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探讨海气间二氧化碳的气体交换。指出海面气体交换的物理过程与大气的强迫作用有关。动力学分析表明：交换速度主要依赖于溶解度、摩擦速度和阻碍系数；海面通量则决定于海与气的浓度差和交换速度，而交换速度随风速增加而增大，随温度增大而减小，其模拟值与风洞实验值基本一致。根据１９９３年１０月、１９９４年４月和１０月在东海三个航次的测定和计算表明，东海海面的二氧化碳通量指向下，其平均值为－４５．５μｇ·ｍ－２ｈ－１
Explore gas exchange between carbon dioxide in the sea. It is pointed out that the physical process of sea gas exchange is related to the forcing effect of the atmosphere. The kinetic analysis shows that the exchange rate mainly depends on the solubility, the friction speed and the obstruction coefficient. The sea flux depends on the concentration difference and the exchange rate between the sea and the gas, while the exchange rate increases with the increase of the wind speed. Small, the simulation value and the wind tunnel experimental values are basically the same. Based on the measurements and calculations of three voyages in the East China Sea in October 1993, April and October 1994, the CO 2 fluxes of the sea surface of the East China Sea point down with an average of -45.5 μg · m -2 h -1