水槽
泥石流
碎片
泥浆
浪涌
流速
地质学
流量(数学)
脉搏(音乐)
前线(军事)
机械
沉积沉积环境
岩土工程
材料科学
地貌学
光学
物理
海洋学
复合材料
构造盆地
探测器
出处
期刊:Journal of hydrology. New Zealand
[New Zealand Hydrological Society]
日期:1990-01-01
卷期号:29 (1): 18-46
被引量:14
摘要
A laboratory moving-bed flume was used to study the development, behaviour and characteristics of high-concentration grain-in-fluid waves. These waves behaved similarly to reported debris-flow pulses. Observation of velocity and concentration profiles within the waves suggests that wave behaviour is mainly controlled by larger grains provided the background slurry of fine grains in water is sufficiently dense; that the front of a pulse is highly erosive while the tail is probably less erosive or depositional; and that the maximum height of a pulse is controlled by the velocity gradient within the flow
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