An experimental study of the mechanical properties of granite after high temperature exposure based on mineral characteristics

被引:156
作者
Chen, You-Liang [1 ]
Wang, Su-Ran [1 ]
Ni, Jing [1 ]
Azzam, Rafig [2 ]
Fernandez-Steeger, Tomas Manuel [3 ]
机构
[1] Univ Shanghai Sci & Technol, Dept Civil Engn, 516 Jungong Rd, Shanghai 200093, Peoples R China
[2] Rhein Westfal TH Aachen, Dept Engn Geol & Hydrogeol, Lochnerstr 4-20 Haus A, D-52064 Aachen, Germany
[3] Tech Univ Berlin, Inst Angew Geowissensch, Ernst Reuter Pl 1,BH 3-1, D-10587 Berlin, Germany
基金
中国国家自然科学基金; 上海市自然科学基金;
关键词
Mineral characteristic; Rock mechanics; Scanning electron microscopy; Phlogopite; High temperature; Fracture toughness; FRACTURE-TOUGHNESS; THERMAL-EXPANSION; WESTERLY GRANITE; IGNEOUS ROCKS; HIGH-PRESSURE; COMPRESSION; PROPAGATION; BEHAVIOR;
D O I
10.1016/j.enggeo.2017.02.010
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
The macroscopic mechanical properties of granite collected from the Fujian Province, China were measured using uniaxial compression and three-point bending after the granite was exposed to high temperatures. The stress strain relationship was measured and mechanical properties including the Young's modulus, uniaxial compressive strength (UCS) and fracture toughness were calculated. In general, the uniaxial compressive strength (UCS), Young's modulus and fracture toughness of the granite specimens decrease with an increase in heat treatment temperature up to 800 degrees C, above which there is no obvious change. The microstructure of the failed specimens was explored using scanning electron microscopy (SEM) and stereomicroscopy. After heat treatment, the minerals within the granite were analysed using X-ray diffraction. The failure mechanisms and the mechanical characteristics of the granite are explained in terms of the microstructure and the minerals present. The results of the experiments indicate that the crystal structure of the phlogopite in granite transforms to a more stable structure between 400 degrees C and 600 degrees C with an associated increase in volume. A dehydroxylation reaction also occurs in the phlogopite at 400 degrees C, after which the uniaxial compressive strength (UCS) decreases and the ductility increases. Using SEM and stereomicroscopy, it was observed that the connection between the minerals within the granite becomes weaker with increasing heat treatment temperature. Intercrystalline cracking is the main failure mode for samples exposed to temperatures below 800 degrees C, whereas transcrystalline cracking can be observed in samples exposed to 1000 degrees C. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:234 / 242
页数:9
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