Research on gas migration properties in a saturated bentonite/sand mixture under flexible boundary conditions

被引:27
作者
Liu, Jiang-Feng [1 ,2 ]
Song, Shuai-Bing [1 ]
Ni, Hong-Yang [1 ]
Cao, Xu-Lou [1 ]
Pu, Hai [1 ]
Mao, Xian-Biao [1 ]
Skoczylas, Frederic [3 ,4 ]
机构
[1] China Univ Min & Technol, Sch Mech & Civil Engn, State Key Lab GeoMech & Deep Underground Engn, Xuzhou 221116, Peoples R China
[2] Chengdu Univ Technol, State Key Lab Geohazard Prevent & Geoenvironm Pro, Chengdu 610059, Sichuan, Peoples R China
[3] CNRS, LML, F-59651 Villeneuve Dascq, France
[4] Ecole Cent Lille, CS 20048, F-59651 Villeneuve Dascq, France
基金
中国博士后科学基金;
关键词
Geological repositories; Bentonite/sand mixture; Gas migration; Gas breakthrough; HYDRAULIC CONDUCTIVITY; WASTE-DISPOSAL; WATER-CONTENT; SAND MIXTURE; CLAY; PRESSURE; BREAKTHROUGH; PERMEABILITY; CLAYSTONE; PATHWAYS;
D O I
10.1016/j.sandf.2017.11.003
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Gas migration/breakthrough in saturated bentonite is an important issue for the evolution of the sealing ability of the engineered barrier in deep geological repositories. The main contribution of our study is to provide insights into the water and gas transport properties in a compacted bentonite/sand mixture, which was wrapped by a flexible Viton (TM) membrane directly before being put into a triaxial cell. The experimental results indicate that the water permeability is very low and the magnitude is in the order of 10(-20) m(2). Gas breakthrough tests show that no continuous gas flow was detected during the entire gas break-through test (until the gas pressure of 10 MPa), which indicates that the compacted bentonite/sand mixture has a good sealing ability after full saturation. Another important finding is that the gas migration properties are closely related to the stress state around the sample, the internal pore fluid pressure, and the creep effects caused by the two factors. (C) 2018 Production and hosting by Elsevier B.V. on behalf of The Japanese Geotechnical Society.
引用
收藏
页码:97 / 109
页数:13
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