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Updated: Oct 7, 2025

Understanding Dissolved Organic Matter Biogeochemistry Through In Situ Nutrient Manipulations in Stream Ecosystems
Published on: October 29, 2016
Temporal Changes in Photoreducible Mercury, Photoreduction Rates, and the Role of Dissolved Organic Matter in
N J O'Driscoll1, T M Christensen2, E A Mann2
1Department of Earth & Environmental Science, Acadia University, Wolfville, NS, B4P 2R6, Canada. nelson.odriscoll@acadiau.ca.
Abstract:
Total photoreducible mercury [Hg(II)RED] and photoreduction rates in the surface waters of four lakes in Kejimkujik National Park, Nova Scotia were measured monthly over a summer. The percent of THg that was photoreducible [%Hg(II)RED] decreased significantly in two of the four lakes from early to late summer: North Cranberry (maximum 42% to minimum 14%) and Big Dam East (maximum 51% to minimum 6%). Hg(II)RED was found to have a linear relationship with THg for all combined site data. THg and Hg(II)RED were found to have positive linear relationships with DOC concentrations (R2 = 0.97; n = 36; p < 0.01 and R2 = 0.75; n = 36; p < 0.01, respectively). A smaller proportion of THg was found to be photoreducible with increasing DOC concentration.
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