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Laboratory scale investigation of stress wave propagation and vibrational characteristics in sand when subjected to air-blast loading

机译:爆炸载荷作用下砂土中应力波传播和振动特性的实验室规模研究

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The main objective of this study is to develop a new approach for evaluating the effects of air-blast on protective barrier made of sand. The air-blast loading is simulated experimentally laboratory using the shock tube test facility. The stress wave propagation in medium dense and dense sand medium are investigated under simulated air-blast loading. Synchronised pressure and accelerometer measurement system is used to capture peak stress wave pressure and peak particle velocity (PPV). The blast wave impact generates a stress wave in the medium leading to the compaction of the soil skeleton, which has led to stress enhancement (4-5 times of peak over-pressure) in top most sand layer, following which the high-pressure gas behind the shock front permeates through the sample. The intensity of stress waves and gas permeation rate gradually decrease with depth. Further, from the result of the simulated air-blast experiments, an empirical equation has been developed with a power law index of 1.88 and 1.36 for medium dense and dense sand respectively, to predict PPV against scaled blast distance. Visualisation of the sand deformation was possible with the help of a high-speed camera; displacement trajectories and strain contours are obtained through digital image correlation (DIC) analyses.
机译:这项研究的主要目的是开发一种新方法,以评估鼓风对砂制成的防护屏障的影响。使用冲击管测试设备在实验室中对鼓风载荷进行了模拟实验。在模拟的空气冲击载荷下,研究了应力波在中等密度和高密度砂土中的传播。同步压力和加速度计测量系统用于捕获峰值应力波压力和峰值粒子速度(PPV)。爆炸冲击波在介质中产生应力波,导致土壤骨架压实,从而导致最顶层砂层的应力增强(峰值超压的4-5倍),其后是高压气体冲击前部的后部穿过样品。应力波的强度和气体渗透率随深度逐渐减小。此外,从模拟爆炸实验的结果出发,针对中密度砂岩和致密砂岩,分别建立了幂律指数为1.88和1.36的经验方程,以预测PPV与成比例爆炸距离的关系。借助高速摄像头可以看到砂土变形。位移轨迹和应变轮廓是通过数字图像相关(DIC)分析获得的。

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