
Natural Resources
Conservation Service
Ecological site F128XY513WV
Mesic Limestone And Dolomite Uplands
Accessed: 05/19/2025
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): 128X–Southern Appalachian Ridges and Valleys
MLRA 128 falls into the East and Central Farming and Forest Region. This MLRA is in Tennessee (36 percent), Alabama (27 percent), Virginia (25 percent), and Georgia (12 percent). It makes up about 21,095 square miles (54,660 square kilometers).
Most of this MLRA is in the Tennessee Section of the Valley and Ridge Province of the Appalachian Highlands. The thin stringers in the western part of the area are mostly in the Cumberland Plateau Section of the Appalachian Plateaus Province of the Appalachian Highlands. A separate area of the MLRA in northern Alabama is in the Highland Rim Section of the Interior Low Plateaus Province of the Interior Plains. The western side of the area is dominantly hilly to very steep and is rougher and much steeper than the eastern side, much of which is rolling and hilly. Elevation ranges from 660 feet (200 meters) near the southern end of the area to more than 2,400 feet (730 meters) in the part of the area in the western tip of Virginia. Some isolated linear mountain ridges rise to nearly 4,920 feet (1,500 meters) above sea level.
The MLRA is highly diversified. It has many parallel ridges, narrow intervening valleys, and large areas of low, irregular hills. The bedrock in this area consists of alternating beds of limestone, dolomite, shale, and sandstone of early Paleozoic age. Ridgetops are capped with more resistant carbonate and sandstone layers, and valleys have been eroded into the less resistant shale beds. These folded and faulted layers are at the southernmost extent of the Appalachian Mountains. The narrow river valleys are filled with unconsolidated deposits of clay, silt, sand, and gravel.
Ecological site concept
This PES occurs dominantly in residuum or colluvium on uplands underlain by limestone or dolomite. Mixed hardwood forests will be most common. On limestone substrates where rock outcrop occurs or where soils are more shallow, barrens have been noted. They are an important conservation concern on this site.
Table 1. Dominant plant species
Tree |
(1) Quercus alba |
---|---|
Shrub |
(1) Rhamnus caroliniana |
Herbaceous |
Not specified |
Physiographic features
This PES occurs dominantly in residuum or colluvium on uplands underlain by limestone or dolomite.
Table 2. Representative physiographic features
Landforms |
(1)
Hill
(2) Interfluve (3) Ridge |
---|---|
Elevation | 459 – 3,287 ft |
Slope | 2 – 60% |
Water table depth | 60 in |
Aspect | N, S |
Climatic features
The average annual precipitation in most of this area is 41 to 55 inches (1,040 to 1,395 millimeters). It increases to the south and is as much as 66 inches (1,675 millimeters) at the highest elevations in east Tennessee and the northwest corner of Georgia. The maximum precipitation occurs in midwinter and midsummer, and the minimum occurs in autumn. Most of the rainfall occurs as high-intensity, convective thunderstorms. Snowfall may occur in winter. The average annual temperature is 52 to 63 degrees F (11 to 17 degrees C), increasing to the south. The freeze-free period averages 205 days and ranges from 165 to 245 days. It is longest in the southern part of the area and shortest at high elevations and at the northern end.
Table 3. Representative climatic features
Frost-free period (average) | 152 days |
---|---|
Freeze-free period (average) | 177 days |
Precipitation total (average) | 45 in |
Figure 1. Monthly precipitation range
Figure 2. Monthly average minimum and maximum temperature
Figure 3. Annual precipitation pattern
Figure 4. Annual average temperature pattern
Climate stations used
-
(1) SALTVILLE 1N [USC00447506], Saltville, VA
-
(2) TAZEWELL [USC00408868], Tazewell, TN
-
(3) PENNINGTON GAP [USC00446626], Pennington Gap, VA
-
(4) PULASKI 2 E [USC00446955], Pulaski, VA
-
(5) STAFFORDSVILLE 3 ENE [USC00448022], Pearisburg, VA
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(6) ROANOKE RGNL AP [USW00013741], Roanoke, VA
Influencing water features
This ecological site is not influenced by wetland or riparian water features.
