
Project Information
Number
Location
Project Contact
Gary Speiran,
USGS Collaborators
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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.
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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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