Virginia Water Science Center

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Project Information

Number

Location

Project Contact
Gary Speiran,

USGS Collaborators


 

Hydrologic and Water-Quality Factors Affecting Habitat Restoration and Management of the Great Dismal Swamp

Problem and Implications

The Great Dismal Swamp National Wildlife Refuge (fig. 1) was established by Congress in 1974 to preserve 110,200 acres of unique, seasonally-flooded, wetland habitats threatened by development in the urbanizing Hampton Roads area of southeastern Virginia and by agricultural activities in northeastern North Carolina. The refuge, which is managed by the U.S. Fish and Wildlife Service (the Service), contains diverse types of wetland habitats. These wetlands are dissected by an extensive network of access roads and ditches constructed since 1763 to drain the wetlands and facilitate logging of the wetlands. This network has profoundly altered the flow of water through the refuge, thereby, changing the characteristics of many of these wetlands. The ditch network contains water-control structures (fig. 2) that can be used to control the flow of water through the ditches and manage the hydrology of the refuge so that selected wetland characteristics can be restored, maintained, and preserved.

Pocosin and similar wetlands containing a dense shrub layer, an open, mature-pine canopy, and few mid-story trees occur in a part of the refuge southeast of Lake Drummond, commonly referred to as “the Blocks” (fig. 1). Each Block consists of  approximately 1 square mile (640 acres) of wetlands bounded by ditches on all sides. Approximately 2,171 acres of these wetlands potentially can be restored, managed, and preserved to provide habitat suitable for reintroduction of the red-cockaded woodpecker (Picoides borealis) (U.S. Fish and Wildlife Service, 2004). The red-cockaded woodpecker (fig. 3) has been listed as a federally endangered species throughout its range since October 13, 1970. The current population of red-cockaded woodpeckers is estimated to be about three percent of the population present during initial European settlement. The red-cockaded woodpecker requires an open, mature pine forest with little mid-story vegetation for foraging habitat and for boring nesting cavities. Invading hardwood species, primarily red maple (Acer rubrum), however, are filling the mid-story and canopy in the Blocks and, therefore, must be harvested and prevented from returning so that this habitat can be restored, maintained, and preserved. Periodic fire also is one of the essential elements needed to maintain this type of habitat such that prescribed burning is one of the key management tools. Harvesting of the hardwoods and prescribed burns, therefore, will help restore, maintain, and preserve the pocosins as habitat needed by red-cockaded woodpeckers.

Management of water levels in the Blocks will be essential to the success of restoring, maintaining, and preserving these pine-forest habitats. To properly manage water levels in the Blocks, the interactions between water levels in the ditches and groundwater levels near the ditches and in the interior of the Blocks need to be studies and understood. Precipitation likely is the primary source of groundwater to the Blocks. Groundwater levels, therefore, can be managed partly by controlling water levels in the ditches by use of the water-control structures and hence, controlling the discharge of groundwater from the wetlands to the ditches. Controlling groundwater levels will help limit the tree species present and maintain sufficient soil moisture to protect the organic peat soils and tree and shrub roots during prescribed burns.

Removal of a large number of hardwoods from the Blocks, however, could appreciably reduce evapotranspiration rates and raise groundwater levels during the growing season. Roots of the pine trees likely have grown to depths adapted to current groundwater levels. With shallower groundwater levels, parts of the pond-pine root systems could remain in saturated soils throughout the growing season, thereby creating prolonged stress that could damage or kill some of these mature pine trees and severely damage the habitat that is to be restored. Such stress likely would reduce growth rates of surviving trees and could be reflected in tree growth rings. Such impacts need to be considered and the ability to mitigate them through management of the ditch system needs to be assessed.

Water quality also is thought to be a critical element of pocosins and similar systems. Precipitation typically is thought to be the only natural outside source of water to these systems and the atmosphere, therefore, is the primary source of nutrients (ombrotrophic). Because this nutrient supply is extremely limited, inputs from other outside sources could adversely alter the nutrient chemistry and budgets and other characteristics of these wetland systems. The ditches throughout the Blocks and sheet flow across the refuge could become significant transport pathways for nutrients, particularly if areas west of the refuge become developed for either agricultural or urban uses. A study of the hydrology and nutrient chemistry, therefore, is essential to the success of restoring, maintaining, and preserving the pine-forest habitat for the red-cockaded woodpecker.

Objectives

The objectives of this study are to identify 1) the relations between water levels in the ditches and groundwater levels near the ditches and in the interior of the Blocks, 2) possible relations between groundwater levels and tree growth rates, and 3) current nutrient chemistry and possible nutrient transport pathways in these wetlands. The study is being conducted by the U.S. Geological Survey (USGS), Virginia Water Science Center, in cooperation with the U.S. Fish and Wildlife Service.

Relevance and Benefits

This project is a part of the USGS efforts to assist other Department of the Interior agencies address management issues on Department of the Interior lands. By better understanding the link between hydrology and the various wetland habitats, the Service can better restore, manage, and preserve habitats critical to various species.

Approach

The study is being conducted prior to the harvesting of hardwoods in Block C1, one of the Blocks planned for restoration, so that hydrologic relations can be identified under undisturbed conditions. The block is bounded by Corapeake Ditch to the south, Western Boundary Ditch to the west, Sycamore Ditch to the north, and Myrtle Ditch to the east.

Groundwater levels and quality are being measured in clusters of three wells: one well in each cluster is open to the water table, one to the bottom of the surficial peat aquifer, and one to the sand aquifer underlying the peat aquifer. Clusters are located along two intersecting lines (transects) that extend from the ditch at the middle of one side of the block to the ditch at the middle of the other side of the block. Transects follow fire breaks that have been cut through the vegetation. Clusters are located next to each ditch, about 100 to 150  feet (ft) from each ditch, about 300 to 400 ft from each ditch, halfway from each ditch to the center of the block, and at the center of the block. Water levels in selected wells and at the ditch sites are being monitored continuously and being transmitted hourly for display as part of the “real time” data on the Science Center’s web page. Water levels in other wells are being measured periodically. Precipitation amounts are being measured at selected sites. Water levels in the ditches will be compared to groundwater levels throughout the year. The data analysis will compare seasonal, precipitation-caused, and diurnal changes differences in water-level changes in the ditches and the wells.

Trees near the sites of selected well clusters will be cored. Growth rings of these cores will be analyzed to determine variations in growth related to potential stresses. Rates will be compared to groundwater levels and precipitation during the study and historic precipitation data obtained from the site closest to the Blocks to identify relations of tree growth to groundwater levels.

Water-quality determinations will include a combination of field-determined characteristics and concentrations of nutrients, major ions, and isotopes of various constituents. Results of these chemical analyses will be used to evaluate the nutrient chemistry as it might affect nutrient availability under what likely is extremely reducing conditions. Water-quality combined with water-level data will help improve the understanding of the hydrology and determine likely nutrient sources.

REFERENCES

U.S. Fish and Wildlife Service, 2004, Environmental assessment for the red-cockaded woodpecker habitat enhancement and reintroduction at the Great Dismal Swamp National Wildlife Refuge, http://greatdismalswamp.fws.gov/pdf%20files/Final%20RCW%20EA.pdf
 

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