Thermal effects on failure characteristics of granite with pre-existing fissures

被引:17
作者
Zhao, Fei [1 ]
Sun, Qiang [2 ]
Yang, Duoxing [3 ]
Zhang, Weiqiang [1 ]
机构
[1] China Univ Min & Technol, Sch Resources & Geosci, Xuzhou, Jiangsu, Peoples R China
[2] Xian Univ Sci & Technol, Geol Res Inst Coal Green Min, Xian, Shaanxi, Peoples R China
[3] China Earthquake Adm, Inst Crustal Dynam, Beijing, Peoples R China
基金
中国国家自然科学基金;
关键词
failure; rocks; rock mechanics; thermal effects; HIGH-TEMPERATURE; MECHANICAL-PROPERTIES; CRACK COALESCENCE; TENSILE-STRENGTH; BEHAVIOR; ROCK; SANDSTONE; STRESS; FLAWS; DAMAGE;
D O I
10.1680/jgere.19.00019
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In order to study the effects of pre-existing fissures on the failure characteristics of granite after high-temperature treatment, granite samples containing three different sets of fissures were heated at different temperatures (100-800 degrees C), and then a uniaxial compression test was carried out. The major findings are as follows. (a) Temperature and pre-existing fissures have a great influence on the strength of granite. When the temperature is low, the compressive strength exhibits an approximately linear upward relation with increasing alpha in the range from 30 to 60 degrees. However, with increasing temperature, the effect of pre-existing fissures on the strength of granite decreases, and this trend of growth gradually diminishes. In addition, the thickness of granite samples (from 16 to 29 mm) has little effect on the strength of granite in this study. (b) The failure of granite is transformed from brittle to plastic deformation with elevated treatment temperature. In addition, according to failure patterns of granite, there are four crack failure modes under uniaxial pressure. Failure modes I and II occur below 600 degrees C, and failure modes III and IV mainly occur above 600 degrees C.
引用
收藏
页码:302 / 311
页数:10
相关论文
共 56 条
[1]   THE INFLUENCE OF MICROCRACK DENSITY ON THE ELASTIC AND FRACTURE MECHANICAL-PROPERTIES OF STRIPA GRANITE [J].
ALM, O ;
JAKTLUND, LL ;
SHAOQUAN, K .
PHYSICS OF THE EARTH AND PLANETARY INTERIORS, 1985, 40 (03) :161-179
[2]  
Andreev G.E., 1995, BRITTLE FAILURE ROCK
[3]   Temperature influence on the physical and mechanical properties of a porous rock: San Julian's calcarenite [J].
Brotons, V. ;
Tomas, R. ;
Ivorra, S. ;
Alarcon, J. C. .
ENGINEERING GEOLOGY, 2013, 167 :117-127
[4]   Experimental study on the influence of temperature on the mechanical properties of granite under uni-axial compression and fatigue loading [J].
Chen, You-Liang ;
Ni, Jing ;
Shao, Wei ;
Azzam, Rafig .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2012, 56 :62-66
[5]  
Clerici A, 1990, B INT ASS ENG GEOLOG, V41, P57, DOI [10.1007/BF02590207, DOI 10.1007/BF02590207]
[6]   Influence of stress-induced and thermal cracking on physical properties and microstructure of La Peyratte granite [J].
David, C ;
Menéndez, B ;
Darot, M .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 1999, 36 (04) :433-448
[7]   Sliding crack model for nonlinearity and hysteresis in the uniaxial stress-strain curve of rock [J].
David, E. C. ;
Brantut, N. ;
Schubnel, A. ;
Zimmerman, R. W. .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2012, 52 :9-17
[8]   Experimental study of heat transfer on the borders of grains in ordered and disordered media [J].
Emirov S.N. ;
Ramazanova A.E. .
Bulletin of the Russian Academy of Sciences: Physics, 2013, 77 (03) :284-287
[9]   Kinematics of throughgoing fractures in jointed rocks [J].
Finn, MD ;
Gross, MR ;
Eyal, Y ;
Draper, G .
TECTONOPHYSICS, 2003, 376 (3-4) :151-166
[10]   Thermal stress-induced microcracking in building granite [J].
Freire-Lista, D. M. ;
Fort, R. ;
Varas-Muriel, M. J. .
ENGINEERING GEOLOGY, 2016, 206 :83-93