Flatwood
From Wikipedia, the free encyclopedia
Flatwood is a soil series with impaired drainage that occurs in the southeastern United States. Flatwood soils are upland soils formed from marine sediments. A shallow water table plays a role in soil formation; typically the water table is only a few feet deep and fluctuates during the year.[1] Flatwood soils are classified in USDA soil taxonomy as fine, mixed, semiactive, mesic Aquic Hapludults.[2]
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