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]
See also
editReferences
edit- ^ "Natural Soils Landscape Positions Classifications: Flatwood Soils". Archived from the original on September 29, 2006. Retrieved September 14, 2007.
- ^ Official Series Description – FLATWOODS Series Archived 2008-09-28 at the Wayback Machine