河口
缺氧(环境)
营养物
环境科学
昼夜垂直迁移
中国海
海洋学
硝酸盐
磷
水文学(农业)
氧气
地质学
生态学
生物
化学
有机化学
岩土工程
作者
⎜Zhuoyi Zhu,Hui Wu,Sumei Liu,Ying Wu,Daji Huang,Jing Zhang,Guosen Zhang
标识
DOI:10.1016/j.marpolbul.2017.07.029
摘要
Large areas of hypoxia have been reported off The Changjiang Estuary and in the East China Sea. Five cruises, covering winter, spring, and summer, were carried out from 2007 to 2013 in this region, and in August 2013 (summer), an extensive hypoxic event (11,150 km2) was observed, which was characterized by an estimated bulk oxygen depletion of 5.1 million tons. A strong tidal impact was observed associated with the bottom oxygen depletion, with the periodicity of diel variations in dissolved oxygen being 12 h (i.e., similar to the tidal cycle). A conservative estimate of nutrient regeneration suggested that during the hypoxic event of August 2013, the amount of regenerated nitrogen (as nitrate) and phosphorus (as dissolved inorganic phosphorus) was 27,000–30,000 tons and 1300–41,000 tons, respectively. Estimates of the absolute (bulk) regenerated nutrient fluxes were much greater than the conservative estimates.
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