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Photo-reduction of divalent mercury (Hg(II)) in waters plays a crucial role in the air-water change of Hg and biogeochemical cycle of Hg in general. As past studies on photo-reduction of Hg(II) have primarily centered on dissolved Hg species, the effects of normal particles on photo-reduction of Hg(II) continue to be largely unidentified, except the presumed light attenuating result through light absorption and scattering. Thinking about the prevalence of particulate Hg because of adsorpt