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An analysis of the influence of mining on water inrush from steep seam floor based on geophysical exploration results |
Yu-He WANG, Zeng-Bin CUI( ), Chun-Peng LI |
Shandong Science and Technology University (Qingdao), Qingdao 266590, China |
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Abstract In order to understand the influence of different propelling distances on water inrush from the working face floor during the mining of steep inclined coal seam, the authors detected the water-bearing strength and water-bearing position of the working face floor at 31515 of a coal mine in Shandong Province by TEM. Then, the fem difference software FLAC 3D was used to simulate the formation and evolution of water inrush channels on the bottom of steep inclined coal seam face in the confined aquifer when different propulsion lengths were simulated. And the change of the pressure water conduction height and seepage flow vector of the bottom plate with the advance of the working face was investigated. The results show that the working face stoping makes the floor form the plastic failure zone, and under the action of the pore pressure of the water in the confined aquifer of the floor, the uplift zone of confined water and the mining failure zone of the floor are conductive, thus the risk of water inrush from the coal seam floor is easy to occur.
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Received: 11 May 2019
Published: 28 November 2019
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Corresponding Authors:
Zeng-Bin CUI
E-mail: 1239219490@qq.com
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Transient electromagnetic detection (vertical) apparent resistivity profile
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Transient electromagnetic (tem) detection (in-plane floor 45° direction) apparent resistivity section
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The changing cloud chart of the plastic zone along the slope of the coal seam with the working face
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Pore water pressure and vectorial cloud picture of the bottom plate during the step forward process of working face
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