Experimental investigation of the mechanical and permeability characteristics of volcanic breccia

被引:13
|
作者
Jia, Chaojun [1 ,2 ]
Xu, Weiya [2 ]
Wang, Huanling [2 ,3 ]
Zhang, Qiang [4 ,5 ]
机构
[1] Cent South Univ, Sch Civil Engn, Changsha 410075, Peoples R China
[2] Hohai Univ, Res Inst Geotech Engn, Nanjing 210098, Peoples R China
[3] Hohai Univ, Key Lab Coastal Disaster & Def, Minist Educ, Nanjing 210098, Peoples R China
[4] China Inst Water Resources & Hydropower Res, Beijing 100048, Peoples R China
[5] Sichuan Univ, State Key Lab Hydraul & Mt River Engn, Chengdu 610065, Peoples R China
基金
国家重点研发计划; 中国博士后科学基金;
关键词
Volcanic breccia; Water effect; Permeability; Mechanical characteristics; Fluid pressure; BAIHETAN HYDROPOWER STATION; COLUMNAR JOINTED ROCK; PORE PRESSURE; STRESS; BEHAVIOR; SANDSTONE; STRENGTH; DAMAGE; EVOLUTION; DEFORMATION;
D O I
10.1007/s10064-020-01949-x
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
In this paper, a series of experiments were conducted on typical volcanic breccia collected from the foundation of Baihetan Dam. Considering previous work, the mechanical behavior and permeability of the volcanic breccia were further investigated. The experimental results showed that the compressive strength and Young's modulus of the volcanic breccia decrease due to the presence of water. However, the Poisson's ratio of the wet specimens was higher than that of the dried specimens. The permeability evolution under triaxial compression was divided into 5 stages. The fluid pressure showed a great influence on the permeability of the volcanic breccia. The water weakening mechanism and the effect of fluid pressure on the permeability were discussed. The effect of water on the strength of volcanic breccia is influenced by both subcritical crack growth and calcite dissolution. Due to the pore pressure gradient and the water weakening effect, the change in permeability with volumetric strain varies greatly.
引用
收藏
页码:599 / 610
页数:12
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