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本文根据1984年2月—1985年2月在台湾海峡西部海域综合调查的资料,以季节收支法计算台湾海峡西海域溶解氧的海-气交换系数和交换速率,当秋冬季氧的交换系数出现负值、交换速率与现场现象产生矛盾时,本文用各季节自然增氧与耗氧速度的平衡运动趋势予以解释,最后,根据所计算出的氧交换系数估算了台湾海峡西部海域溶解氧的海-气交换通量,得出了氧在本海域从海水向大气的释放量比从大气溶入海水的量大得多的结论。
Based on the comprehensive survey of the western part of the Taiwan Strait from February 1984 to February 1985, the sea-to-air exchange coefficient and exchange rate of dissolved oxygen in the western Taiwan Strait were calculated by the Seasonal Income and Expenditure Act. When the coefficient of exchange of autumn-winter oxygen When there is a negative value, the exchange rate and the phenomenon of the scene contradict each other, this paper explains the trend of equilibrium movement of natural oxygen consumption and oxygen consumption rate in each seasons. Finally, based on the calculated oxygen exchange coefficient, the dissolved oxygen of western Taiwan Strait The result of the sea-air exchange flux shows that the release of oxygen from the seawater to the atmosphere in this area is much larger than the amount of oxygen dissolved into the seawater.