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Coupled chemical dynamics of North Branch carbonate and DIN systems were studied. Water residence time of ∼30 d enhances estuarine respiration and CaCO3 dissolution. The North Branch biogeochemistry contributes to Changjiang element export fluxes. Biogeochemical controls of pCO2 in inner Changjiang Estuary were better understood.
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The North Branch pCO2 distribution pattern is unique compared with many other estuaries where aquatic pCO2 normally declines with salinity increase. Furthermore, the biogeochemical additions of ammonium and alkalinity were identified in salinities between 4 and 16 in the North Branch. Based on field data analyses and simplified stoichiometric equations, we suggest that the relatively high North Branch pCO2 values and estuarine additions of dissolved inorganic nitrogen/carbon in the mid-salinity area were strongly associated with each other. These signals were primarily controlled by biogeochemical processes in the North Branch, combining biogenic organic matter decomposition (i.e. respiration), ammonia oxidation, CaCO3 dissolution, and CO2 degassing.
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This page is a summary of: Biogeochemical generation of dissolved inorganic carbon and nitrogen in the North Branch of inner Changjiang Estuary in a dry season, Estuarine Coastal and Shelf Science, October 2017, Elsevier,
DOI: 10.1016/j.ecss.2017.08.027.
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