PLYMOUTH COUNTY, MASSACHUSETTS SOIL SURVEY UPDATE
Merrimac Soils: Very deep, somewhat excessively drained soil formed in glacial outwash. Merrimac soils are on broad areas of outwash plains and deltas; less extensive areas occur on glacial lake plains.
Link
to Official Series Description
S08MA023003 (Forested)
| S08MA023002
(Cropped) |
Merrimac Pedon
Description 2325401 |Merrimac Pedon
Description 2325402 |
Merrimac Pedon Description 2325403 |
Merrimac Pedon Description 2325404 |
Merrimac Pedon Description 2325405 |Merrimac Pedon Description 2325307
Map
Unit (s): 254A, 254B, 254C
Map
Phases:
Taxonomic
Classification: Sandy, mixed, mesic, Typic Dystrochrepts.
Drainage
Class: Somewhat excessively drained.
Parent
Material: Gravelly glacial fluvial deposits.
Permeability:
Moderately rapid or rapid in the solum and rapid or very rapid in
the substratum.
Available
Water Holding Capacity: Low.
Soil
Reaction: Extremely acid to moderately acid throughout.
Depth
to Bedrock: Greater than 65 inches.
Seasonal
High Watertable: Depth: greater than 5 feet.
Type: apparent.
Months:
Hydrologic
Group: A.
Hydric
Soil: No.
Flooding/Ponding
Potential: Frequency and Type: None.
Potential
Inclusions: Barnstable, Windsor, Hinckley and Carver soils
are similar inclusions. . Moderately well drained Sudbury and
Deerfield soils are on lower elevations. Poorly drained Wareham
and Pipestone soils are along drainageways.
Soil Suitability:
Agriculture: Map units 254A and 254B are prime farmland soil map units. 254C is an important farmland map unit. Irrigation is needed for optimal production.
Woodland: Well suited for woodland.
Development: Merrimac soils have few limitations for development. They are associated with aquifer recharge areas and measures should be taken to protect the aquifer.