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首页> 外文期刊>Journal of Korean Forest Society >Examining Velocity Estimation Equations of Debris Flow Using Small-scaled Flume Experiments
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Examining Velocity Estimation Equations of Debris Flow Using Small-scaled Flume Experiments

机译:使用小缩放的水槽实验检查碎片流量的速度估计方程

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摘要

With its rapid velocity and wide deposition, debris flow is a natural disaster that causes loss of human life and destruction of facility. To design effective debris barriers, impact force of debris flow should be first considered. Debris flow velocity is one of the key features to estimate the impact force of debris flow. In this study, we conducted small-scale flume experiments to analyze flow characteristics of debris flow, and determine flow resistance coefficients with different slope gradientsand sediment mixtures. Flow velocity significantly varied with flume slope and mixture type. Debris flow depth decreased as slope increased, but difference in depth between sediment mixtures was not significant. Among flow resistance coefficients, Chezycoefficient (Ci) showed not only relatively highest goodness of fit, but also constant value (20.19 m"1'2 s"1) regardless the scale of debris flow events. The overall results suggested that Ci can be most appropriately used to estimate flow velocity, thekey factor of assessing impact force, in wide range of debris flow scale.
机译:凭借其快速速度和广泛的沉积,碎片流动是一种自然灾害,导致人类生命丧失和设施的破坏。为了设计有效的碎片障碍,应首先考虑碎片流动的冲击力。碎屑流速是估计碎屑流动冲击力的关键特征之一。在这项研究中,我们进行了小型水槽实验,以分析碎片流动的流动特性,并确定具有不同坡梯度和沉积物混合物的流动性系数。流速显着变化了水槽斜率和混合物类型。随着斜率的增加,碎片流动深度降低,但沉积物混合物之间深度的差异并不显着。在流动性系数中,ChezyCoefficient(CI)不仅表现出相对最高的合适的优点,而且恒定值(20.19m“1'2 s”1)无论碎片流动事件的规模如何。总体结果表明,CI可以最适当地用于估计流速,评估冲击力的基因因子,在广泛的碎片流量范围内。

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