Official Series Description


Lab Data Summary

Aggregate lab data for the BLOOMINGDALE soil series. This aggregation is based on all pedons with a current taxon name of BLOOMINGDALE, 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 BLOOMINGDALE 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
12887P014486TN163 Bloomingdale-OSDBloomingdale7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties36.5733333,-82.435

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BLOOMINGDALE 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 BLOOMINGDALE 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 BLOOMINGDALE 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 BLOOMINGDALE 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 BLOOMINGDALE 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 BLOOMINGDALE series and competing. Series are sorted according to hierarchical clustering of median values. Source: SSURGO map unit geometry and 1981-2010, 800m PRISM data .

There are insufficient data to create the annual climate figure.

Geomorphic description summaries for the BLOOMINGDALE 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 .

There are insufficient data to create the 2D hillslope position figure.

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

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

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

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

Soil series sharing subgroup-level classification with BLOOMINGDALE, 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. TN-2010-11-02-21 | McMinn County - 2004

    lationship of soils and parent material in the Fullerton-Bodine-Rockdell and Coile-Apison-Sunlight general soil map units (Soil Survey of McMinn County, Tennessee; 2004).

  2. TN-2012-03-19-24 | McMinn County - 2004

    Relationship of soils and parent material in the Fullerton-Bodine-Rockdell and Coile-Apison-Sunlight general soil map units (Soil Survey of McMinn County, TN; 2004).

Map Units

Map units containing BLOOMINGDALE 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
Bloomingdale silt loam, 0 to 2 percent slopes, occasionally floodedBdA262316117911r368ga01520131:12000
Bloomingdale-Urban land complex, 0 to 2 percent slopes, occasionally floodedBnA12425542332qvpnga01520131:12000
Bloomingdale silt loam, pondedBm87025079422q784ga61920121:24000
Bloomingdale silty clay loam, occasionally floodedBd107526416kns5tn01920001:24000
Bloomingdale silty clay loam, frequently floodedBm370525011km9vtn05719961:24000
Bloomingdale-Hamblen complex, 0 to 3 percent slopes, occasionally floodedBh3392632836p7j2tn09320051:12000
Bloomingdale silt loam, 0 to 2 percent slopes, occasionally floodedBd2321632835p7j1tn09320051:12000
Bloomingdale silty clay loam, occasionally floodedBm4861526137knh5tn10719991:24000
Tupelo-Bloomingdale complex, 0 to 3 percent slopes, frequently floodedTu109914212391jpxftn12119681:15840
Bloomingdale-Tupelo complex, frequently floodedBm68315422541nrv4tn12119681:15840
Bloomingdale silty clay loam, frequently floodedBm1368728817sgd7tn14320031:24000
Bloomingdale silty clay loam, occasionally floodedBg15514743391lh5btn14520051:24000
Bloomingdale silty clay loam, 0 to 2 percent slopes, occasionally floodedBm3577530051kskftn16319911:20000
Bloomingdale silt loam, occasionally pondedBm2372524756km1mtn60620011:24000

Map of Series Extent

Approximate geographic distribution of the BLOOMINGDALE 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 .