Snowmelt water breakthrough into coal mine
DOI:
https://doi.org/10.51301/ejsu.2025.i6.06Keywords:
underground mining, ground surface, sinkhole, floodwater, technogenic rock stresses, natural hydrofracture, filtration, wa-ter inrushAbstract
The paper addresses the mechanism of flood water inrush from a technogenic ground sinkhole into underground excavation. Basing on computer simulation it was demonstrated that an area of tensile stresses is formed in the zone affected by underground mining. A natural hydrofracture of rocks may develop from the sinkhole into the mine opening under the effect of tensile stresses and water hydrostatic pressure. Hazardous water inflow into underground mine opening may be associated both with direct hydrofracture crack egress into the opening and with preliminary intense filtration water inflow from the crack into the opening if the crack development slows down. On approaching the mine opening the fracture may stop growing due to local rock compression near the opening. The modeling has demonstrated that the actual picture of the catastrophic water inflow into the ventilation gallery cannot be explained by filtration mechanism only. The catastrophic water breakthrough may be caused by development of a major water-conducting crack growing from natural frost crack in the bottom of the sinkhole towards the mine opening.
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