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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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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:泥石流是一种速度快、沉积范围广的自然灾害,造成人员伤亡和设施破坏。设计有效的泥石流屏障,首先要考虑泥石流的冲击力。泥石流流速是评价泥石流冲击力的关键特征之一。在本研究中,我们进行了小型水槽试验,以分析泥石流的流动特性,并确定不同坡度和泥沙混合物的流动阻力系数。流速随水槽坡度和混合料类型而显著变化。泥石流深度随着坡度的增加而减小,但沉积物混合物之间的深度差异不显著。在流阻系数中,契兹系数(Ci)不仅表现出相对最高的拟合优度,而且无论泥石流事件的规模大小,它都表现出恒定值(20.19 m“1'2 s”1)。总体结果表明,在广泛的泥石流规模范围内,Ci最适合用于估算流速,流速是评估冲击力的关键因素。

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