Soil features
These soils formed dominantly in residuum or colluvium on uplands underlain by limestone or dolomite. The slopes range from 0 to 80 percent. They are moderately deep to very deep (20 to more than 60 inches) to bedrock, and range from moderately well to somewhat excessively drained. The available water capacity of these soils ranges from low to high. The depth to a seasonal high water table is more than 6 feet. They are not subject to flooding or ponding. The soil reaction ranges from extremely acid to moderately alkaline (pH from 3.5 to 8.4).
The soil series associated with this site are: Bland, Brushy, Caneyville, Chilhowie, Claiborne, Clarksville, Colbert, Collegedale, Dewey, Dunmore, Faywood, Frederick, Fullerton, Hagerstown, Minvale, Poynor, Talbott, and Watahala.
Parent Material Kind: Residuum, Colluvium, and Creep deposits.
Parent Material Origin: Limestone, Limestone (cherty), Limestone interbedded with sandstone, siltstone, or shale, Argillaceous limestone, and Limestone and dolomite.
Table 4. Representative soil features
Parent material |
(1)
Residuum
–
cherty limestone
(2) Colluvium – argillaceous limestone |
---|---|
Surface texture |
(1) Channery clay (2) Gravelly loam (3) Extremely gravelly sandy loam |
Drainage class | Moderately well drained to somewhat excessively drained |
Permeability class | Rapid |
Soil depth | 23 – 56 in |
Surface fragment cover <=3" | 1 – 9% |
Surface fragment cover >3" | 1 – 9% |
Available water capacity (0-40in) |
1.6 – 7.5 in |
Soil reaction (1:1 water) (0-40in) |
4.5 – 6.8 |
Subsurface fragment volume <=3" (Depth not specified) |
80% |
Subsurface fragment volume >3" (Depth not specified) |
57% |
Ecological dynamics
Two of the three available vegetation classification plots from the Virginia Department of Natural Heritage (VA-DNH) have the community listed as Dry-Mesic Calcareous Forest. The third available plot classifies it under Limestone / Dolomite Barren. The calcareous vegetation associated with this PES may be due to different mapunit components. This will be investigated in field projects in the future. For the purposes of this provisional description, we assume the vegetation is similar to the thermic equivalent ESD. That vegetation community is characterized by white oak and pignut hickory in the overstory. This may change under the mesic temperature regime. Ecological dynamics are also interpreted to be similar. Future field investigations are needed.
DeSelm had numerous vegetation plots on these soil map units in the following TN Counties: Claiborne, Bradley, Union, Loudon and Campbell. The plot in Loudon County is likely not representative since that is in the thermic temperature regime. Although he describes multiple forest types, the most common is dominated by white oak or other oaks (chestnut oak, "mixed oak", black oak, etc.) with other oaks or hickories as strong co-dominants. In one case, he describes "barren with probably planted schizachyrium", which was probably not in a natural state for this site. However, it does match the Natural Heritage data describing a barren. He also describes a few plots with calcareous oak species. That may be due to some spatial error or because (most likely) he was sampling on a bluff. On bluffs, where dolomite is exposed, more calcareous species can gain a foothold. He also describes hemlocks on bluffs. This has been observed in Anderson County, Tennessee close to the thermic/mesic temperature delineation. The presence of hemlock in that case is likely due to the proximity to Norris lake and the Clinch river. Sinkholes and other karst features may also be important on this site. Field investigations are needed.
In general this PES occurs as a mixed hardwood forest dominated by oak, hickory, beech and maple. In some cases, on areas with shallow soils, barrens can occur. Anthropogenic barrens are probably also important and native warm season grasses have been noted to occur. Grazing is an important past land-use. Depending on location, timber production could also be important.
State and transition model
More interactive model formats are also available.
View Interactive Models
Click on state and transition labels to scroll to the respective text
State 1 submodel, plant communities
State 2 submodel, plant communities
State 3 submodel, plant communities
State 1
Naturalized State-Upland Mixed Hardwood
The Naturalized State for this ecological site is characterized by a closed-canopy hardwood forest dominated by oaks. Tupliptree may be more common on these sites than on similar drier sites, indicating that fragment content is related to soil moisture. Tuliptree would be more competitive on sites with more available moisture while white oak, for example, would likely do better on drier sites. To maintain this state, the mixed hardwood species, especially oaks, must be present in multiple age classes. In most cases red maple, sugar maple and American beech are colonizing the midstory and understory. A species composition shift toward these more mesophytic species is widely recognized throughout the eastern United States (McEwan et al., 2011).
