ABSTRACT Rivers emit large amounts of greenhouse gases globally. The confluence area is a crucial component of the carbon cycle in inland waters. However, a comprehensive understanding of the characteristics and control of vertical greenhouse gas exchanges in confluence areas is still lacking. The fluxes of CH4 and CO2 in a typical confluence area in Northwest China (Yellow-Fen River) were measured using a flux-box-greenhouse gas analyzer in February 2023. Additionally, environmental and water quality parameters were measured to determine the changing characteristics and principal drivers of greenhouse gas emissions in the river confluence waters. The results showed that the CO2 and CH4 fluxes in the confluence area ranged from 94.89 to 326.29 and 1.47 to 3.89 mg m−2 h−1, respectively. The greenhouse gas emission intensity at the confluence surpassed that at the other sample points. Further analysis indicated that pH, chemical oxygen demand (COD), v (flow velocity), (dissolved organic carbon) DOC, (dissolved inorganic carbon) DIC and (dissolved total carbon) DTC were the key factors affecting greenhouse gas emissions in these areas. This study is important for understanding the characteristics of CO2 and CH4 fluxes in river confluence areas, and provides useful reference information for future research and prediction models.
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