Development of Energy-Based Brittleness Index for Sandstone Subjected to Freeze-Thaw Cycles and Impact Loads

被引:21
作者
Zhang, Jian [1 ,2 ]
Deng, Hongwei [1 ]
Deng, Junren [1 ]
Ke, Bo [3 ]
机构
[1] Cent S Univ, Sch Resources & Safety Engn, Changsha 410083, Hunan, Peoples R China
[2] Univ Adelaide, Sch Civil Environm & Min Engn, Adelaide, SA 5005, Australia
[3] Wuhan Univ Technol, Sch Resource & Environm Engn, Wuhan 430070, Hubei, Peoples R China
基金
中国国家自然科学基金;
关键词
Sandstone; energy; brittleness; freeze-thaw; impact load; MECHANICAL-PROPERTIES; MAGNETIC-RESONANCE; SEDIMENTARY-ROCKS; PERMEABILITY; COMPRESSION; STRENGTH; SHALE; FLUID; NMR;
D O I
10.1109/ACCESS.2018.2867349
中图分类号
TP [自动化技术、计算机技术];
学科分类号
0812 ;
摘要
As one of the most important parameters of rock materials, brittleness is affected by external conditions such as temperature and dynamic disturbances. However, there is no universal criterion for brittleness. In this paper, the brittleness of sandstone subjected to rapid freeze-thaw (F-T) cycles and impact loads are investigated. The 25 specimens were subjected to different F-T cycles and impact loads and then investigated. It was found that the dynamic strength and Young's modulus of the specimens decrease, whereas porosity increases after the application of F-T cycles. The dynamic stress-strain curves demonstrated that after the peak point, the rock sample first exhibited class I behavior and then class II behavior. Previous studies implied that the brittleness index based on the pre-peak stress-strain characteristics was not sufficient to describe the rock fracture. Two brittleness indices based on the pre-peak and post-peak strain energy were thus derived using the complete dynamic stress-strain characteristics of rock samples. The two brittleness indices were strongly correlated with the physical parameters, such as porosity and mechanical parameters, including peak stress and dynamic modulus.
引用
收藏
页码:48522 / 48530
页数:9
相关论文
共 44 条
[1]   Mechanical property degradation of ignimbrite subjected to recurrent freeze-thaw cycles [J].
Altindag, R ;
Alyildiz, IS ;
Onargan, T .
INTERNATIONAL JOURNAL OF ROCK MECHANICS AND MINING SCIENCES, 2004, 41 (06) :1023-1028
[2]  
Altindag R, 2002, J S AFR I MIN METALL, V102, P61
[3]  
Altindag R., 2008, P 9 REG ROCK MECH S, P427
[4]  
Andreev G.E., 1995, BRITTLE FAILURE ROCK
[5]  
[Anonymous], 2012, SPE
[6]  
Batougina I., 1983, TECH REP
[7]  
Bergman S., 1983, P 5 INT SOC ROCK MEC, P302
[8]  
Bishop A.W., 1967, Proc. Geotech. Conf, V2, P142
[9]  
Chen J., 2014, CONSTRUCTION SHALE R, P2861
[10]   PORE-SIZE DISTRIBUTIONS FROM NUCLEAR-MAGNETIC-RESONANCE SPIN-LATTICE RELAXATION MEASUREMENTS OF FLUID-SATURATED POROUS SOLIDS .1. THEORY AND SIMULATION [J].
DAVIES, S ;
PACKER, KJ .
JOURNAL OF APPLIED PHYSICS, 1990, 67 (06) :3163-3170