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| 下载次数 | 被引频次 | 阅读次数 |
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。
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.
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基本信息:
DOI：10.16441/j.cnki.hdxb.1999.s1.023
中图分类号:P734
引用信息:
[1]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].青岛海洋大学学报(自然科学版),1999(S1):149-153.DOI:10.16441/j.cnki.hdxb.1999.s1.023.
基金信息:
国家自然科学基金
1999-12-30
1999-12-30