Research Article
The application of an integrated biogeochemical model (PnET-BGC) to five forested watersheds in the Adirondack and Catskill regions of New York
Article first published online: 11 OCT 2004
DOI: 10.1002/hyp.5571
Copyright © 2004 John Wiley & Sons, Ltd.
Issue
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Hydrological Processes
Special Issue: Interrelationships between atmospheric deposition and landscape features of forest catchments in regulating surface water biogeochemistry
Volume 18, Issue 14, pages 2631–2650, 15 October 2004
Additional Information
How to Cite
Chen, L., Driscoll, C. T., Gbondo-Tugbawa, S., Mitchell, M. J. and Murdoch, P. S. (2004), The application of an integrated biogeochemical model (PnET-BGC) to five forested watersheds in the Adirondack and Catskill regions of New York. Hydrol. Process., 18: 2631–2650. doi: 10.1002/hyp.5571
Publication History
- Issue published online: 11 OCT 2004
- Article first published online: 11 OCT 2004
- Manuscript Accepted: 15 SEP 2003
- Manuscript Received: 10 JAN 2002
Funded by
- New York State Energy Research and Development Authority
- W.M. Keck Foundation
- US Environmental Protection Agency Clean Air Markets Division
- Abstract
- References
- Cited By
Keywords:
- acidic deposition;
- modelling;
- Adirondacks;
- Catskills;
- acid neutralizing capacity
Abstract
PnET-BGC is an integrated biogeochemical model formulated to simulate the response of soil and surface waters in northern forest ecosystems to changes in atmospheric deposition and land disturbances. In this study, the model was applied to five intensive study sites in the Adirondack and Catskill regions of New York. Four were in the Adirondacks: Constable Pond, an acid-sensitive watershed; Arbutus Pond, a relatively insensitive watershed; West Pond, an acid-sensitive watershed with extensive wetland coverage; and Willy's Pond, an acid-sensitive watershed with a mature forest. The fifth was Catskills: Biscuit Brook, an acid-sensitive watershed. Results indicated model-simulated surface water chemistry generally agreed with the measured data at all five sites. Model-simulated internal fluxes of major elements at the Arbutus watershed compared well with previously published measured values. In addition, based on the simulated fluxes, element and acid neutralizing capacity (ANC) budgets were developed for each site. Sulphur budgets at each site indicated little retention of inputs of sulphur. The sites also showed considerable variability in retention of NO3−. Land-disturbance history and in-lake processes were found to be important in regulating the output of NO3− via surface waters. Deposition inputs of base cations were generally similar at these sites. Various rates of base cation outputs reflected differences in rates of base cation supply at these sites. Atmospheric deposition was found to be the largest source of acidity, and cation exchange, mineral weathering and in-lake processes served as sources of ANC. Copyright © 2004 John Wiley & Sons, Ltd.

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