| 长江入海泥沙的扩散 |
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| 引用本文： | 蔡爱智. 长江入海泥沙的扩散[J]. 海洋学报, 1982, 4(1): 78-88. |
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| 作者姓名： | 蔡爱智 |
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| 作者单位： | 中国科学院海洋研究所 |
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| 摘 要： | 长江是我国和亚洲第一大河、世界第三大河.据大通水文站观测,长江年总径流量平均为9,950亿公方,平均流量为30,2O0公方/秒,最大洪峰流量为92,600公方/秒,最小枯水流量为6,020公方/秒.平均含沙量为0.518克/公升,年输沙量平均为4.8亿吨[1].
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| 收稿时间： | 1979-05-28 |
DIFFUSION OF SEDIMENTS OF THE CHANGJIANG RIVER DISCHARGING INTO THE SEA |
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| Cai Aizhi. DIFFUSION OF SEDIMENTS OF THE CHANGJIANG RIVER DISCHARGING INTO THE SEA[J]. Haiyang Xuebao, 1982, 4(1): 78-88. |
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| Authors: | Cai Aizhi |
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| Affiliation: | Institute of Oceanology, Academia Sinica, Qingdao |
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| Abstract: | The diffusion of sediments of the Changjiang River(Yangtze River) flowing into the sea is an important subject in the study of oceanography of china, and a more important object for marine deposit and development of the coast of the East China Sea. |
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