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陕渑煤田顶底板水害评价与防治对策研究
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摘要
本文研究了豫西陕渑煤田主要含水层和其补径排条件,收集了已发生的矿井水害资料,指出:矿井现生产采区的主要水害类型为顶板砂岩水和底板灰岩水,重点是底板奥陶系灰岩溶裂隙水。应用“三图-双预测”法对顶板砂岩水的突水条件进行了危险性分区和涌水量预算,应用脆弱性指数法对底板太原组灰岩与奥陶系灰岩含水层的突水危险性分别进行了评价和危险性分区,指出:由于长期疏排(泄),顶板砂岩水和底板太原组薄层灰岩水水位大幅下降,储量不足,对矿井正常生产影响有限;矿井防治水工作的重点和难点在于预防奥灰含水层突水。根据奥灰突水危险性分区,提出了加强管理、健全水位动态观测系统、扩大矿井排水能力、综合物探查异、注浆改造底板、排用结合等对策与建议。
In this paper, the main aquifers and their conditions of recharge, runoff and discharge inShanmian coalfield have been studied. According to the water hazards data, the main waterhazards are sandstone water from the roof and karst water from the floor. The Ordovician Karstfissure water from the floor is the research emphasis. By using the method of three maps and twopredictions, the water inrush condition of sandstone water from the roof has been analyzed and thewater inflow has been calculated. By using the method of Vulnerability Index (VI), the waterinrush conditions of Taiyuan Formation and Ordovician Karst aquifer have been evaluated andanalyzed. The results show that the sandstone water from the roof and the Taiyuan Formation karstwater have limited influence as long-term drainage and lower water level. The key point anddifficulty of mining control is how to prevent the water inrush from the Ordovician aquifer.According to the risking zoning, some suggestions are put forward, such as, the managementshould be strengthened, the dynamic observation system should be perfected, the drainagecapacity should be enlarged, the floor should be strengthened, comprehensive geophysicalprospecting should be carried out.
引文
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