Seasonal variations in the inorganic carbon system in the Pearl River (Zhujiang) estuary
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摘要
Seasonal variations in the inorganic carbon system in the Pearl River estuary are examined based on data from five surveys during the spring, summer, fall, and winter seasons. Both total dissolved inorganic carbon (DIC) and total alkalinity (TAlk) values in the freshwater end-members are high in the dry season (>2700 μmol kg−1 for DIC and >2400 μmol kg−1 for TAlk) and substantially lower in the wet season (DIC and TAlk were not, vert, similar1000 and 700 μmol kg−1, respectively). Riverine DIC flux and drainage basin weathering rates, however, are significantly higher in the wet season (611×109 mol yr−1 and 13.6×105 mol km−2 yr−1) than in the dry season (237×109 mol yr−1 and 5.3×105 mol km−2 yr−1).

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