长江口泥沙的来源分析与数量计算的研究
A STUDY ON THE SOURCE AND QUANTITY OF SEDIMENT AT THE YANGTZE RIVER ESTUARY
Received date: 1988-02-01
Online published: 1989-01-15
林承坤 . 长江口泥沙的来源分析与数量计算的研究[J]. 地理学报, 1989 , 44(1) : 22 -31 . DOI: 10.11821/xb198901005
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,they are the coeffcients related to heavy minerals or clay minerals, By which the converging percentage of each of the supplying regions is calculated. The result of calculation shows that over 92.1% of silt and fine sand, 94.6% of clay sediment, come from the Yangtze River. The research shows that most sediments are deposited in the Yangtze River Estuary, the remainder to be transported to the southeast. As the converging percentage of the Yangtze River upstream (x1) is known and the total amount of sediment supply from Datong Station is also known (475.00 million tons per year), the amount of sediment at the Yangtze River Estuary is computed, which is 460.50 million tons per year. This numerical value agrees quite well with the value of 460.10 million tons per year by comparing with the topographic map of the Yangtze River Estuary in 1915 and in 1963.
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