节点文献

南黄海东部泥区沉积速率和物源探讨

DISCUSSION ON SEDIMENTATION RATES AND MATERIAL SOURCE IN THE EAST PART OF THE SOUTH YELLOW SEA

  • 推荐 CAJ下载
  • PDF下载
  • 不支持迅雷等下载工具,请取消加速工具后下载。

【作者】 李凤业; 杨永亮; 何丽娟; 史玉兰; 朴龙安; 崔镇勇;

【Author】 LI Feng-ye; YANG Yong-Liang; HE Li-Juan; SHI Yu-Lan; PARK Yong-Ahn; CHOI JinYong (Institute of Oceanology, Chinese Academy of Sciences,Qingdao 266071 ) (DepaTtment of Oceangraphy, Seoul National University, Seoul 151 - 742, Korea)

【机构】 中国科学院海洋研究所!青岛266071; 韩国汉城大学海洋研究所!汉城151-742;

【摘要】 根据测定岩芯中210Pb放射性活度,南黄海东部泥区最高现代沉积速率为1.65 cm/a,泥区边缘沉积速率为0.12cm/a。表层沉积物中的化学成分CaCO3,Cu,Sr,Ti和Rb的 含量表明黄河物源对该泥区没有影响,长江物源对该区贡献较小。

【Abstract】 The sedimentation rates in the east part of the South Yellow Sea were determined based on profiles of 210Pb in the cores. It ranges from 0. 12 to 1. 65 cm/a. In order to discuss material sources of fine-grained mud in the eastern South Yellow Sea, Chemical elements CaCO3,Sr,Cu,Ti and Rb have been determined. The contents of CaCO3 and Sr showed that the Huanghe River materials could hardly be transported to the eastern South Yellow Sea. The contents of Cu,Ti and Rb showed that parts of terrigenous materials from the Changjiang River were transported to the mud areas. This research was supported by the National Natural Science Foundation of China and Korea.

【基金】 中国自然科学基金;韩国科学工程基金!49576288
  • 【文献出处】 海洋科学 ,MARINE SCIENCES , 编辑部邮箱 ,1999年05期
  • 【分类号】P736.2
  • 【被引频次】28
  • 【下载频次】301
节点文献中: