CH4 production, oxidation and emission in a U.K. ombrotrophic peat bog: Influence of SO42− from acid rain
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2019, Science of the Total EnvironmentCitation Excerpt :As a predominant S species of biogenic S gases (Aneja et al., 1981, Aneja, 1990; Steudler and Peterson, 1984; Goldan et al., 1987), hydrogen sulfide (H2S) is both foul smelling and noxious (Barton et al., 2014), and has important impacts on atmospheric acid deposition, aerosol formation (Aneja, 1990; Bates et al., 1992; Cooper et al., 1987; Vet et al., 2014), and global climate change through its association with cloud formation and ‘solar dimming’ (Charlson et al., 1987; Lohmann and Feichter, 2005). The emission of H2S is also closely related to iron cycling, carbon mineralization, and methane emission (Johnston et al., 2014; Nedwell and Watson, 1995). H2S emitted from natural sources (4.42 Tg yr−1) is of the same order of magnitude as the anthropogenic emissions (3.30 Tg yr−1), and is one of the major sources of sulfur gases in the atmosphere (Watts, 2000), playing a significant role in the global sulfur cycle.
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2018, Science of the Total EnvironmentCitation Excerpt :Therefore, changes in vascular plant production and composition may be caused by even very small changes in the groundwater level (Wallen et al., 1988; Potvin et al., 2015). Increasing the groundwater level in peat soil will also increase its biological activity (Nedwell and Watson, 1995) and increase the diffusion of oxygen – O2 may penetrate as far as 2 cm below the water table (Benstead and Lloyd, 1994). From the discussion above, it can be concluded that the habitat degradation resulting from the drainage works on the peat-bogs in the Bieszczady Mts.
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