Official Series Description


Lab Data Summary

Aggregate lab data for the BLOOMFIELD soil series. This aggregation is based on all pedons with a current taxon name of BLOOMFIELD, 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 BLOOMFIELD 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
108B82IL0110621982IL011062Bloomfield1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.4882303,-89.7810857
11072IL0910121972IL091012Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.1478816,-88.0478137
111CCS76011976IN017001Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.7764583,-86.2788472
111CCS76021976IN017002Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.8096111,-86.2685167
114ACL77021977IN021002Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.243225,-87.1283861
114A91P074391IN119020Bloomfield6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.1877785,-86.8411102
114BJN79011979IN071001Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.8591389,-86.0798639
115AKX76081976IN083008Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7462806,-87.4774444
115AKX77101977IN083010Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.7982278,-87.4495889
115AGN80021980IN055002Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.9414,-87.0989
115APK80011980IN125001Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.5340833,-87.2360611
115AGB83131983IN051013Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.2745583,-87.7601306
115A86IL1930601986IL193060Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.0991861,-88.0783917
115A88P042086IL193058Bloomfield6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.9469452,-88.1399994
115C65IL0710021965IL071002Bloomfield5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.9332317,-90.9384872
115C78IL1710411978IL171041Bloomfield1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6241079,-90.5277437
115C82IL1710051982IL171005Bloomfield1Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.6058498,-90.5005344
115C84IL1250061984IL125006Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.376075,-89.9498667
115C84IL1250071984IL125007Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.3213333,-90.0417472
115C84IL1250121984IL125012Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties40.1161389,-90.1070861
120B93P0541S1993IN123001Bloomfield6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties37.8683319,-86.6458359
121SW81211981IN155021Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties38.6977389,-85.2027444
98KO77011977IN085001Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3268361,-85.9573667
n/a79IL1570771979IL157077Bloomfield2Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/a80IL1570991980IL157099Bloomfield3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLOOMFIELD 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 BLOOMFIELD 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 BLOOMFIELD 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 BLOOMFIELD 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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Click the image to view it full size.

Competing Series

Soil series competing with BLOOMFIELD 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 BLOOMFIELD 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 BLOOMFIELD 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.

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There are insufficient data to create the 3D flats position figure.

Soil series sharing subgroup-level classification with BLOOMFIELD, 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-2011-08-04-59 | Mason County - 1995

    Typical pattern of soils and parent material in the Plainfield-Bloomfield association (Soil Survey of Mason County, Illinois; 1995).

  2. IL-2011-08-04-67 | Mason County - 1995

    Typical pattern of soils and parent material in the Fayette-Alvin-Bloomfield association (Soil Survey of Mason County, Illinois; 1995).

  3. IN-2010-09-24-18 | Owen County -

    Typical pattern of soils and parent materials in the Alvin-Princeton-Bloomfield and Stonelick-Gessie-McAdoo associations (Soil Survey of Owen County, Indiana).

  4. IN-2012-01-19-19 | Gibson County - June 1989

    Pattern of soils and parent material in the Bloomfield-Alvin association (Soil Survey of Gibson County, Indiana; 1989).

  5. IN-2012-01-19-27 | Jackson County - October 1990

    Typical pattern of soils and parent material in the Bloomfield-Alvin association (Soil Survey of Jackson County, Indiana; 1990).

