Laboratory investigation of the mode-I fracture of sandstone caused by a combination of freeze-thaw cycles and chemical solutions

被引:23
作者
Han, Tielin [1 ,2 ]
Wang, Xianfeng [2 ]
Li, Zhihui [1 ]
Li, Dawang [2 ]
Xing, Feng [2 ]
Han, Ningxu [2 ]
机构
[1] Xian Univ Technol, Sch Civil Engn & Architecture, Xian 710048, Shaanxi, Peoples R China
[2] Shenzhen Univ, Coll Civil Engn, Guangdong Prov Key Lab Durabil Marine Civil Engn, Shenzhen 518060, Peoples R China
基金
中国国家自然科学基金;
关键词
Sandstone deterioration; Chemical corrosion; Freeze-thaw cycle; Mode-I fracture; Damage variable; SLOW CRACK-GROWTH; MECHANICAL-PROPERTIES; FROST-RESISTANCE; TOUGHNESS; ROCK; WATER; PROPAGATION; DAMAGE; DECAY; DEFORMATION;
D O I
10.1007/s10064-020-01762-6
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The mechanical parameters and deterioration mechanisms of sandstone specimens obtained from the hydrofluctuation belt in the Three Gorges Reservoir Region of China were investigated under a combination of freeze-thaw cycles and different chemical solutions. The degradation in several mechanical characteristics was discussed, and the degree of freeze-thaw deterioration of the mechanical behaviors was quantitatively analyzed based on the crack propagation radii and a damage variable that reflects the changes in porosity. The results showed that the mechanical parameters of sandstone had a significant damage deteriorating trend under freeze-thaw cycles and different chemical solutions. And the degree of damage deterioration of fracture toughnessK(IC)was the greatest, followed by that of tensile strength; that of compression strength was the smallest. There was obvious consistency among fracture toughnessK(IC), tensile strength, and compression strength of sandstone under a combination of freeze-thaw cycles and different chemical solutions; those were obvious linear relationship. The crack propagation radii for the various effects of freeze-thaw cycles and chemical solutions were smaller than those of the natural state and the radii generally decreased with increasing freeze-thaw cycles.
引用
收藏
页码:3689 / 3706
页数:18
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