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低应变率冲击荷载下节理花岗岩的动力响应规律

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岩体中节理面的存在是引起冲击应力波衰减的主要原因,会造成爆炸能量的衰减及降低爆破效果.为探讨低应变率下不同节理倾角花岗岩在冲击荷载作用下的动态力学性质、应力波传递规律和能量传递规律,利用分离式霍普金森压杆(split Hopkinson pressure bar,简称SHPB)试验装置对低应变率下3种不同冲击气压、4种不同倾角的节理花岗岩进行冲击试验.结果表明:(1)在含节理的岩样中,其峰值应力随节理倾角的增大呈下降趋势,随冲击荷载的增大呈上升趋势;(2)透射系数随节理倾角的增加先增大后减小,随冲击荷载的增大先减小后增大;(3)能量传递系数随节理倾角的增加先增高后降低,完整岩样、节理倾角θ=0°和45°的岩样,其能量传递系数都随着冲击荷载的增大而减小,而节理倾角θ=15°和30°的岩样,其能量传递系数随着冲击荷载的增大先减小后增大.
Dynamic response of jointed granite under low strain rate impact load
The presence of joint surfaces in rock masses primarily causes the attenuation of shock stress waves,leading to reduced explosion energy and blasting effectiveness.To investigate the dynamic mechanical properties,stress wave transfer law,and energy transfer law of granite with different joint dip angles under low strain rate impact loads,impact tests were conducted on jointed granite using the split Hopkinson pressure bar(SHPB)device.The tests involved three different impact pressures and four different dip angles.The results indicate that:(1)In rock samples with joints,the peak stress decreases with the increase of joint dip angle and increases with the increase of impact load.(2)The transmission coefficient initially increases and then decreases with increasing joint dip angles,and initially decreases and then increases with increasing impact load.(3)The energy transfer coefficient initially increases and then decreases with the increase of joint dip angle.For intact rock samples and rock samples with joint dip angles of θ=0° and 45°,the energy transfer coefficient decreases with the increase of impact load.For rock samples with joint dip angles of θ=15° and 30°,the energy transfer coefficient of first decreases and then increases with the increase of impact load.

dip anglesjointed graniteSHPB impact testdynamic responselow strain rate

王智德、司莹莹、李杰、钱梦凡、安佳兴

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武汉理工大学土木工程与建筑学院,湖北武汉 430070

武汉市勘察设计有限公司,湖北武汉 430000

倾角 节理花岗岩 SHPB冲击试验 动力响应 低应变率

国家自然科学基金国家自然科学基金磷资源开发利用教育部工程研究中心开放基金武汉市城乡建设委员会科技计划武汉市城乡建设委员会科技计划

4207722851374163LKF202004武城建[2017]12号-201740武城建[2019]68号-201941

2024

岩土力学
中国科学院武汉岩土力学研究所

岩土力学

CSTPCD北大核心
影响因子:1.614
ISSN:1000-7598
年,卷(期):2024.45(6)