Multiphysics Multicoupled Modeling of Rock Fragmentation under High-Voltage Electrical Pulse

被引:3
|
作者
Feng, Weikang [1 ]
Rao, Pingping [1 ]
Cui, Jifei [1 ]
Ouyang, Peihao [2 ]
Chen, Qingsheng [3 ]
Nimbalkar, Sanjay [4 ]
机构
[1] Univ Shanghai Sci & Technol, Sch Environm & Architect, Shanghai 200093, Peoples R China
[2] Tongji Univ, Dept Geotech Engn, Shanghai 200092, Peoples R China
[3] Hubei Univ Technol, Technol Res Ctr Ecol Rd Engn, Wuhan 430068, Peoples R China
[4] Univ Technol Sydney, Sch Civil & Environm Engn, 15 Broadway, Ultimo, NSW 2007, Australia
基金
中国国家自然科学基金;
关键词
High-voltage electrical pulse; Multiphysics coupling; Particles; Electric damage; Plasma channel; Rock breaking; DISINTEGRATION; FRACTURE; COAL; LIBERATION; BREAKAGE; WASTE;
D O I
10.1061/IJGNAI.GMENG-9298
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
In this research, the finite-element numerical software COMSOL Multiphysics is used to simulate the electric pulse rock-breaking process, and the novel numerical model takes into account the multiple fields of electrical, thermal, and mechanical physics. The electric field strength inside the rock under the action of the electric pulse is updated by the full coupling function of COMSOL (version 6.1) software, and the electric damage variable chi is used to describe the process of electric breakdown inside the rock, to simulate the formation of plasma channel in the process of electric pulse rock-breaking. The voltage change curves and plasma channel trajectories in the electric breakdown process of the model in this paper are compared with the literature to verify the accuracy of the model. The formation process of plasma channels captures the temperature and stress changes during the whole process of electric pulse rock-breaking, to reveal the mechanism of the electric pulse rock-breaking process. With the presence of conductive particles inside the rock, the particles can effectively promote the formation of plasma channels, increase the area of electrical damage, and improve rock-breaking efficiency. Before the formation of the plasma channel, the internal temperature of the rock is about 600 K, and the stress is about 10-2 MPa; when the channel is formed, the energy of the electric pulse is mainly concentrated in the plasma channel, and the temperature of the plasma channel rises to 104 K. When the maximum stress exceeds the critical stress of the rock, the rock undergoes fracture. Furthermore, an appropriate increase in the rise time of the electric pulse increases the speed and area of rock-breaking, subsequently improving the efficiency of rock fracture. The results of the numerical modeling in this paper help to better understand the mechanism of the electric pulse rock-breaking process, which is of great engineering significance for the development of new electric pulse rock-breaking technology in the realm of geotechnical engineering.
引用
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页数:12
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