PLYMOUTH COUNTY, MASSACHUSETTS SOIL SURVEY UPDATE
Swansea Soils: Very deep, level, very poorly drained soil formed in 16 to 51 inches of highly decomposed organic material overlying glacial sediments. Swansea soils are in depressions, kettles or in low level areas of outwash plains and uplands.
Link to Official Series Description
Swansea Pedon Description 2305901
Swansea Pedon Description 2305101
Swansea Pedon Description 2305102
Map
Unit (s): 051, 060
Map
Phases:
Taxonomic
Classification: Sandy or sandy skeletal, mixed, dysic mesic,
Terric Medisaprists.
Drainage
Class: Very poorly drained.
Parent
Material: Swansea soils formed in 16 to 51 inches of organic
material underlain by fluvial or lacustrine sediments.
Permeability:
Moderate or moderately rapid.
Available
Water Holding Capacity: High.
Soil
Reaction: pH is less than 4.5 in 0.01 molar calcium chloride.
Depth
to Bedrock: Greater than 65 inches.
Seasonal
High Watertable: Depth: +2.5 to 0.5 feet below the
surface. Type: Apparent.
Months: January to December.
Hydrologic
Group: D.
Hydric
Soil: Yes.
Flooding/Ponding
Potential: Frequency and Type: Frequently ponded. Duration
and Months: Long to very long, November to May.
Map unit 060 is periodically flooded throughout the year
for cranberry management practices.
Potential
Inclusions: Very poorly drained Scarboro, Berryland, and
Freetown soils are similar inclusions. Poorly drained Wareham,
Saugatuck and Pipestone soils are on higher elevations.
Soil Suitability:
Agriculture: Poorly suited for most agricultural uses mainly due to wetness. Map unit 060 is important/unique farmland for cranberry production.
Woodland: Poorly suited due to wetness. Swansea soils have a sever limitation for tree throw hazard.
Development: Poorly suited due to seasonal high watertables at or near the surface for prolong periods of time. Organic layers have very low strength and should be removed to support loads.
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