吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (5): 1376-1388.doi: 10.13278/j.cnki.jjuese.20180189
王梓龙1,2, 裴向军1, 张御阳1, 张硕1, 魏小佳3, 王双3
Wang Zilong1,2, Pei Xiangjun1, Zhang Yuyang1, Zhang Shuo1, Wei Xiaojia3, Wang Shuang3
摘要: 为了对松动岩体的工程特性进行系统研究,以楞古水电站厂址区边坡为例,对该边坡岩体进行了详细的地质编录和物理勘探试验,重点对节理裂隙的空间发育规律、镶嵌结构和碎裂结构岩体的发育深度及空间分布、软弱结构面发育分布规律以及边坡已有变形破坏特征这四个方面进行了系统的统计和分析,认为松动岩体是区域断裂活动和浅表生改造的结果,岩体工程效应差、变形模量低;同时结合应力测试、声波测速、高密度电磁勘探等试验成果进行分析,结果显示松动岩体具低波速(波速大部分小于3 000 m/s)、低应力(最大主应力不超过20 MPa)、强透水性(透水性系数大于10 L/(min·m·m))。认为岩体破碎主要受断层及节理裂隙影响,分析了岩体破裂松动的演化过程及特征。
中图分类号:
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