Dominant plant species
-
white oak (Quercus alba), tree
-
black oak (Quercus velutina), tree
-
southern red oak (Quercus falcata), tree
-
tuliptree (Liriodendron tulipifera), tree
Community 1.1
White oak-Black oak
This phase is dominated by oaks and hickories in the overstory, but mid-story composition is shifting toward more shade and moisture-loving species. The understory is relatively rich in herbaceous diversity (including vines) but tree regeneration overwhelmingly favors the shade-tolerant species. Oak regeneration is difficult and often requires management. Decisions should be made on-site, based on existing conditions. These conditions include acorn production, seedling establishment, and the amount of advanced regeneration from seedlings (Brose et al., 2013). Several types of management can be employed, including prescribed fire, mechanical and chemical competition control, site preparation, and planting. However, depending on the stand and its history, management for oak/hickory is typically intensive and often requires multiple treatments over time ( approximately 10-25 years), (Loftis, 2004). Without intensive management, in most cases, stands will naturally succeed to a more mesophytic forest type dominated by shade tolerant species (the maples and American beech). Dendroecology studies in nearby, very similar old-growth forest stands indicate that oak species have dominated stands for the past 300 years. They speculate that the recent proliferation of maples in the understory will inhibit the regeneration of oak and pine under the current disturbance regime (Hart et al., 2012a). Oak and hickory can regenerate in canopy gaps formed by uprooted trees, but only on very dry sites, indicating that gap-phase dynamics will favor maple overall (Hart and Kupfer, 2011).
Dominant plant species
-
white oak (Quercus alba), tree
-
black oak (Quercus velutina), tree
-
tuliptree (Liriodendron tulipifera), tree
Table 5. Soil surface cover
Tree basal cover | 3-5% |
---|---|
Shrub/vine/liana basal cover | 1-2% |
Grass/grasslike basal cover | 0-1% |
Forb basal cover | 0-1% |
Non-vascular plants | 0-1% |
Biological crusts | 0% |
Litter | 60-89% |
Surface fragments >0.25" and <=3" | 0-5% |
Surface fragments >3" | 2-15% |
Bedrock | 0% |
Water | 0% |
Bare ground | 0% |
Table 6. Woody ground cover
Downed wood, fine-small (<0.40" diameter; 1-hour fuels) | 0-5% |
---|---|
Downed wood, fine-medium (0.40-0.99" diameter; 10-hour fuels) | 0-5% |
Downed wood, fine-large (1.00-2.99" diameter; 100-hour fuels) | 0-7% |
Downed wood, coarse-small (3.00-8.99" diameter; 1,000-hour fuels) | 0-7% |
Downed wood, coarse-large (>9.00" diameter; 10,000-hour fuels) | 0-6% |
Tree snags** (hard***) | 0-1% |
Tree snags** (soft***) | 0-2% |
Tree snag count** (hard***) | 10 per acre |
Tree snag count** (hard***) | 20 per acre |
* Decomposition Classes: N - no or little integration with the soil surface; I - partial to nearly full integration with the soil surface.
** >10.16cm diameter at 1.3716m above ground and >1.8288m height--if less diameter OR height use applicable down wood type; for pinyon and juniper, use 0.3048m above ground.
