长江口航道黏性原状土冲刷特性试验
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Experiment of scour characteristics of viscous undisturbed soil of the Yangtze River estuary channel
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    摘要:

    通过封闭有压矩形管槽的物理模型试验,对长江口航道底质淤泥质粉沙原状土进行冲刷试验,分析原状土的起动和冲刷特性,以及土样深度对土样冲刷效应的影响。结果表明,冲刷前后的泥沙沉积密度相当,冲刷后的土样含沙量较小,沉积密度略小于冲刷前。土样的临界起动切应力随着临界起动流速增大而增大,两者满足指数关系且函数拟合性较好。随着土样深度的增加,土样的冲刷率和冲刷系数均减小,这表明位于长江口航道的底质泥沙随着深度呈现不均匀的分布特征,深度越大的泥沙抗冲刷能力越强,深度越浅的泥沙颗粒组成越不稳定,容易被水流扰动冲刷。

    Abstract:

    Based on the physical model test of closed and rectangular flume with pressure,we carry out the scour test of undisturbed soil of silt in the channel of the Yangtze River estuary to analyze the starting and scour characteristics of undisturbed soil and the influence of the depth of soil sample on the scour effect of soil sample.The results show that the density of soil sample almost keeps constant before and after scouring,and because of a smaller proportion of sand in the eroded soil,the soil density after scouring performs slightly smaller. Besides,the critical incipient shear stress increases with the increasing critical incipient velocity,the two can satisfy the exponential relation with each other,and the fitting of function is excellent. When the depth of soil increases,both scour rate and scour coefficient decrease which illustrate the uneven distribution of bottom silt along the depth of the Yangtze River estuary channel,the deeper silt has a larger scouring resistance while surface silt has the more unstable the particle composition and is more easily to be eroded.

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黄健钧,陈国平,马洪蛟.长江口航道黏性原状土冲刷特性试验[J].水运工程,2020(9):40-44.

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  • 在线发布日期: 2020-09-02
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