PLYMOUTH COUNTY, MASSACHUSETTS SOIL SURVEY UPDATE
Broadbrook Soils: Very deep, well drained soil formed in silty eolian sediments underlain by loamy dense glacial till. Broadbrook soils are on smooth, convex topslopes and upper sideslopes of drumlins and glaciated hills.
Link
to Official Series Description
Broadbrook Pedon Description 2334101
Broadbrook Pedon Description 2334102
Map Unit (s): 340B, 340C, 340D,
341B, 341C, 341D
Map Phases:
Taxonomic Classification:
Coarse - loamy, mixed, mesic, Oxyaquic Dystrochrepts.
Drainage Class: Well drained.
Parent Material: Eolian silt
and very fine sand underlain by dense glacial till.
Permeability: Moderate in
the solum, slow or very slow in the dense substratum.
Available Water Holding Capacity:
Moderate.
Soil Reaction: Very strongly
acid to moderately acid throughout. .
Depth to Bedrock: Greater than 65
inches.
Seasonal High Watertable: Depth:
2.5 to 4 feet.
Type: Perched
Months: January to May.
Hydrologic Group: C.
Hydric Soil: No.
Flooding/Ponding Potential: Frequency
and Type: None.
Potential Inclusions: Paxton
and Montauk soils are similar inclusions. Moderately well drained
Scituate, Birchwood, and Woodbridge soils are on concave slopes
and lower elevations. Poorly drained Norwell, Sippican, and
Ridgebury soils are in depressions and along drainageways.
Soil Suitability:
Agriculture: Map unit 340B is a prime farmland soil. Map units 340C, 341C and 341B are important farmland soils.
Woodland: Well suited for woodland.
Development: Major limitations related to slow permeability in the dense till substratum. Large surface and subsurface stones and boulders may interfere with excavation. Erosion hazards are likely during development, measures should be taken to prevent erosion.