The development and application of a mass balance model for mercury (total,elemental and methyl) using data from a remote lake (Big Dam West,Nova Scotia,Canada) and the multi-species multiplier method |
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Authors: | A.L.M. Ethier,D. Mackay,L.K. Toose-Reid,N.J. O&rsquo Driscoll,A.M. Scheuhammer,D.R.S. Lean |
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Affiliation: | 1. Biology Department, Centre for Advanced Research in Environmental Genomics, Faculty of Science, University of Ottawa, P.O. Box 450, Stn. A., Ottawa, ON, Canada K1N 6N5;2. Canadian Environmental Modelling Centre, Trent University, 1600 West Bank Dr., Peterborough, ON, Canada K9J 7B8;3. Department of Earth & Environmental Sciences, K.C. Irving Environmental Science Center, Acadia University, Wolfville, NS, Canada B4P 2R6;4. Environment Canada, National Wildlife Research Centre, Carleton University, 1125 Colonel By Dr., Raven Road, Ottawa, ON, Canada K1A 0H3 |
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Abstract: | Big Dam West, located in Kejimkujik Park, Nova Scotia, Canada, is a remote lake with elevated Hg concentrations in fish due in part to low pH and high dissolved organic carbon (DOC) concentrations. These features reflect the poor buffering capacity of peat lands in the flat drainage basin. To address the multiple species of Hg, a model was developed by coupling the “multiplier method” for multi-species chemicals with average concentration ratios to the Quantitative Water Air Sediment Interaction (QWASI) model. Elemental Hg was the “key species” modeled. Total Hg fluxes and concentrations were computed using concentration ratios. Many of the concentrations and Hg flux processes within the Big Dam West catchment had been previously measured with concentration ratios that were either computed or taken from the literature when measured data were not available. Measured values for total Hg concentration in each compartment (air, water, sediment) and Hg fluxes (e.g., precipitation, sediment deposition) enable verification of model concentration and flux estimates for total Hg in each environmental compartment. The model was also run with and without the inclusion of upward Hg fluxes from the underlying sediment to determine the significance of this controversial flux. The Hg QWASI model presented in this paper could be a valuable screening tool, especially for remote lakes, due to its ability to provide reasonable Hg estimates with a limited amount of data (water inflow rate, suspended particulate matter, sediment deposition velocity, and concentration of Hg in atmosphere and inflow water). |
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