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Water-Resources Investigations Report 96-4048 |
SEDIMENT DEPOSITION IN LAKE CLARKE, LAKE ALDRED, AND CONOWINGO
RESERVOIR, PENNSYLVANIA AND MARYLAND, 1910-93
by Lloyd A.
Reed and Scott A. Hoffman
The Susquehanna River carries a significant amount of the sediment
and the nutrient load transported to the Chesapeake Bay. Three large
hydroelectric dams are located near the mouth of the Susquehanna
River. The three dams and associated reservoirs are Safe Harbor
(Lake Clarke) and Holtwood (Lake Aldred) in southern Pennsylvania
and Conowingo (Conowingo Reservoir) in northern Maryland. Two of
these reservoirs, Lakes Clarke and Aldred, have reached a state
of equilibrium with sediment transport in the river. The third,
Conowingo Reservoir, continues to accumulate sediment as well as
particulate organic nitrogen and particulate phosphorus. Bottom-elevation
surveys of Conowingo Reservoir made in 1959, 1990, and 1993 indicate
that the reservoir will reach equilibrium with sediment transport
of the river during the next 10 to 20 years. Data collected from
1985-89 indicate that the Susquehanna River transports about 1,780
million pounds of sediment, 147 million pounds of nitrogen, and
5.1 million pounds of phosphorus to the Chesapeake Bay during a
year of normal streamflow. Once equilibrium is reached in the Conowingo
Reservoir, these loads may increase to levels currently transported
by the river to the reservoirs, about 6,600 million pounds of sediment,
153 million pounds of nitrogen, and 9.1 million pounds of phosphorus
per year. These higher loads may effect progress made on reducing
nutrient loads and should be considered when planning future programs.
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