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作 者:Jun-De Li Jian Sun Binliang Lin
机构地区:[1]College of Engineering and Science, Victoria University [2]State Key Laboratory of Hydroscience and Engineering,Tsinghua University
出 处:《International Journal of Sediment Research》2018年第2期126-136,共11页国际泥沙研究(英文版)
基 金:supported financially by the National Key Research and Development Program of China (2016YFA0600901);the program of State Key Laboratory of Hydroscience and Engineering, Tsinghua University(2015-ky-02)
摘 要:A function for the bed-load sediment transport rate is derived. This function is obtained by using the entrainment probabilities of the rolling and lifted sediment grains, and by introducing two travel lengths,respectively. The predictions from the new bed-load function agree well with experimental results over the entire experimental range and show significant improvement over the commonly used formula for the bed-load transport rate. The new function shows that, in terms of contributing to the bed-load transport rate, the total entrainment probability of the sediment grains is a weighted summation of those for the lifted and rolling grains, rather than a simple addition of the two. The function is also used to predict the total entrainment probability, saltation length, and the bed layer thickness at a high bed-load transport rate. These predictions all agree well with the experimental results. It is found that, on average,the travel length for the rolling sand grains is about an order of magnitude less than that of the lifted grains.A function for the bed-load sediment transport rate is derived. This function is obtained by using the entrainment probabilities of the rolling and lifted sediment grains, and by introducing two travel lengths,respectively. The predictions from the new bed-load function agree well with experimental results over the entire experimental range and show significant improvement over the commonly used formula for the bed-load transport rate. The new function shows that, in terms of contributing to the bed-load transport rate, the total entrainment probability of the sediment grains is a weighted summation of those for the lifted and rolling grains, rather than a simple addition of the two. The function is also used to predict the total entrainment probability, saltation length, and the bed layer thickness at a high bed-load transport rate. These predictions all agree well with the experimental results. It is found that, on average,the travel length for the rolling sand grains is about an order of magnitude less than that of the lifted grains.
关 键 词:SEDIMENTATION Bed load Entrainment probability
分 类 号:TV143[水利工程—水力学及河流动力学]
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