Official Series Description


Lab Data Summary

Aggregate lab data for the BROOKSIDE soil series. This aggregation is based on all pedons with a current taxon name of BROOKSIDE, 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 BROOKSIDE 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
126WVU0042S2002WV051005Brookside5Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties39.7672222,-80.6480556
n/aMS-0151977-OH119-015Brookside3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a
n/aJF-0191984-OH081-019Brookside3Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Propertiesn/a

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the BROOKSIDE 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 BROOKSIDE 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 BROOKSIDE 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 BROOKSIDE 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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Competing Series

Soil series competing with BROOKSIDE 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 BROOKSIDE 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 BROOKSIDE 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 flats position figure.

Soil series sharing subgroup-level classification with BROOKSIDE, 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. KY-2012-01-27-62 | Estill and Lee Counties - August 1974

    Pattern of soils and underlying material in the Shelocta-Brookside-Latham association (Soil Survey of Estill and Lee Counties, Kentucky; August 1974).

  2. KY-2012-02-01-29 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Rigley-Brookside-Steinsburg association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

  3. KY-2012-02-01-30 | Menifee and Rowan Counties and Northwestern Morgan County - December 1974

    Pattern of soils and underlying material in the Rigley-Cranston-Steinsburg association (Soil Survey of Menifee and Rowan Counties and Northwestern Morgan County, Kentucky; December 1974).

  4. OH-2012-02-16-14 | Belmont County - July 1981

    Typical pattern of soils in the Westmoreland-Lowell association (Soil Survey of Belmont County, Ohio; July 1981).

  5. OH-2012-02-16-15 | Belmont County - July 1981

    Typical pattern of soils in the Elkinsville-Nolin Variant-Brookside association (Soil Survey of Belmont County, Ohio; July 1981).

