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1985年6月初曾母暗沙水文气象印海面化学要素同步连续观测资料的分析结果表明,该海区海一气能量交换和海面化学要素含量的周日变化有如下特点:1).本海区海一气能量交换主要是田海洋传给大气;2)大气不稳定时,能显交換量增大,ΣCO_2含量减小,而大气稳定时则与此相反;3)活性硅酸盐含量的周日变化与能量交换量周日变化趋势一致;4)能量交换量的周日变化与NH_4-N含量的周日变化相似,与NO_3-N含量的周日变化趋势基本相反,该海区海一气能量交换不仅与水文气象条件和浮游植物活动有关,而且与海面化学要素含量有密切关系。
The results of the simultaneous and continuous observations of the chemical elements of the sea surface in Zengmu and Sham hydrometeoro- meteorological Indian in early June 1985 show that the variation of the sea-atmosphere energy exchange and the chemical composition of the sea surface has the following characteristics: 1) Mainly due to the ocean being transferred to the atmosphere; 2) when the atmosphere is unstable, the exchangeable amount increases obviously, the content of ΣCO_2 decreases, while the atmosphere stabilizes, on the contrary; 3) the daily change of active silicate and energy exchange The daily variation of the amount of energy exchange is similar to that of NH_4-N, but the trend of the daily variation of NO_3-N is basically the opposite. The exchange of sea-air energy in the sea area is not only related to the hydrological meteorological The conditions are related to phytoplankton activities and are closely related to the chemical composition of the sea surface.