Map Units

Map units containing BLOOMFIELD 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
Bloomfield fine sand, 1 to 7 percent slopes53B29992627868tfzil01720031:12000
Bloomfield fine sand, 7 to 15 percent slopes53D15362627878tg0il01720031:12000
Bloomfield fine sand, 10 to 15 percent slopes53D1151746615vr7il02719921:15840
Bloomfield fine sand, 1 to 12 percent slopes53C516211690738qil05919661:20000
Bloomfield fine sand, 12 to 30 percent slopes53E499211691738ril05919661:20000
Bloomfield fine sand, 1 to 7 percent slopes53B44721177073c9il06119681:15840
Bloomfield fine sand, 7 to 15 percent slopes53D20421177173cbil06119681:15840
Bloomfield fine sand, 15 to 45 percent slopes53F14021177273ccil06119681:15840
Bloomfield loamy fine sand, 7 to 15 percent slopes53D781194953223fn4il08519901:12000
Bloomfield fine sand, 4 to 7 percent slopes53C6851767405xx9il10119521:42240
Bloomfield fine sand, 2 to 4 percent slopes53B5831767395xx8il10119521:42240
Bloomfield fine sand, 7 to 12 percent slopes53D1551767425xxcil10119521:42240
Bloomfield fine sand, 7 to 12 percent slopes, eroded53D2641767435xxdil10119521:42240
Bloomfield fine sand, 4 to 7 percent slopes, eroded53C2631767415xxbil10119521:42240
Princeton-Bloomfield fine sands, 7 to 15 percent slopes, eroded861D2151815960441qkt9il10720061:12000
Princeton-Bloomfield fine sands, 15 to 35 percent slopes861F61215960451qktbil10720061:12000
Princeton-Bloomfield fine sands, 1 to 7 percent slopes, eroded861B233415960921qkvvil10720061:12000
Bloomfield loamy fine sand, 2 to 5 percent slopes, rarely flooded7053B6431989456p0lil11920011:12000
Bloomfield fine sand, 1 to 7 percent slopes53B198021778025z0kil12519891:15840
Bloomfield fine sand, 7 to 15 percent slopes53D28191778035z0lil12519891:15840
Princeton-Bloomfield fine sands, 1 to 7 percent slopes, eroded861B2322914088451j90mil12920051:12000
Princeton-Bloomfield fine sands, 7 to 15 percent slopes, eroded861D2155714088481j90qil12920051:12000
Princeton-Bloomfield fine sands, 15 to 35 percent slopes861F68414088491j90ril12920051:12000
Bloomfield fine sand, 1 to 7 percent slopes53B24714062531j6b0il12920051:12000
Bloomfield fine sand, 7 to 15 percent slopes53D15514062541j6b1il12920051:12000
Bloomfield loamy sand, 15 to 35 percent slopes53F20316721661t40vil13719841:15840
Bloomfield fine sand, 7 to 15 percent slopes53D5516721651t40til13719841:15840
Bloomfield fine sand, 1 to 7 percent slopes53B2216721641t40sil13719841:15840
Bloomfield fine sand, 1 to 7 percent slopes53B5201728325sv7il15519871:15840
Bloomfield fine sand, 7 to 15 percent slopes53D4861728365svcil15519871:15840
Bloomfield loamy fine sand, 2 to 5 percent slopes53B2332004546ql8il15720011:12000
Bloomfield loamy fine sand, 10 to 18 percent slopes, eroded53D21962004556ql9il15720011:12000
Bloomfield loamy fine sand, 18 to 40 percent slopes53F1152020956s96il16920001:12000
Bloomfield loamy sand, 15 to 35 percent slopes53F94525420602qrbril17119841:12000
Bloomfield fine sand, 7 to 15 percent slopes53D71025420592qrbqil17119841:12000
Bloomfield fine sand, 1 to 7 percent slopes53B39125420582qrbnil17119841:12000
Bloomfield fine sand, 18 to 30 percent slopes53F20517970060zsil18519621:20000
Bloomfield fine sand, 1 to 5 percent slopes53B167415438641ntj2il19320061:12000
Bloomfield fine sand, 5 to 10 percent slopes53C112915438651ntj3il19320061:12000
Bloomfield fine sand, 10 to 18 percent slopes53D39415438661ntj4il19320061:12000
Bloomfield-Alvin loamy sands, 6 to 12 percent slopesBluC4402009166r25in00520021:12000
Bloomfield loamy fine sand, 4 to 12 percent slopesBmC37501624195g0bin01719791:15840
Bloomfield loamy fine sand, 25 to 50 percent slopesBmF4961595935c25in02119801:15840
Bloomfield loamy fine sand, 12 to 18 percent slopesBmD2871595925c24in02119801:15840
Bloomfield loamy fine sand, 6 to 12 percent slopesBlC44411629305gjtin02719691:20000
Bloomfield loamy fine sand, 2 to 6 percent slopesBlB17971629295gjsin02719691:20000
Bloomfield loamy fine sand, 12 to 18 percent slopesBlD17101629315gjvin02719691:20000
Bloomfield loamy fine sand, 18 to 35 percent slopesBlF11921629325gjwin02719691:20000