*** Hard - tree is dead with most or all of bark intact; Soft - most of bark has sloughed off.
Table 7. Canopy structure (% cover)
Height Above Ground (ft) | Tree | Shrub/Vine | Grass/ Grasslike |
Forb |
---|---|---|---|---|
<0.5 | – | 11-20% | 0-1% | 0-5% |
>0.5 <= 1 | – | 1-20% | 0-2% | 1-5% |
>1 <= 2 | – | 0-5% | – | – |
>2 <= 4.5 | 1-5% | 1-5% | – | – |
>4.5 <= 13 | 1-5% | 1-5% | – | – |
>13 <= 40 | 2-25% | – | – | – |
>40 <= 80 | 2-45% | – | – | – |
>80 <= 120 | 30-75% | – | – | – |
>120 | 20-30% | – | – | – |
Community 1.2
Maple species-American beech
This community phase has not yet been attained in most cases because forests currently dominated by oaks and hickories are in transition. Without management or large-scale disturbance, stands will naturally succeed to more mesophytic species composition in the overstory and the oaks and hickories will lose their dominance over time. Small-scale gap dynamics caused by tree throws would likely be a natural part of this state and would favor the maple component in forest stands (Hart et al., 2012a). A recent study of red maple on the nearby Cumberland Plateau found that canopy accession strategy and climate-growth relationships are critical factors in the shift from state 1.1 to state 1.2 (Hart et al., 2012b). Red maples are gap-opportunists and can take advantage of smaller-scale disturbances such as tree-throws. Oaks in contrast, seem to have needed high frequency, intense disturbances to establish their current dominance in the forest. Red maples do best in times of cool, wet springs preceded by wet autumns and warm winters (Hart et al., 2012a). Depending on climate conditions in the coming years, the weather may or may not favor their continued establishment. Red maple might also cause local environmental changes that facilitate perpetuation of favorable conditions for regeneration such as modification of understory light levels and soil characteristics (Nowacki and Abrams, 2008). The denser canopies might reduce understory temperature and increase relative humidity, which would also favor the more shade-tolerant, moisture loving state (Alexander and Arthur, 2010). Prescribed burning is a management tool that may be used to reverse the trend. While it may be a useful tool in some cases and most likely in combination with other management approaches, using fire alone is unlikely to produce the desired results in most stands (Clark and Schweitzer, 2013).
Forest overstory. The forest overstory is dominated by mature maples and American beech. Tree throws create small-scale gap dynamics in the forest, which favor recruitment of the maples and in some cases, tuliptree. Oaks and hickories will always be a part of the species composition in this state, but will not be dominant.
Forest understory. Forest understory composition will be similar to community phase 1.1, dominated by native herbs, forbs, and vines. Shade tolerant trees will be present in the regeneration. Spring ephemeral wildflowers will be prolific in places.
Dominant plant species
-
American beech (Fagus grandifolia), tree
-
red maple (Acer rubrum), tree
-
sugar maple (Acer saccharum), tree
Pathway 1.1A
Community 1.1 to 1.2
Time (typically greater than 100 years) with little or no large-scale disturbance will favor shade-tolerant, late-successional species including sugar maple, red maple and American beech.
Pathway 1.2A
Community 1.2 to 1.1
Establish advanced oak regeneration (natural or planted) is critical to recruiting oak back into the overstory, but a combination of natural and managed steps will likely be required to favor oak. Depending on the residual stand, management recommendations might include timber stand improvement, mechanical or chemical treatment of unwanted species, and prescribed fire. Consult with a professional forester before implementing any management practice, especially the use of prescribed burning. Arthur et al. (2012) discusses conditions when fire should and should not be used in oak management.
Conservation practices
Prescribed Burning | |
---|---|
Tree/Shrub Site Preparation | |
Tree/Shrub Establishment | |
Upland Wildlife Habitat Management | |
Forest Trails and Landings | |
Forest Stand Improvement | |
Fuel Break | |
Forest Management Plan - Written | |
Forest Management Plan - Applied |
State 2
High-graded Forest State
Forests in the high-graded state have been logged using diameter-limit cutting methods, multiple times in most cases. As a result, most forest stands have undesirable species composition, low vigor, and poor health. The genetic quality of the forest has been depleted due to the best trees being taken out over time.
Community 2.1
American beech - Sugar maple/Sourwood - Sassafras
Canopies in the high graded state are generally thick enough to prevent adequate oak regeneration; more shade tolerant species such as red maple, sugar maple and American beech will predominate. Oak and hickory species that remain typically have low genetic timber quality, so white and northern red oak are noticeably absent in stands that have been high-graded multiple times.
