Microseismic monitoring system for instantaneous outbursts in coal mines

2013 ◽  
Author(s):  
Binxin Hu ◽  
Tongyu Liu ◽  
Jinyu Wang ◽  
Guangdong Song

2018 ◽  
Vol 1065 ◽  
pp. 252012
Author(s):  
Binxin Hu ◽  
Guangdong Song ◽  
Feng Zhu ◽  
Hua Zhang ◽  
Tongyu Liu

2012 ◽  
Vol 190-191 ◽  
pp. 1179-1182
Author(s):  
Xiu Zhi Meng ◽  
Zeng Zhi Zhang ◽  
Zong Sheng Wang

The mining boundary ultra-layer & cross-border of some small coal mines in the profit-driven results in a many of safety accidents, waste of resources and environmental damage while the state can not achieve the full uninterrupted supervision because of the backward monitoring tools and equipment. In this situation the real-time monitoring system for underground mining activities is designed based on explosion source location technology. Small and medium-sized coal mines tunnel by blasting operations. The P waves are picked up by acceleration vibration sensors buried underground that are identified and dealt by using wavelet transform. The bursting point is located by the Geiger algorithm and displayed in the mine’s electronic map. The monitor system has good stability, small positioning error by field-proven.


Measurement ◽  
2021 ◽  
pp. 110449
Author(s):  
Shili Li ◽  
Yong Ni ◽  
Yu Wang ◽  
Jinhui Shi ◽  
Shichao Zhang ◽  
...  

2013 ◽  
Vol 838-841 ◽  
pp. 889-893
Author(s):  
Biao Li ◽  
Feng Dai ◽  
Nu Wen Xu ◽  
Chun Sha

The right bank underground powerhouse of Houziyan hydropower station is a typical deep-buried type with high geostress and complicated geological conditions. To monitor and analyze the stability of surrounding rock mass during continuous excavation of the powerhouse excavation and locate the potential failure zones, an ESG (Engineering Seismology Group) microseismic monitoring system manufactured in Canada was installed in April, 2013. The wave velocity of the monitoring system was determined through fixed blasting tests. And the average location error is the minimum while P-wave velocity is 5700m/s, less than 10m and meeting the system request. By combining the temporal and spatial distribution regularity of microseimic events with field excavation, micro-crack clusters and potential instability zones were identified and delineated. The results will provide a reference for later excavations and supports of the underground powerhouse. Furthermore, a new monitoring method can also be supplied for the stability analysis of surrounding rock mass in deep-buried underground powerhouses.


2020 ◽  
Vol 1621 ◽  
pp. 012004
Author(s):  
Guangdong Song ◽  
Binxin Hu ◽  
Feng Zhu ◽  
Hua Zhang ◽  
Tongyu Liu

2017 ◽  
Author(s):  
Weibo Wang* ◽  
Zhiwei Wang ◽  
Chenxi Sun ◽  
Huagang Zhao ◽  
Zelin Hou ◽  
...  

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