4.8 Article

Basin-specific pollution and impoundment effects on greenhouse gas distributions in three rivers and estuaries

Journal

WATER RESEARCH
Volume 236, Issue -, Pages -

Publisher

PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.watres.2023.119982

Keywords

Carbon dioxide (CO2 ); Estuary; Eutrophication; Methane (CH4 ); Nitrous oxide (N2O); River impoundment

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There are uncertainties about the combined effects of pollution and impoundment on riverine greenhouse gas emissions. It is debated whether eutrophication can transform downstream estuaries into carbon sinks. This study combined surveys along three impounded rivers in Korea and samplings at estuarine sites to assess the human impacts on CO2, CH4, and N2O distributions. Results showed that pollution generated localized hotspots of GHGs in metropolitan areas, but the highest GHG levels in the upriver areas did not carry over into the estuary. CH4 levels were elevated in eutrophic reaches, indicating enhanced phytoplankton production. The study emphasizes the importance of considering specific pollution sources and impoundments when evaluating GHG distributions and estuarine carryover effects.
Large uncertainties exist regarding the combined effects of pollution and impoundment on riverine greenhouse gas (GHG) emissions. It has also been debated whether river eutrophication can transform downstream estuaries into carbon sinks. To assess human impacts on the riverine and estuarine distributions of CO2, CH4, and N2O, two source-to-estuary surveys along three impounded rivers in Korea were combined with multiple samplings at five or six estuarine sites. The basin-wide surveys revealed predominant pollution effects generating localized hotspots of riverine GHGs along metropolitan areas. The localized pollution effect was pronounced in the lower Han River and estuary adjacent to Seoul, while the highest GHG levels in the upper Yeongsan traversing Gwangju were not carried over into the faraway estuary. CH4 levels were elevated across the eutrophic middle Nakdong reaches regulated by eight cascade weirs in contrast to undersaturated CO2 indicating enhanced phytoplankton production. The levels of all three GHGs tended to be higher in the Han estuary across seasons. Higher summertime d(13)C-CH4 values at some Nakdong and Yeongsan estuarine sites implied that temperature-enhanced CH4 production may have been dampened by increased CH4 oxidation. Our results suggest that the location and magnitude of pollution sources and impoundments control basin-specific longitudinal GHG distributions and estuarine carryover effects, warning against simple generalizations of eutrophic rivers and estuaries as carbon sinks.

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