• Solange Filoso,

  • Joseph Vallino,

  • Charles Hopkinson,

  • Edward Rastetter,

  • Luc Claessens

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      Respectively, Postdoctoral Scientist, Assistant Scientist, Senior Scientist, and Associate Scientist, Marine Biological Laboratory, Marine Biological Laboratory, 7 MBL Street, Woods Hole, Massachusetts 02543 (current address/Filoso: Department of Ecology and Evolutionary Biology, Cornell University, Ithaca, New York 14853); and Doctoral Candidate, Department of Geography, University of California-Santa Barbara, Ellison Hall 3611, Santa Barbara, California 93106–4060 (E-Mail/Filoso:

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    Paper No. 03052 of the Journal of the American Water Resources Association (JAWRA) (Copyright © 2004). Discussions are open until April 1, 2005.


ABSTRACT: Increased riverine nitrogen (N) fluxes have been strongly correlated with land use changes and are now one of the largest pollution problems in the coastal region of the United States. In the present study, the Hydrological Simulation Program-FORTRAN (HSPF) is used to simulate transport of N in the Ipswich River basin in Massachusetts and to evaluate the effect of future land use scenarios on the water quality of the river. Model results show that under a land use change scenario constructed with restrictions from environmental protection laws, where 44 percent of the forest in the basin was converted to urban land, stream nitrate concentrations increased by about 30 percent of the present values. When an extreme land use scenario was used, and 100 percent of the forest was converted to urban land, concentrations doubled in comparison to present values. Model simulations also showed that present stream nitrate concentrations might be four times greater than they were prior to urbanization. While pervious lands with high density residential land use generated runoff with the highest N concentrations in HSPF simulations, the results suggested that denitrification in the riparian zone and wetlands coupled with the hydrology of the basin are likely to control the magnitude of nitrate loads to the aquatic system. The simulation results showed that HSPF can predict the general patterns of inorganic N concentrations in the Ipswich River and tributaries. Nevertheless, HSPF has some difficulty simulating the extreme variability of the observed data throughout the main stem and tributaries, probably because of limitations in the representation of wetlands and riparian zones in the model, where N processes such as denitrification seem to play a major role in controlling the transport of N from the terrestrial system to the river reaches.