Bloomfield sand, 2 to 6 percent slopesBlB49651601075clrin05119861:15840
Bloomfield sand, 6 to 12 percent slopesBlC34371601085clsin05119861:15840
Bloomfield sand, 0 to 2 percent slopesBlA11811601065clqin05119861:15840
Bloomfield sand, 18 to 50 percent slopesBlF9721601105clvin05119861:15840
Bloomfield sand, 12 to 18 percent slopesBlD6621601095cltin05119861:15840
Alvin-Bloomfield complex, 2 to 6 percent slopesAnB31831615145f24in05519841:15840
Alvin-Bloomfield complex, 6 to 12 percent slopesAnC29621615155f25in05519841:15840
Bloomfield sand, 15 to 25 percent slopesBlE16331615235f2fin05519841:15840
Bloomfield sand, 35 to 60 percent slopesBlG5781615245f2gin05519841:15840
Bloomfield-Alvin complex, 6 to 15 percent slopes, erodedBkeC2264775650v13zin06120071:12000
Bloomfield-Alvin complex, 1 to 6 percent slopesBkeB6956190675522047in07119851:15840
Bloomfield-Alvin complex, 6 to 15 percent slopes, erodedBkeC26758190675622048in07119851:15840
Urban land-Bloomfield-Alvin complex, 1 to 6 percent slopesUfaB145819076662212min07119851:15840
Bloomfield fine sand, 15 to 45 percent slopesBlfF1325190675422046in07119851:15840
Urban land-Bloomfield-Alvin complex, 6 to 15 percent slopesUfaC46619076672212nin07119851:15840
Bloomfield loamy fine sand, 4 to 12 percent slopesBmC1697570111r97in07719821:15840
Bloomfield-Alvin complex, 1 to 6 percent slopesBkeB27709132rsx7in07920101:12000
Bloomfield loamy fine sand, 2 to 10 percent slopesBlB97131644675j4din08319791:15840
Bloomfield loamy fine sand, 12 to 18 percent slopesBlD16411644685j4fin08319791:15840
Bloomfield loamy sand, 3 to 10 percent slopesBlrC263716515301sfk5in09319821:15840
Bloomfield-Alvin complex, 1 to 6 percent slopesBkeB86716515511sfkvin09319821:15840
Alvin-Bloomfield loamy fine sands, 15 to 35 percent slopes complexAmoE1816514891sfhvin09319821:15840
Alvin-Bloomfield loamy fine sands, 4 to 10 percent slopes, eroded complexAmoC21516514881sfhtin09319821:15840
Alvin-Bloomfield loamy fine sands, 4 to 10 percent slopes, erodedAmoC2136514430681kfmlin10119841:15840
Alvin-Bloomfield loamy fine sands, 15 to 35 percent slopesAmoE111914430691kfmmin10119841:15840
Bloomfield loamy fine sand, 6 to 12 percent slopesBmC3471631975gtfin10919791:15840
Alvin-Bloomfield-Princeton complex, 18 to 25 percent slopesAffE5071658615klcin11919971:12000
Alvin-Bloomfield loamy sands, 6 to 12 percent slopesAfeC4731658595kl9in11919971:12000
Alvin-Bloomfield loamy sands, 12 to 18 percent slopesAfeD3141658605klbin11919971:12000
Bloomfield-Alvin complex, 6 to 15 percent slopes, erodedBkeC2603535695kzfhin12319971:12000
Alvin-Bloomfield complex, 6 to 15 percent slopesAoC17031618865fg4in12519831:15840
Bloomfield loamy fine sandy, 25 to 50 percent slopesBlF3461618955fgfin12519831:15840
Bloomfield loamy fine sand, 18 to 35 percent slopesBlF11351598815ccgin12919781:15840
Bloomfield loamy fine sand, 2 to 6 percent slopesBlB8131598785cccin12919781:15840
Bloomfield loamy fine sand, 6 to 12 percent slopesBlC6771598795ccdin12919781:15840
Bloomfield loamy fine sand, 12 to 18 percent slopesBlD4471598805ccfin12919781:15840
Bloomfield loamy fine sand, 6 to 12 percent slopesBlC28641626565g7zin15319661:15840
Bloomfield loamy fine sand, 2 to 6 percent slopesBlB28371626555g7yin15319661:15840
Bloomfield loamy fine sand, 12 to 18 percent slopesBlD8011626575g80in15319661:15840
Bloomfield loamy fine sand, 18 to 40 percent slopesBlF5931626585g81in15319661:15840
Bloomfield loamy fine sand, 4 to 12 percent slopesBmC267535263kyzkin15519841:15840
Bloomfield loamy fine sand, 2 to 6 percent slopesBlB17501596515c41in16719711:20000
Bloomfield loamy fine sand, 6 to 12 percent slopesBlC12681596525c42in16719711:20000
Bloomfield loamy fine sand, 12 to 18 percent slopesBlD4821596535c43in16719711:20000
Bloomfield loamy fine sand, 18 to 40 percent slopesBmF433535460kz5xin17519841:15840
Bloomfield loamy fine sand, 6 to 18 percent slopesBmC360535459kz5win17519841:15840

Map of Series Extent

Approximate geographic distribution of the BLOOMFIELD 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 .