Official Series Description


Lab Data Summary

Aggregate lab data for the WESTBROOK soil series. This aggregation is based on all pedons with a current taxon name of WESTBROOK, 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 WESTBROOK 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
144A08N0702S2008CT011002Westbrook6Primary | Supplementary | Taxonomy | Pedon | Water Retention | Correlation | Andic Soil Properties41.3382492,-71.8756104

Water Balance

Monthly water balance estimated using a leaky-bucket style model for the WESTBROOK 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 WESTBROOK 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 WESTBROOK 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 WESTBROOK 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 WESTBROOK 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 WESTBROOK 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 WESTBROOK 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 hills figure.

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

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

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Soil series sharing subgroup-level classification with WESTBROOK, 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. MA-2012-02-02-01 | Essex County, Northern Part - February 1981

    Typical pattern of soils and parent material in the Ipswich-Westbrook-Udipsamments association (Soil Survey of Essex County, Massachusetts, Northern Part; February 1981).

Map Units

Map units containing WESTBROOK 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
Westbrook mucky peat, 0 to 2 percent slopes, very frequently flooded98491633958632tyqfct60120031:12000
Westbrook mucky peat, low salt99132333958649ls8ct60120031:12000
Westbrook mucky peat, low salt99266934002379ls8ct60220031:12000
Westbrook mucky peat, 0 to 2 percent slopes, very frequently flooded98199634002362tyqfct60220031:12000
Westbrook mucky peat, 0 to 2 percent slopes, very frequently flooded62A6642770602tyqfma60219761:20000
Ipswich and Westbrook mucky peats, 0 to 2 percent slopes, very frequently flooded712A96887904082tyqnma60519771:15840
Ipswich and Westbrook mucky peats, 0 to 2 percent slopes, very frequently flooded712A82717910922tyqnma60619811:15840
Westbrook mucky peat, 0 to 2 percent slopes, very frequently flooded5975252793542tyqfnh01519861:24000
Westbrook, Ipswich, and Sandyhook soils, 0 to 2 percent slopes, very frequently floodedTrkAv280014452222tyqhnj00319861:24000
Westbrook mucky peat, 0 to 2 percent slopes, very frequently floodedWectA192725153672tyqfnj01720121:12000
Westbrook, Ipswich, and Sandyhook soils, 0 to 2 percent slopes, very frequently floodedTrkAv52414440882tyqhnj03919891:24000
Westbrook mucky peat, sandy substratum, 0 to 1 percent slopes, very frequently floodedWbA1225891772dv2kny00520141:12000
Westbrook mucky peat, sandy substratum, 0 to 1 percent slopes, very frequently floodedWbA14122295992dv2kny08520141:12000

Map of Series Extent

Approximate geographic distribution of the WESTBROOK 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 .