Gas flow unified measurement system for sequential measurement of gas diffusion and gas permeability of partially hydrated geosynthetic clay liners

被引:43
作者
Rouf, Md A. [1 ]
Bouazza, Abdelmalek [2 ]
Singh, Rao M. [3 ]
Gates, Will P. [2 ]
Rowe, R. Kerry [4 ]
机构
[1] Monash Univ, Dept Civil Engn, 18 Alliance Lane, Clayton, Vic 3800, Australia
[2] Monash Univ, Dept Civil Engn, 23 Coll Walk, Clayton, Vic 3800, Australia
[3] Univ Surrey, Dept Civil & Environm Engn, 24 AA 02, Guildford GU2 7XH, Surrey, England
[4] Queens Univ, Dept Civil Engn, Ellis Hall, Kingston, ON K7L 3N6, Canada
基金
澳大利亚研究理事会;
关键词
geosynthetic clay liner; gas flow; diffusion; advection; gravimetric water content; HYDRAULIC CONDUCTIVITY; OXYGEN DIFFUSION; POROUS-MEDIA; GASEOUS-DIFFUSION; CATION-EXCHANGE; COMPOSITE LINER; GCL; PERFORMANCE; TAILINGS; COVERS;
D O I
10.1139/cgj-2015-0123
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
A gas flow unified measurement system (UMS-G) for sequential measurement of gas diffusion and gas permeability of geosynthetic clay liners (GCLs) under applied stress conditions (2 to 20 kPa) is described. Measurements made with the UMS-G are compared with measurements made with conventional experimental devices and are found to give similar results. The UMS-G removes the need to rely on two separate systems and increases further the reliability of the gas properties' measurements. This study also shows that the gas diffusion and gas permeability reduce greatly with the increase of both gravimetric water content and apparent degree of saturation. The effect of applied stress on gas diffusion and gas permeability is found to be more pronounced at gravimetric water content greater than 60%. These findings suggest that at a nominal overburden stress of 20 kPa, the GCL used in the present investigation needs to be hydrated to 134% gravimetric water content (65% apparent degree of saturation) before gas diffusion and gas permeability drop to 5.5 x 10(-11) m(2).s(-1) and 8.0 x 10(-13) m.s(-1), respectively, and to an even higher gravimetric water content (apparent degrees of saturation) at lower stress.
引用
收藏
页码:1000 / 1012
页数:13
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