Physico-mechanical characterization of Higher Himalayan granite under the thermal treatments of different heating-cooling conditions

被引:10
作者
Ram, Bikash Kumar [1 ,2 ]
Gupta, Vikram [1 ,3 ]
机构
[1] Wadia Inst Himalayan Geol, Dehra Dun, India
[2] Indian Inst Petr & Energy, Visakhapatnam, India
[3] Sikkim Univ, Dept Geol, Gangtok, India
关键词
Air cooling; Himalayan granite; Point load strength; P-Wave velocity; Water cooling; MECHANICAL-PROPERTIES; HIGH-TEMPERATURE; GEOTHERMAL-ENERGY; STRATHBOGIE GRANITE; TENSILE-STRENGTH; RESERVOIR ROCKS; BEHAVIOR; PERMEABILITY; POROSITY; QUARTZ;
D O I
10.1007/s11440-023-02224-5
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Although point load strength is considered as a best proxy for uniaxial compressive strength and also incorporated in the routinely used rock mass rating (RMR) system, the effects of temperature treatments on the point load strength has not gained ample attention over the years. Accordingly, in this investigation, two different cooling techniques (i.e. water- and air-cooling methods) has been used in order to study the influence of different heating-cooling treatments on the physical properties, microstructural characteristics and point load strength of Himalayan granite collected from Sangla valley, Himachal Pradesh. The temperatures for heat treatment were targeted at 100 degrees C, 200 degrees C, 300 degrees C, 400 degrees C, 500 degrees C and 600 degrees C. As a response to thermal treatments, increase in effective porosity, decrease in density and increase in damage coefficient occurs which causes exponential decrease in point load strength. It decreases as high as 74% and 81% under air-cooling and water cooling, respectively, after heating of about 600 degrees C with reference to thermally untreated specimens. The microstructural study reveals that the grain boundary is quite intact, and the thermal-induced cracks are less pronounced up to 200 degrees C in both the thermal treatments. However, the increase in crack density due to thermal stresses and thermal shocks induce additional micro-cracks like intra-, inter- and trans-granular cracks, at and beyond 300 degrees C onwards and their coalescence with each other at higher temperatures (i.e. >= 500 degrees C) under both the thermal treatments contribute towards the variation in point load strength of thermally treated granites.
引用
收藏
页码:2841 / 2854
页数:14
相关论文
共 68 条
[1]   Comprehensive study including testing, monitoring and thermo-hydro modelling for design and implementation of a geothermal system in Torino (Italy) [J].
Barla, Giovanni .
GEOMECHANICS AND GEOPHYSICS FOR GEO-ENERGY AND GEO-RESOURCES, 2017, 3 (02) :175-188
[2]   Predicting uniaxial compressive strength by point load test: Significance of cone penetration [J].
Basu, A. ;
Aydin, A. .
ROCK MECHANICS AND ROCK ENGINEERING, 2006, 39 (05) :483-490
[3]   A Method for Estimating Crack-initiation Stress of Rock Materials by Porosity [J].
Basu, A. ;
Mishra, D. A. .
JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA, 2014, 84 (04) :397-405
[4]   Rock failure modes under uniaxial compression, Brazilian, and point load tests [J].
Basu, A. ;
Mishra, D. A. ;
Roychowdhury, K. .
BULLETIN OF ENGINEERING GEOLOGY AND THE ENVIRONMENT, 2013, 72 (3-4) :457-475
[5]  
Bieniawski ZT., 1989, Engineering rock mass classification, P251
[6]  
Breede K., 2013, GEOTHERM ENERGY, V1, P1, DOI [10.1186/2195-9706-1-4, DOI 10.1186/2195-9706-1-4]
[7]   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
[8]   Influence of thermal damage on physical properties of a granite rock: Porosity, permeability and ultrasonic wave evolutions [J].
Chaki, S. ;
Takarli, M. ;
Agbodjan, W. P. .
CONSTRUCTION AND BUILDING MATERIALS, 2008, 22 (07) :1456-1461
[9]  
Chandrasekharam D, 2005, PROC WORLD GEOTHERM
[10]   Shear Behavior of Artificial and Natural Granite Fractures After Heating and Water-Cooling Treatment [J].
Chen, Yuedu ;
Zhang, Chongyuan ;
Zhao, Zhihong ;
Zhao, Xingguang .
ROCK MECHANICS AND ROCK ENGINEERING, 2020, 53 (12) :5429-5449