Map Units

Map units containing BROOKSIDE 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
Brookside silty clay loam, 35 to 60 percent slopes, bouldery690G10592005076qmzil15720011:12000
Brookside silty clay loam, 18 to 35 percent slopes, stony690F10422005066qmyil15720011:12000
Brookside-Rock outcrop complex, 30 to 75 percent slopesBrF6025552383ljstky19919691:12000
Brookside-Faywood-Rock outcrop complex, 30 to 65 percent slopesBxF12018552253ljnmky62819731:20000
Vandalia-Brookside complex, 15 to 25 percent slopesVbD15400537395l16boh00919811:15840
Brookside silt loam, 15 to 25 percent slopesBrD69805373442t31voh00919811:15840
Elba-Brookside-Berks complex, 40 to 70 percent slopesEbF4480537355l151oh00919811:15840
Vandalia-Brookside complex, 25 to 40 percent slopesVbE3630537396l16coh00919811:15840
Brookside silt loam, 25 to 40 percent slopesBrE1300537345l14qoh00919811:15840
Brookside silt loam, 8 to 15 percent slopesBrC4305373432t31woh00919811:15840
Brookside silty clay loam, 15 to 25 percent slopesBsD37255370632t31roh01319781:15840
Brookside silty clay loam, 25 to 40 percent slopesBsE27245370642t31toh01319781:15840
Brookside silty clay loam, 8 to 15 percent slopesBsC7835370622t31soh01319781:15840
Brookside-Urban land complex, 15 to 40 percent slopesBuD647537066l0vqoh01319781:15840
Brookside-Urban land complex, 3 to 15 percent slopesBuB576537065l0vpoh01319781:15840
Brookside-Vandalia complex, 15 to 25 percent slopesBtD4313536879l0npoh05919981:15840
Brookside-Vandalia complex, 25 to 40 percent slopesBtE543536880l0nqoh05919981:15840
Brookside silt loam, 15 to 25 percent slopes, erodedBsD235815929191qgkhoh05919981:15840
Brookside silt loam, 15 to 25 percent slopesBsD3405368772t31voh05919981:15840
Brookside-Vandalia complex, 8 to 15 percent slopesBtC189536878l0nnoh05919981:15840
Brookside silty clay loam, 8 to 15 percent slopes, erodedBrC211115929051qgk1oh05919981:15840
Brookside silty clay loam, 15 to 25 percent slopesBkD3715929152t31roh05919981:15840
Brookside silty clay loam, 25 to 40 percent slopesBkE3215929162t31toh05919981:15840
Brookside silty clay loam, 15 to 40 percent slopesBrE815929061qgk2oh05919981:15840
Brookside-Vandalia complex, 15 to 25 percent slopes, erodedBtD2215929201qgkjoh05919981:15840
Brookside silty clay loam, 15 to 25 percent slopesBsD685367222t31roh06719931:15840
Brookside silty clay loam, 25 to 40 percent slopesBsE1516954972t31toh06719931:15840
Brookside silty clay loam, 25 to 40 percent slopesBsE29245360632t31toh08119871:15840
Brookside silty clay loam, 15 to 25 percent slopesBsD14445360622t31roh08119871:15840
Brookside silty clay loam, 8 to 15 percent slopesBsC2445360612t31soh08119871:15840
Vandalia-Brookside complex, 15 to 25 percent slopesVbD1015274201n8dmoh10519911:15840
Brookside silt loam, 15 to 25 percent slopes, erodedBsD25214692431l9vyoh11119681:15840
Brookside silty clay loam, 15 to 25 percent slopesBtD2614692682t31roh11119681:15840
Brookside silty clay loam, 20 to 35 percent slopesBrE2975537425l179oh11519921:15840
Brookside silty clay loam, 12 to 20 percent slopesBrD1534537424l178oh11519921:15840
Vandalia-Brookside complex, 12 to 20 percent slopes, erodedVbD2344537469l18qoh11519921:15840
Brookside silty clay loam, 15 to 40 percent slopesBtE25015411301nqnwoh11519921:15840
Brookside silty clay loam, 15 to 40 percent slopesBsE1270537863l1pfoh11919891:15840
Brookside silty clay loam, 8 to 15 percent slopes, erodedBsC2843537862l1pdoh11919891:15840
Brookside silt loam, 15 to 25 percent slopes, erodedBsD23600536985l0s3oh12119861:15840
Brookside-Vandalia complex, 25 to 35 percent slopes, erodedBtE21300536987l0s5oh12119861:15840
Brookside-Vandalia complex, 15 to 25 percent slopes, erodedBtD21100536986l0s4oh12119861:15840
Brookside-Vandalia complex, 15 to 25 percent slopesBtD71114818001lqy0oh12119861:15840
Brookside silt loam, 8 to 15 percent slopes, erodedBsC2350536984l0s2oh12119861:15840
Brookside-Vandalia complex, 8 to 15 percent slopesBtC20314817991lqxzoh12119861:15840
Brookside-Vandalia complex, 25 to 40 percent slopesBtE11514818011lqy1oh12119861:15840
Brookside silt loam, 15 to 25 percent slopesBrD9314818172t31voh12119861:15840
Brookside silt loam, 8 to 15 percent slopesBrC1514818162t31woh12119861:15840
Brookside silt loam, 25 to 40 percent slopesBrE514818181lqyloh12119861:15840
Brookside silty clay loam, 18 to 25 percent slopesBsE1708536458l073oh16719731:15840
Brookside silty clay loam, 12 to 18 percent slopesBsD960536457l072oh16719731:15840
Brookside silty clay loam, 6 to 12 percent slopesBsC542536456l071oh16719731:15840
Brookside bouldery silty clay loam, 18 to 35 percent slopesBtF538536459l074oh16719731:15840
Brookside silt loam, 15 to 25 percent slopesBrD245116023132t31vwv05120071:12000
Brookside silt loam, 25 to 35 percent slopesBrE240216023121qsbhwv05120071:12000
Brookside silt loam, 8 to 15 percent slopesBrC43216023142t31wwv05120071:12000
Urban land-Brookside complex, 15 to 25 percent slopesUmD26716088461r048wv05120071:12000
Urban land-Brookside complex, 3 to 15 percent slopesUmC10416088441r046wv05120071:12000
Brookside silt loam, 3 to 8 percent slopesBrB77186260820j64wv05120071:12000
Brookside silt loam, 15 to 25 percent slopesBrD119116025452t31vwv60419701:12000

Map of Series Extent

Approximate geographic distribution of the BROOKSIDE 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 .