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东海冬、夏两季表层海水的二氧化碳分压
引用本文:张龙军,王彬宇,张经.东海冬、夏两季表层海水的二氧化碳分压[J].中国海洋大学学报(自然科学版),1999(Z1).
作者姓名:张龙军  王彬宇  张经
作者单位:青岛海洋大学化学化工学院!青岛,266003,青岛海洋大学化学化工学院!青岛,266003,青岛海洋大学化学化工学院!青岛,266003
摘    要:1997 年冬、1998 年夏在东海进行了两个航次的调查,采用气相色谱一喷洒式平衡器系统,现场测定了表层海水和大气的CO2 分压。东海表层海水CO2 分压受东海环流、生物活动、季节等因素影响而变化。冬季受垂直混合作用的影响,陆架区是CO2 的源;黑潮水是CO2 的汇,夏季受生物活动的影响,陆架区水系是CO2 的汇;黑潮及影响区域是CO2 的源。

关 键 词:东海  CO_2分压  碳循环

pCO_2 in the Surface Water of the East China Sea in Winter and Summer
Zhang Longjun,Wang Binyu,Zhang Jing.pCO_2 in the Surface Water of the East China Sea in Winter and Summer[J].Periodical of Ocean University of China,1999(Z1).
Authors:Zhang Longjun  Wang Binyu  Zhang Jing
Abstract:pCO 2 in the surface water and the atmosphere of the East China Sea are measured in situ by the G.C equilibrium system in two surveys carried in Winter 1997 and Summer 1998. pCO 2 in the sea water is influenced by current systems, biological activities and seasonal factors, in Winter, the coastal area and the Kuroshio are the source and sink of CO 2 respectivdy due to the influence of vertical mixing; in Summer, the situation becomes the inverse due to biological activities.
Keywords:East China Sea  partial pressure of CO_2  carbon cycle
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