摘要
根据广东汕头湾泥沙实测资料的分析 ,石英百分含量随含沙量增大而减小 ,绝对含量却随含沙量增大而增加 ,并与含沙量有很好的相关关系 ,原因是随着含沙量的增大 ,细颗粒泥沙的含量增加较快 ,其使悬沙的平均粒径减小 ,而粗颗粒泥沙的百分含量变化正好相反。通过建立石英含量与含沙量和水位上涨率 (或下降率 )与含沙量之间的相关关系式 ,本文就汕头湾显损含沙量的年出现率及含沙量和石英含量的特征值进行了推算。
Based on the analysis of measured data in Shantou Bay, Guangdong province, there is a good interrelation between quartz component and suspended sediment concentration. With the increasing of suspended sediment concentration, the percentage of quartz decreases, while the amount of quartz material increases. The reason for this phenomenon is the number of fine grain size sediment goes up quickly with sediment concentration increasing, which reduces the median grain size of suspended sediment. By setting up relational expressions of quartz to sediment conncentration and the rising rate and descending rate of water level to sediment concentration, the year occurrence number of wearing sediment concentration and characteristic values of quartz and suspended sediment concentration are calculated.
出处
《泥沙研究》
CSCD
北大核心
2004年第4期51-55,共5页
Journal of Sediment Research
关键词
石英含量
含沙量
水位
汕头湾
quartz component
sediment concentration
water level
Shantou Bay