膨胀的
泥石流
流量(数学)
机械
碎片
剪应力
地质学
流速
流动特性
岩土工程
物理
海洋学
出处
期刊:Journal of the Hydraulics Division
[American Society of Civil Engineers]
日期:1978-08-01
卷期号:104 (8): 1153-1169
被引量:385
标识
DOI:10.1061/jyceaj.0005046
摘要
A mechanism of occurrence of bore-like debris flow due to the appearance of overland flow on the debris accumulation is considered using the applying shear stress and resisting stress relationship in the bed. The criteria for the occurence of the nonstationary bed flow and the partly stationary bed flow are made clear. The partly stationary bed flow approaches a quasi-steady state, whose depth, velocity and concentration are predictive applying the concept of dilatant fluid introduced by Bagnold. Although the front height of the nonstationary bed flow increases versus distance, the translation velocity and concentration are nearly constant and flow characteristics are theoretically predictive by some appropriate assumptions.
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