长江入海泥沙的扩散
DIFFUSION OF SEDIMENTS OF THE CHANGJIANG RIVER DISCHARGING INTO THE SEA
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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].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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