Table 8. Ground cover
Tree foliar cover | 10-25% |
---|---|
Shrub/vine/liana foliar cover | 0-1% |
Grass/grasslike foliar cover | 0% |
Forb foliar cover | 0-1% |
Non-vascular plants | 0% |
Biological crusts | 0% |
Litter | 60-70% |
Surface fragments >0.25" and <=3" | 0% |
Surface fragments >3" | 2-5% |
Bedrock | 0% |
Water | 0% |
Bare ground | 0% |
Table 9. Canopy structure (% cover)
Height Above Ground (ft) | Tree | Shrub/Vine | Grass/ Grasslike |
Forb |
---|---|---|---|---|
<0.5 | 0-2% | 0-2% | – | 0-2% |
>0.5 <= 1 | 0-3% | 0-4% | – | 0-3% |
>1 <= 2 | 0-3% | 1-3% | – | 0-1% |
>2 <= 4.5 | 0-5% | 1-5% | – | – |
>4.5 <= 13 | 5-15% | 1-5% | – | – |
>13 <= 40 | 5-10% | 1-5% | – | – |
>40 <= 80 | 25-50% | – | – | – |
>80 <= 120 | 15-25% | – | – | – |
>120 | – | – | – | – |
State 3
Cleared Grassland State
This state represents a once-forested area now cleared for pasture. Most pastures are very old and have been established for a long time. Management practices focus primarily on maintaining healthy pasture conditions rather than new pasture establishment, although that is certainly an option. Balancing stocking rates, grazing rotation, and nutrient inputs are the primary management concerns. Forage species considered excellent for this site include the legumes alfalfa, ladino clover, and red clover. Cool season grasses rated as excellent include annual ryegrass, orchardgrass, tall fescue, timothy, and winter small grains. Warm season grasses rated as excellent include bermudagrass, big bluestem, caucasian bluestem, eastern gamagrass, indiangrass, little bluestem, switchgrass, pearl millet and sorghum sudangrass. Some species listed as excellent were not included in this description because they are known to have invasive tendencies and should be avoided if possible. In general, pasture management recommendations focus on maximizing desirable forage species to outcompete undesirable or weedy species. Production practices that result in overgrazing and low fertility levels favor emergence, propagation, and growth of weeds (Green et al., 2006). Effective pasture management includes the following practices: - maintaining proper soil pH and fertility levels - using controlled grazing practices - mowing at proper timing and stage of maturity - allowing new seedlings to become well established before use, and - renovating pastures when needed (Green et al., 2006). Perilla (Perilla frutescens) mint is an exotic, invasive weed that is a major problem in many pastures. In Tennessee, It causes more cattle deaths than any other toxic plant (Steckel and Rhodes, 2007). Keeping a ready supply of quality feed for farm animals in the late summer and early fall will help to minimize the risk to livestock. Cattle will not normally feed on perilla unless there is a shortage of other feed.
Community 3.1
Orchardgrass-tall fescue
The dominance of orchardgrass (Dactylis glomerata), red clover (Trifolium pratense), and tall fescue (Schedonorus arundinaceus) in this community phase indicate that nutrient levels are adequate, and grazing rotations are long enough to allow pasture plants to recover. Overstocking and infrequent pasture rotation will allow weedier species to invade, such as nimblewill and rush species.
Forest overstory. The overstory in the grassland state is minimal and consists of a few trees growing along the parameter of pastures, and scattered shade trees within pastures.
Forest understory. Pastures in good condition can be characterized by the MDWRV (G128XY021TN) forage suitability group (FSG) in Tennessee. Forage species rated as excellent for this site include the legumes alfalfa, ladino clover, and red clover. Cool season grasses rated as excellent include annual ryegrass, orchardgrass, tall fescue, timothy, and winter small grains. Warm season grasses rated as excellent include bermudagrass, big bluestem, caucasian bluestem, eastern gamagrass, indiangrass, little bluestem, switchgrass, pearl millet and sorghum sudangrass. Some species listed as excellent were not included in this description because they are known to have invasive tendencies and should be avoided if possible.
