Evolution of Permeability in Sandstone During Confined Brazilian Testing

被引:6
|
作者
Hagengruber, T. [1 ]
Taha, M. M. Reda [1 ]
Rougier, E. [2 ]
Knight, E. E. [2 ]
Stormont, J. C. [1 ]
机构
[1] Univ New Mexico, Dept Civil Construct & Environm Engn, Albuquerque, NM 87131 USA
[2] Los Alamos Natl Lab, Los Alamos, NM USA
关键词
Permeability; Confined Brazilian test; Confined extension; Intermediate principal stress; Strength; Fracture initiation; TENSILE-STRENGTH; FRACTURE; ROCK; COMPACTION;
D O I
10.1007/s00603-021-02527-7
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Permeability measurements were made on sandstone during confined Brazilian strength tests. The test involves 50 mm diameter disk-shaped, jacketed samples that are subjected to confining stresses while they are diametrically loaded. Specially designed end caps allow for concurrent gas flow measurements. The test configuration allows for the samples to be subjected to a range of stresses, with the confining stress as the intermediate principal stress. The majority of the tests measured permeability during loading to failure in the confined extension region. The permeability of the sandstone sample increases significantly well before the peak load is reached due to newly formed microcracks that continue to coalesce and dilate with further loading. Permeability increases are inversely proportional to the intermediate principal stress as increased confining pressures suppress growth, coalescence, and dilation of microcracks. Additional testing includes unloading and reloading cycles prior to failure. With each unloading-reloading cycle, permeability at comparable stresses is increased compared to the previous cycle, consistent with increasing damage in the form of an expanding microcrack network.
引用
收藏
页码:2651 / 2664
页数:14
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