Monitoring Direct Current Resistivity During Coal Mining Process for Underground Water Detection: An Experimental Case Study

被引:14
|
作者
Su, Benyu [1 ]
Liu, Shengdong [2 ]
Deng, Lei [3 ]
Gardoni, Paolo [4 ]
Krolczyk, Grzegorz M. [5 ]
Li, Zhixiong [5 ,6 ]
机构
[1] China Univ Min & Technol, Dept Geophys, Xuzhou 221116, Jiangsu, Peoples R China
[2] China Univ Min & Technol, Sch Mech & Civil Engn, Xuzhou 221116, Jiangsu, Peoples R China
[3] Univ Wollongong, Sch Elect Comp & Telecommun Engn, Wollongong, NSW 2522, Australia
[4] Univ Illinois, Dept Civil & Environm Engn, Champaign, IL 61820 USA
[5] Opole Univ Technol, Fac Mech Engn, PL-45758 Opole, Poland
[6] Yonsei Univ, Yonsei Frontier Lab, Seoul 03722, South Korea
关键词
Conductivity; Three-dimensional displays; Coal mining; Coal; Monitoring; Rocks; Electric potential; 3-D cross borehole; direct current resistivity (DCR); geoelectrical sensing; underground water detection; BOREHOLE; INVERSION; TOMOGRAPHY;
D O I
10.1109/TGRS.2022.3173623
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Karst water may break into coal tunnels through the rock fissures and cause severe coal mine disasters. The direct current resistivity (DCR) is sensitive to underground water and can be used to detect fissures during the coal mining process. However, the three-dimensional (3-D) measurement of the DCR is still a challenging task and has not been applied to the practical coal mining dynamic process. To bridge this research gap, this study proposes a new 3-D cross-borehole method by monitoring the DCR at multiple points to analyze the geoelectrical field evolution in the underground coal mining process. Based on the forward and inversion theoretical analysis, a DCR observation system is developed for a real unground coal mine to evaluate the cross-borehole points. The 3-D resistivity distributions at different positions in the coal mining process are calculated. The analysis result demonstrates obvious resistivity changes with the evolution of the Karst water zone during the coal mining, and the location and movement of the Karst water can be well estimated. As a result, the proposed 3-D cross-borehole method is very effective for monitoring the DCR and is able to accurately detect the underground water.
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页数:8
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