黄金科学技术 ›› 2020, Vol. 28 ›› Issue (6): 868-876.doi: 10.11872/j.issn.1005-2518.2020.06.055
王倩倩1,2(),徐颖1,2(),汪海波1,郑强强1,2,倪贤1,2,胡浩2
Qianqian WANG1,2(),Ying XU1,2(),Haibo WANG1,Qiangqiang ZHENG1,2,Xian NI1,2,Hao HU2
摘要:
地下深部复杂环境导致砂岩内部出现无裂损伤区,然而关于矿山深部爆破应力波作用下岩体的破裂与损伤尚未有成熟、系统的理论体系。以水泥砂浆作为砂岩相似材料进行变循环阈值试验得到无裂纹损伤试块,采用分离式霍普金森压杆(SHPB)装置对砂岩相似材料进行动态冲击压缩试验,通过调整冲击气压实现不同应变率条件下的砂岩相似材料冲击压缩,得到不同试验条件下试件的应力、应变和应变率变化关系。试验结果表明:无损和不同程度损伤砂岩的动态应力—应变曲线的形态相似,曲线峰值点随阈值增长出现右下移的现象,且动态压缩强度随损伤程度的加剧而削减,动态冲击损伤在循环阈值达到60%时到达损伤门槛值,与静态分析结果相呼应;峰值应力和峰值应变均存在应变率效应,且动态冲击荷载对试块的耦合效应在低应变率下更为显著,超过破碎应变率就不再发挥作用。
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