Table 10. Ground cover
Tree foliar cover | 0-2% |
---|---|
Shrub/vine/liana foliar cover | 0-2% |
Grass/grasslike foliar cover | 60-70% |
Forb foliar cover | 20-30% |
Non-vascular plants | 0% |
Biological crusts | 0% |
Litter | 0-5% |
Surface fragments >0.25" and <=3" | 0-3% |
Surface fragments >3" | 0-15% |
Bedrock | 0% |
Water | 0% |
Bare ground | 0-2% |
Community 3.2
Tall fescue-nimblewill
This community phase is transitional to a more degraded phase. While some desirable pasture plants are still present [e.g. tall fescue, white clover (Trifolium repens)], [Dallisgrass (Paspalum dilatatum), Crabgrass (Digitaria spp.) and other warm season plants], undesirable species such as nimblewill (Muhlenbergia schreberi), rush (Carex spp.), cinquefoil (Potentilla spp.), thistle (Cirsium spp.) and little barley (Hordeum pusillum) will begin to proliferate. Heavy grazing pressure may favor weedy species over grass (Rhodes and Phillips, 2012). Just removing or reducing livestock will not always be enough to restore desirable conditions after a point. Some type of nutrient improvement may also be needed.
Community 3.3
Multiflora rose-blackberry spp.
Pastures with a history of overgrazing can be susceptible to invasion by weedy plants, shrubs, and small trees if grazing pressure is reduced and nothing further is done to improve the site. Indicator plants for this phase include blackberry, broomsedge, and multi-flora rose. Clipping undesirable plants and adding nutrient input can help pastures in this phase recover. Using goats for grazing, mowing and applying herbicide can be useful for clearing unwanted plants.
Pathway 3.1A
Community 3.1 to 3.2
Overstocked pasture with infrequent rotation.
Pathway 3.2B
Community 3.2 to 3.1
Rotational grazing with a longer recovery period and higher grazing height; improved fertility.
Pathway 3.2A
Community 3.2 to 3.3
Overgrazed; low fertility
Pathway 3.3A
Community 3.3 to 3.2
Clipping pasture with nutrient improvement or controlled grazing.
Transition T1A
State 1 to 2
Selective harvesting and high grading multiple times degrades forest stand quality in terms of altered species composition, forest structure, and genetic fitness. Diameter limit cuts, incorrectly implemented, remove the biggest and best trees and leave those of lowest quality in terms of both timber and ecology.
Transition T1B
State 1 to 3
Forest clearing, herbicide application, and establishment of pasture plants, hay or crops will convert forested stands to a grassland state. Most pastures in this site are old and were converted many years ago.
Restoration pathway R2A
State 2 to 1
Implementing restoration practices should be determined strictly on a stand-by-stand basis as conditions may vary depending on the type and extent of past logging practices, the damage from wind, ice, or fire, and the presence or absence of invasive exotic plants. In general, a large scale disturbance such as a clear-cut would allow stand re-establishment over time. In some cases, planting desirable species (primarily oaks) could be merited. If planting is determined to be a viable option, competition control and protection from deer browse are important. Improved tree stock is recommended for the best results. Further management practices such as weed control, timber stand improvement, and thinning would likely be needed intermittently during stand re-establishment to achieve the desired result. NRCS conservation practice 666 is forest stand improvement (FSI) and could be utilized for this pathway.
Transition T2A
State 2 to 3
Forest clearing, herbicide application, and establishment of pasture plants, hay or crops will convert forested stands to a grassland state. Most pastures in this site are old and were converted many years ago.
Restoration pathway R3A
State 3 to 1
Abandoned pastures can revert to forest naturally, although the presence of invasive, exotic plants may prevent desirable species establishment. In the past, most of this ecological site has been cleared and grazed and then abandoned but invasive plants were not as prolific then. It is almost certain that some type of weed control will be needed in addition to the natural regeneration process. Additionally, planting desirable species can sometimes be merited. If this approach is attempted, improved tree planting stock, competition control and prevention of deer browse is recommended. Sites may need multiple treatments over time and monitoring is critical to successful restoration.
