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秋季黄海和东海海域沉降颗粒物及其地球化学组成

倪建宇 张美 刘小涯 林以安

倪建宇, 张美, 刘小涯, 林以安. 秋季黄海和东海海域沉降颗粒物及其地球化学组成[J]. 海洋学报, 2006, 28(1): 158-162.
引用本文: 倪建宇, 张美, 刘小涯, 林以安. 秋季黄海和东海海域沉降颗粒物及其地球化学组成[J]. 海洋学报, 2006, 28(1): 158-162.
NI Jian-yu, ZHANG Mei, LIU Xiao-ya, LI Yi-an. Sinking particles and their geochemical compositions in the Huanghai and East China Seas in autumn[J]. Haiyang Xuebao, 2006, 28(1): 158-162.
Citation: NI Jian-yu, ZHANG Mei, LIU Xiao-ya, LI Yi-an. Sinking particles and their geochemical compositions in the Huanghai and East China Seas in autumn[J]. Haiyang Xuebao, 2006, 28(1): 158-162.

秋季黄海和东海海域沉降颗粒物及其地球化学组成

基金项目: 国家重点基础研究发展规划资助项目(G1999043704);国家自然科学青年基金资助项目(40206012)

Sinking particles and their geochemical compositions in the Huanghai and East China Seas in autumn

  • 摘要: 水体中的颗粒物对于海水中物质的迁移有着重要的作用,已有的研究表明,海水中溶解态元素和颗粒物之间的相互作用决定了微量元素和常量元素在海洋中的分布[1].虽然近岸水体只占全球海洋表面的小部分,但河流搬运的陆源物质最终将通过近岸水体进入外海,目前普遍认为海岸带在物质迁移过程中起着极为重要的过滤器作用[2~3].黄海和东海作为具有宽阔陆架的边缘海,每年大量来自陆地的物质在这里沉积、迁移,其海域内的沉降颗粒物不仅是陆源入海物质的主要组成部分,也是人类活动入海污染物的主要载体.
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出版历程
  • 收稿日期:  2004-03-19
  • 修回日期:  2005-06-13

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