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The U.S. Geological Survey (USGS), in cooperation with the Maryland Department of the Environment, the Metropolitan Washington Council of Governments, and the Virginia Department of Environmental Quality, is studying the amount of nutrient pollution that enters Chesapeake Bay annually from its major tributaries (fig. 1). Results of the study are used to determine whether steps taken to reduce the amount of pollution entering the Bay are working.
1 Figure 1. Location of major tributaries to Chesapeake Bay and sample sites and trends in nitrogen and phosphorus levels in each tributary.
The largest amount of nitrogen entering the Bay is contributed by the Susquehanna River, which drains some of the most productive agricultural land in the Nation. The sources of nutrient pollution from agricultural land are fertilizer and animal waste. In general, the amount
of nitrogen entering the Bay from each tributary is related to the area of agricultural land drained by that tributary and its contribution of water to the Bay.
Approximately 30 million pounds of phosphorus entered the Bay from its nine major tributaries from 1990 through 1992. About 90 percent of that amount came from the Susquehanna, the Potomac, and the James Rivers (fig. 2). The levels of phosphorus from the Potomac and the smaller rivers are related to their contribution of water to the Bay. Phosphorus levels entering the Bay from the Susquehanna River are low in comparison to its water contribution. Phosphorus, which is bound to soil particles, gets trapped behind a series of dams in the river. The high level of phosphorus entering the Bay from the James River compared to its water contribution may be related to discharge from sewage-treatment plants.
Pollution-reduction strategies are having a positive impact on phosphorus levels in the Susquehanna, the Potomac, and the Patuxent Rivers. Controls directed at reducing agricultural and urban erosion also contribute to the lower phosphorus levels seen in these tributaries.
Despite the success of phosphorus-reduction efforts in the Susquehanna, the Potomac, and the Patuxent Rivers, nitrogen is increasing in the Susquehanna and the Potomac Rivers, although the data indicate that the rate of increase has slowed significantly. The increase in nitrogen is probably caused by the continued use of nitrogen fertilizer on lawns and cropland, growing agricultural animal populations and associated wastes, and atmospheric deposition of nitrogen from industrial and automotive air pollution. Much of the nitrogen from these sources dissolves in water and slowly moves underground through the soil and into the ground water, where it discharges into rivers and eventually the Bay. The effect of nitrogen reduction may take decades to see because of the slow movement of nitrogen in the ground water. As a result, the effect of nitrogen-control efforts will take much longer to appear in the rivers than the effects of controlling phosphorus, which is attached to soil particles and is transported primarily in surface-water runoff. In the case of the Patuxent River, nitrogen is decreasing primarily because of improved technology at the eight major sewage-treatment plants that discharge to the river.
Although progress has been made in reducing phosphorus and nitrogen in some rivers, continued reductions will have to be made to offset increases in population growth in the Chesapeake Bay Basin. Continued water-quality monitoring of the rivers will be needed to assess the effectiveness of new technology and strategies aimed at reducing nutrient pollution, thereby restoring the economic, commercial, and recreational productivity of Chesapeake Bay.
---Linda D. Zynjuk
Figure 2. Relative contributions of flow and nutrient load from tributaries entering Chesapeake Bay, 1990--92.
from U.S. Department of the Interior, U.S. Geological Survey, Fact Sheet FS-055-95