泥石流
山崩
碎片
地质学
流量(数学)
航程(航空)
前线(军事)
环境科学
二次方程
机械
水文学(农业)
岩土工程
土壤科学
材料科学
数学
物理
几何学
海洋学
复合材料
作者
Louis Bugnion,Brian W. McArdell,Perry Bartelt,Corinna Wendeler
出处
期刊:Landslides
[Springer Science+Business Media]
日期:2011-09-09
卷期号:9 (2): 179-187
被引量:202
标识
DOI:10.1007/s10346-011-0294-4
摘要
We present measurements of hillslope debris flow impact pressures on small obstacles. Two impact sensors have been installed in a real-scale experimental site where 50 m3 of water-saturated soil material are released from rest. Impact velocities vary between 2 and 13 m/s; flow heights between 0.3 and 1.0 m. The maximum impact pressures measured over 15 events represent between 2 and 50 times the equivalent static pressures. The measurements reveal that quadratic velocity-dependent formulas can be used to estimate impact pressures. Impact coefficients C are constant from front to tail and range between 0.4 < C < 0.8 according to the individual events. The pressure fluctuations to depend on the sensor size and are between 20% and 60% of the mean pressure values. Our results suggest that hazard guidelines for hillslope debris flows should be based on quadratic velocity-dependent formulas.
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