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- W2002188020 abstract "connectivity to stream water. The volatilization rate of elemental mercury (Hg o )i n the beaver meadow wetland is of similar magnitude compared to total atmospheric Hg deposition and constitutes an important component of the overall annual Hg budget. In contrast, annual Hg o fluxes exhibited net transfer from the atmosphere to soil at the riparian wetland possibly because volatilization rates were retarded by slower diffusion of Hg o through soil to the air-water interface in water-saturated soil. The storage of THg and MeHg in wetland soil is a large pool which appears coupled with carbon and sulfur accumulation. In the current scenario of decreasing Hg emissions and atmospheric deposition, the large ‘‘active’’ soil pool in wetlands is a potential short-term and long-term source of Hg and MeHg to downstream aquatic ecosystems." @default.
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- W2002188020 date "2008-06-01" @default.
- W2002188020 modified "2023-10-18" @default.
- W2002188020 title "Inputs, storage, and transport of total and methyl mercury in two temperate forest wetlands" @default.
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- W2002188020 doi "https://doi.org/10.1029/2008jg000739" @default.
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