Natural Resources
Conservation Service
Ecological site F122XY005KY
Moderately Deep Well Drained Uplands
Accessed: 11/13/2024
General information
Provisional. A provisional ecological site description has undergone quality control and quality assurance review. It contains a working state and transition model and enough information to identify the ecological site.
MLRA notes
Major Land Resource Area (MLRA): 122X–Highland Rim and Pennyroyal
MLRA 122 is in Tennessee (47 percent), Kentucky (43 percent), Indiana (7 percent), and Alabama (3 percent). It makes up about 21,530 square miles (55,790 square kilometers). Bloomington, Indiana, is in the small part of this area that extends into southern Indiana.
SOILS:
Many of the soils in this MLRA are Udalfs. The moderately deep to very deep, well drained, clayey soils formed in limestone residuum. They are dominantly in rolling to steep areas of the “Outer Basin” (Mimosa, Braxton, Gladdice, and Hampshire series) and the undulating to hilly areas of the “Inner Basin” (Talbott and Bradyville series). The most agriculturally productive soils are the very deep, well drained, clayey or loamy soils that formed in alluvium and/or loess over alluvium or limestone residuum in nearly level to undulating areas (Armour, Cumberland, Harpeth, Lomond, and Maury series). The less extensive soils generally are moderately well drained to somewhat poorly drained and formed in loamy or clayey alluvium and/or residuum (Byler, Capshaw, Colbert, and Tupelo series). This MLRA has a significant acreage of Mollisols. Shallow or moderately deep, well drained, clayey Udolls (Ashwood and Barfield series) formed in limestone residuum dominantly in rolling to steep areas. Very shallow, well drained, clayey Rendolls (Gladeville series) formed in limestone residuum dominantly in undulating to rolling areas of the “Inner Basin.” Very deep, well drained or moderately well drained Udolls (Arrington, Egam, Lynnville, and Staser series) and somewhat poorly drained or poorly drained Aquolls (Agee, Godwin, and Lanton series) formed in loamy or clayey alluvium derived from limestone on flood plains. Most of the remaining soils on flood plains are moderately well drained or well drained Udepts (Lindell and Ocana series). Udults are of small extent in this area. Most are very deep, well drained, and loamy and formed in gravelly colluvium or colluvium and the underlying residuum on steep hillsides (Dellrose soils). Rock outcrops are common on uplands.
BIOLOGICAL RESOURCES:
This area supports mixed oak forest vegetation. White oak, black oak, northern red oak, and some scarlet oak are the dominant tree species. Shagbark hickory, bitternut hickory, pignut hickory, and mockernut hickory also occur. Oak, blackgum, flowering dogwood, sassafras, Virginia pine, pitch pine, and shortleaf pine grow mostly on ridgetops.
(Excerpt from United States Department of Agriculture, Natural Resources Conservation Service. 2006. Land Resource Regions and Major Land Resource Areas of the United States, the Caribbean, and the Pacific Basin. U.S. Department of Agriculture Handbook 296.)
Classification relationships
Scientific Name: Southern Interior Low Plateau Dry-Mesic Oak Forest, Unique Identifier: CES202.898
Possible NatureServe Association(s):
white oak - black oak - hickory forest
Quercus velutina - Quercus alba - Carya (glabra, ovata) Forest, CEGL002076
Ecological site concept
Moderately Deep Well-Drained Uplands
MLRA 122
Ecological Dynamics:
This PES describes hypotheses based on available data of many different scales and sources. This PES also does not encompass the entire complexity or diversity of these sites. Field studies would be required to develop a comprehensive and science-based native plant restoration plan for these sites.
Ecological Dynamics
This PES describes an oak-hickory forest community on moderately-deep, well-drained, soils formed in residuum of limestone or interbedded limestone/shale.
The range of variation in plant composition on these sites vary mainly due to soil depth, available water, and aspect.
State 1. Forestland
Only two tree species can be selected for entry into the database as dominants; however, multiple tree species may be dominant on these sites and it will vary depending on aspect, soil depth, seed sources, management, and disturbance history.
Phase 1.1:
black oak – white oak / coralberry - Carolina buckthorn / bedstraw- bignonia
(Quercus velutina – Quercus alba / Symphoricarpos orbiculatus - Frangula caroliniana / Gallium spp. -Bignonia capreolata)
These sites are characterized by moderately-deep soils predominately influenced by parent materials of limestone, calcareous shale, or interbedded limestone and shale. Soil depths of 20 to 40 inches provide an adequate moisture and growing environment for a wide range of quality hardwood trees, including various species of oaks and hickories. White oak, black oak, shagbark hickory, chinkapin oak, and sugar maple are likely to be on these sites.
Remaining wooded sites on these soil are generally located on hillsides and ridges, and are oak-hickory or oak-hickory-sugar maple forests with a robust and diverse herbaceous layer. Understory species may include agrimony, bedstraws, black snakeroots, white snakeroot, Virginia creeper, bignonia, smooth Solomon's seal, and false Solomon's seal. The shrub layer usually consisted of coralberry, Carolina buckthorn, and/or northern spicebush.
Other States and phases are described in the Community Phase Data Section.
Table 1. Dominant plant species
Tree |
(1) Quercus velutina |
---|---|
Shrub |
(1) Symphoricarpos orbiculatus |
Herbaceous |
(1) Galium |
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