Official Series Description


Lab Data Summary

Aggregate lab data for the BRINKLOW soil series. This aggregation is based on all pedons with a current taxon name of BRINKLOW, 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 BRINKLOW 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
14886P0384S1985MD031011Brinklow7Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.2550011,-77.3494415

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BRINKLOW 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 BRINKLOW 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 BRINKLOW 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 BRINKLOW 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 terrace figure.

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

Competing Series

Soil series competing with BRINKLOW 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 BRINKLOW 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 BRINKLOW 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 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 BRINKLOW, 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. MD-2010-09-07-03 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Mt. Airy-Glenelg-Blocktown general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  2. MD-2010-09-10-01 | Cecil County -

    Elsinboro-Delanco-Sassafras association (Soil Survey of Cecil County, Maryland).

  3. MD-2010-09-10-02 | Cecil County -

    Glenelg-Brinklow-Manor-Glenville association (Soil Survey of Cecil County, Maryland).

  4. MD-2010-09-10-06 | Howard County - 2008

    Relationship of soils, topography, and underlying material in the Occoquan-Brinklow-Glenelg general soil map unit (Soil Survey of Howard County, Maryland; 2008).

  5. MD-2010-09-10-08 | Howard County - 2008

    Relationship of soils, topography, and underlying material in the Glenelg-Manor-Glenville general soil map unit (Soil Survey of Howard County, Maryland; 2008).

  6. MD-2012-02-03-18 | Frederick County - 2002

    Relationship of soils, topography, and underlying material in the Mt. Airy-Glenelg-Blocktown general soil map unit (Soil Survey of Frederick County, Maryland; 2002).

  7. MD-2012-02-03-22 | Montgomery County - July 1995

    Typical pattern of soils in the Piedmont physiographic province in Montgomery County (Soil Survey of Montgomery County, Maryland; July 1995).

Map Units

Map units containing BRINKLOW 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
Brinklow channery loam, 15 to 25 percent slopesBkD235724798822v7gfde00320091:24000
Brinklow-Blocktown complex, 25 to 65 percent slopesBnF93024798832p7j7de00320091:24000
Brinklow channery loam, 25 to 65 percent slopes, very stonyBrvF22424798842p7j8de00320091:24000
Manor-Brinklow complex, 25 to 45 percent slopes, very rockyMdE2435324038852lpfpmd00520101:12000
Brinklow channery loam, 15 to 25 percent slopesBhD1336224036552v7gfmd00520101:12000
Brinklow channery loam, 8 to 15 percent slopesBhC475124036542v7ggmd00520101:12000
Brinklow channery loam, 3 to 8 percent slopesBhB333624036532v7h6md00520101:12000
Manor-Brinklow complex, 45 to 65 percent slopes, very rockyMdF238524811792p8w1md00520101:12000
Brinklow channery loam, 8 to 15 percent slopesBrC3619424957652v7ggmd01320101:12000
Brinklow channery loam, 15 to 25 percent slopesBrD2436324957642v7gfmd01320101:12000
Brinklow channery loam, 3 to 8 percent slopesBrB871524957632v7h6md01320101:12000
Brinklow channery loam, 25 to 45 percent slopesBrE521924957662v7h7md01320101:12000
Manor-Brinklow complex, 25 to 45 percent slopes, very rockyMcE90224960152ptmymd01320101:12000
Manor-Brinklow complex, 45 to 65 percent slopes, very rockyMcF65624960162ptmzmd01320101:12000
Manor-Brinklow complex, 15 to 25 percent slopes, very rockyMcD48924960142ptmxmd01320101:12000
Brinklow very channery loam, 25 to 65 percent slopes, very rockyBsF19824957672ptj3md01320101:12000
Brinklow channery loam, 15 to 25 percent slopesBkD141324407502v7gfmd01520091:12000
Brinklow channery loam, 25 to 65 percent slopes, very stonyBrvF48124407542mxt0md01520091:12000
Brinklow-Blocktown complex, 25 to 65 percent slopesBnF28924407512mxsxmd01520091:12000
Brinklow channery loam, 15 to 25 percent slopes, very stonyBrvD18024407532mxszmd01520091:12000
Brinklow channery loam, 8 to 15 percent slopes, very stonyBrvC7424407872mxv2md01520091:12000
Brinklow-Blocktown channery loams, 15 to 25 percent slopesBkD12902534913kym8md02120011:12000
Manor-Brinklow complex, 25 to 65 percent slopes, very rockyMkF2319793440vmmvmd02720041:12000
Brinklow channery loam, 15 to 25 percent slopesBrD13427928032v7gfmd02720041:12000
Brinklow-Blocktown channery loams, 25 to 65 percent slopesBtF595792804vlzbmd02720041:12000
Brinklow channery loam, 8 to 15 percent slopesBrC3217928022v7ggmd02720041:12000
Brinklow-Blocktown channery silt loams, 15 to 25 percent slopes16D17021533581kx79md03119891:15840
Brinklow-Blocktown channery silt loams, 8 to 15 percent slopes16C16897533580kx78md03119891:15840
Brinklow-Blocktown channery silt loams, 3 to 8 percent slopes16B12400533579kx77md03119891:15840
Manor-Brinklow complex, 25 to 65 percent slopes, very rockyMfF41724748622p298md03320091:12000
Brinklow-blocktown channery loams, 25 to 65 percent slopesByF6424552232ndvrmd03320091:12000
Brinklow channery loam, 8 to 15 percent slopesBwC3324552212v7ggmd03320091:12000
Brinklow channery loam, 15 to 25 percent slopesBwD824552222v7gfmd03320091:12000
Brinklow-Blocktown channery loams, 15 to 25 percent slopes complexByD624550482ndp3md03320091:12000
Brinklow channery loam, 25 to 35 percent slopesBkE15198448630ynfpa04519601:20000
Brinklow silt loam, 15 to 25 percent slopes33D3397189529221m6gva06120061:12000
Brinklow silt loam, 25 to 45 percent slopes33E1593189529421m6jva06120061:12000

Map of Series Extent

Approximate geographic distribution of the BRINKLOW 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 .