A two-dimensional model of the movement of fluid mud in a high energy turbid estuary
A two-dimensional model of the movement of fluid mud in a high energy turbid estuary
复制标题
高能浑浊河口泥浆运动的二维模型
DOI：
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发表时间：
1988
期刊：
影响因子：
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通讯作者：
A. Cooper
中科院分区：
文献类型：
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作者：
N.W.M. Odd;A. Cooper
流体泥浆的运动被认为是世界上大多数位于泥泞河口的港口快速淤积的最可能原因。在过去，很难预测或量化这种额外的淤积，在某些情况下，这可能会使新港口扩建的年度和维护疏浚费用增加一倍。新模型模拟了悬浮泥浆、流体泥浆和沉降泥浆相之间的泥浆交换。利用该方法建立了塞文河口泥沙输运的中试模型。
The movement of fluid mud has been cited as the most likely cause of rapid siltation in the majority of the ports in the world located in muddy estuaries. In the past, it has been very difficult to predict or quantify this extra siltation, which may in some cases double the annual and maintenance dredging bill for a new port extension. The new model simulated the interchange of mud between the suspended mud, fluid mud and settled mud phases. The new modelling method was used to set up a pilot model of mud transport in the Severn Estuary.