Additional community tables
Table 11. Community 1.1 forest overstory composition
Common name | Symbol | Scientific name | Nativity | Height (ft) | Canopy cover (%) | Diameter (in) | Basal area (square ft/acre) |
---|---|---|---|---|---|---|---|
Tree
|
|||||||
tuliptree | LITU | Liriodendron tulipifera | Native | 60–110 | 30–35 | 13–20 | – |
red maple | ACRU | Acer rubrum | Native | 13–29 | 5–25 | 3–4 | – |
black oak | QUVE | Quercus velutina | Native | 50–130 | 5–25 | 22–38 | – |
white oak | QUAL | Quercus alba | Native | 50–140 | 20–25 | 18–29 | – |
sugar maple | ACSA3 | Acer saccharum | Native | 13–75 | 5–10 | 7–16 | – |
southern red oak | QUFA | Quercus falcata | Native | 40–100 | 5–10 | 27 | – |
pignut hickory | CAGL8 | Carya glabra | Native | 13–15 | 0–5 | 0–2 | – |
American beech | FAGR | Fagus grandifolia | Native | 13–25 | 0–5 | 4–5 | – |
black cherry | PRSE2 | Prunus serotina | Native | 25–35 | 0–5 | 0–9 | – |
sourwood | OXAR | Oxydendrum arboreum | Native | 20–44 | 1–2 | 8–10 | – |
Interpretations
Supporting information
Other references
DeSelm, Hal. 1989 – 2009. Natural Terrestrial Vegetation of Tennessee (Vegetation Plot Data). Unpublished raw data. http://treeimprovement.utk.edu/DeSelmData/DataDSC.htm
Griffith, G.E., Omernik, J.M., and Azevedo, S.H., 1997, Ecoregions of Tennessee: Corvallis, Oregon, U.S. Environmental Protection Agency EPA/600R-97/022, 51 p.
Martin, William H. 1989. Forest patterns in the Great Valley of Tennessee. Journal of the Tennessee Academy of Science 64(3): 137 – 143.
Thornthwaite, Charles W. 1948. An approach toward a rational classification of climate. Geographical Review 38(1): 55-94.
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.
Vegetation plot data. 2015. Retrieved from: http://vegbank.org/vegbank/index.jsp
Vegetation community description. 2015.
Retrieved from: http://www.basic.ncsu.edu/segap/
Contributors
Belinda Esham Ferro
Rangeland health reference sheet
Interpreting Indicators of Rangeland Health is a qualitative assessment protocol used to determine ecosystem condition based on benchmark characteristics described in the Reference Sheet. A suite of 17 (or more) indicators are typically considered in an assessment. The ecological site(s) representative of an assessment location must be known prior to applying the protocol and must be verified based on soils and climate. Current plant community cannot be used to identify the ecological site.
Author(s)/participant(s) | |
---|---|
Contact for lead author | |
Date | 05/16/2025 |
Approved by | Matthew Duvall |
Approval date | |
Composition (Indicators 10 and 12) based on | Annual Production |
Indicators
-
Number and extent of rills:
-
Presence of water flow patterns:
-
Number and height of erosional pedestals or terracettes:
-
Bare ground from Ecological Site Description or other studies (rock, litter, lichen, moss, plant canopy are not bare ground):
-
Number of gullies and erosion associated with gullies:
-
Extent of wind scoured, blowouts and/or depositional areas:
-
Amount of litter movement (describe size and distance expected to travel):
-
Soil surface (top few mm) resistance to erosion (stability values are averages - most sites will show a range of values):
-
Soil surface structure and SOM content (include type of structure and A-horizon color and thickness):
-
Effect of community phase composition (relative proportion of different functional groups) and spatial distribution on infiltration and runoff:
-
Presence and thickness of compaction layer (usually none; describe soil profile features which may be mistaken for compaction on this site):
-
Functional/Structural Groups (list in order of descending dominance by above-ground annual-production or live foliar cover using symbols: >>, >, = to indicate much greater than, greater than, and equal to):
Dominant:
Sub-dominant:
Other:
Additional:
-
Amount of plant mortality and decadence (include which functional groups are expected to show mortality or decadence):
-
Average percent litter cover (%) and depth ( in):
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Expected annual annual-production (this is TOTAL above-ground annual-production, not just forage annual-production):
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Potential invasive (including noxious) species (native and non-native). List species which BOTH characterize degraded states and have the potential to become a dominant or co-dominant species on the ecological site if their future establishment and growth is not actively controlled by management interventions. Species that become dominant for only one to several years (e.g., short-term response to drought or wildfire) are not invasive plants. Note that unlike other indicators, we are describing what is NOT expected in the reference state for the ecological site:
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Perennial plant reproductive capability:
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The Ecosystem Dynamics Interpretive Tool is an information system framework developed by the USDA-ARS Jornada Experimental Range, USDA Natural Resources Conservation Service, and New Mexico State University.
Click on box and path labels to scroll to the respective text.