent slopes233B13089213322sssbil10320041:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C298815960502sssdil10720061:12000
Birkbeck-Senachwine complex, 5 to 10 percent slopes, severely eroded733C381015960811qkvhil10720061:12000
Birkbeck-Senachwine silt loams, 5 to 10 percent slopes, eroded733C242815960801qkvgil10720061:12000
Birkbeck silt loam, 2 to 5 percent slopes233B21115960492sssbil10720061:12000
Birkbeck silt loam, 2 to 5 percent slopes, eroded233B261431991002ssscil11320001:12000
Birkbeck silt loam, 2 to 5 percent slopes233B33421990992sssbil11320001:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C212771991012sssdil11320001:12000
Birkbeck silt loam, 2 to 5 percent slopes233B966319139462sssbil11520071:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C245251821202sssdil12319971:15840
Birkbeck silt loam, 2 to 5 percent slopes233B22961821172sssbil12319971:15840
Birkbeck silt loam, 2 to 5 percent slopes, eroded233B28391821192ssscil12319971:15840
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C232042085717013il14120051:12000
Birkbeck silt loam, 2 to 5 percent slopes233B24162085707012il14120051:12000
Birkbeck silt loam, 2 to 5 percent slopes233B22641726922sssbil15519871:15840
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C214191726952sssdil15519871:15840
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C2160415920071qfm2il17720061:12000
Birkbeck silt loam, 10 to 18 percent slopes, eroded233D217717074751v9rvil17720061:12000
Birkbeck silt loam, 2 to 5 percent slopes233B12715920051qfm0il17720061:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C2109151793792sssdil17919911:15840
Birkbeck silty clay loam, 5 to 10 percent slopes, severely eroded233C3163217938060ngil17919911:15840
Birkbeck silt loam, 10 to 18 percent slopes, eroded233D211471793812sssfil17919911:15840
Birkbeck silt loam, 2 to 5 percent slopes233B217416131792sssbil18320061:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C21070793046vm74il19520031:12000
Birkbeck silt loam, 5 to 10 percent slopes, eroded233C265278691932sssdil20320081:12000
Birkbeck silt loam, 2 to 5 percent slopes, eroded233B254348691922ssscil20320081:12000
Birkbeck silt loam, 10 to 18 percent slopes, eroded233D27068691942sssfil20320081:12000
Birkbeck silt loam, 0 to 2 percent slopesBbA128416128041r47yin04119581:15840
Birkbeck silt loam, 2 to 6 percent slopes, moderately erodedBbB230916128061r480in04119581:15840
Birkbeck silt loam, 2 to 6 percent slopes, slightly erodedBbB111816128051r47zin04119581:15840
Birkbeck silt loam, 2 to 6 percent slopes, erodedBhyB22486242313844kin04519991:12000
Birkbeck silt loam, 0 to 2 percent slopesBhyA642242310844gin04519991:12000
Xenia-Birkbeck silt loams, 2 to 6 percent slopes, erodedXgB2177651630832w0w5in10719841:15840
Birkbeck silt loam, 0 to 2 percent slopesBbA120116129531r4drin16119581:15840
Birkbeck silt loam, 2 to 6 percent slopes, slightly erodedBbB17616129541r4dsin16119581:15840
Birkbeck silt loam, 2 to 6 percent slopes, moderately erodedBbB21316129551r4dtin16119581:15840
Birkbeck silt loam, 0 to 2 percent slopesBhA9271719445rxloh02719991:12000
Birkbeck silt loam, 2 to 6 percent slopesBhB7621719455rxmoh02719991:12000
Birkbeck silt loam, 1 to 4 percent slopesBbB22071692805p4noh05719741:15840
Birkbeck silt loam, 2 to 6 percent slopesBcB10185747420bvjoh05719741:15840
Birkbeck silt loam, 1 to 4 percent slopesBbB4081713185r8doh16519671:20000
Birkbeck-Urban land complex, 1 to 4 percent slopesBbUB69342222331ghcoh16519671:20000
Urban land-Birkbeck complex, 1 to 4 percent slopesUBbB23342222431ghdoh16519671:20000

Map of Series Extent

Approximate geographic distribution of the BIRKBECK 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 .