ISSN 1000-3665 CN 11-2202/P

    隧道工程建设对华蓥山中部岩溶地下水环境的影响研究

    Influence of tunnel construction on karst groundwater environment in central Huaying Mountain

    • 摘要: 华蓥山中部地质构造复杂,碳酸盐岩广泛出露,已建的地下工程均遭遇了不同程度的涌突水灾害并对地下水环境影响造成了一定程度的影响,华蓥山现有岩溶研究精度、广度无法满足工程建设的需要,亟需系统全面的分析岩溶涌突水原因及其对地下水环境的影响。本文通过野外调查与收集整理大量地下工程涌突水资料,运用地下水系统理论方法,分析了华蓥山背斜地下水径流特征、已建的G42华蓥山隧道及绿水洞煤矿工程活动对地下水环境的影响,研究了新建广邻快速公路华蓥山隧道对岩溶地下水环境造成的潜在影响。结果显示:已建地下工程活动使得华蓥山中部天池向斜岩溶槽谷及绿水洞背斜内的诸多泉点、暗河减流或断流,对地下水的影响范围面积大致为29.6 km2,仅G42华蓥山隧道泄水洞每年排水量大致在94.6~730.0×104 m3/年;计算得出新建广邻快速公路华蓥山隧道正常涌水量约12.05×104 m3/d,对岩溶地下水的影响范围在1.0~2.1 km,对隧道北侧岩溶地下水有一定程度影响,而对隧道南侧饮用水源地水量及天池湖水影响微弱。该研究可为华蓥山及川东平行岭谷区线路选线、岩溶隧道涌突水预测、生态环境保护提供一定的参考与理论支撑。

       

      Abstract: With complex geological structures and extensive exposure of carbonate rocks in the middle section of Huaying Mountain, the underground projects have suffered from water inrush disasters of varying degrees and have impacts on the groundwater environment. Current karst studies in the region are insufficient to meet the needs of engineering projects, highlighting the need for a more systematic and comprehensive analysis of the causes of karst water inrush and its effects on the groundwater environment. This study, based on field investigation and extensive data collection of underground engineering water inrush events, utilized groundwater system theory to analyze the groundwater runoff characteristics in the Huayingshan anticline, The study also assessed the influence of the existing Huayingshan tunnel on highway G42 and the Lvshuitong coal mine engineering activities on the groundwater environment, and explored the potential impact of the new Huayingshan tunnel of Gaung’an-Lingshui highway on the karst groundwater environment. The results show that human activities, particularly underground engineering, have altered the hydrology of the central Huaying Mountain area, transforming multiple spring points into reduced or disconnected subsurface river flows, especially in the Tianchi synclinal karst valley and Green Water Cave. The influence area of groundwater is 29.6 km2, with the annual displacement of drainage hole of Huayingshan tunnel on highway G42 of 94.6~730×104 m3/year; the normal inflow of the new tunnel of Gaung’an-Lingshui highway is approximately 12.05×104 m3/d, with the influence range of karst groundwater of 1.0~2.1 km. The impact on karst groundwater to the north of the new tunnel is significant, while the influence on the drinking water source and the lake water of Tianchi Lake to the south of the new tunnel is relatively weak. This study can provide basic information and theoretical support for route selection in the Huaying Mountain and parallel ridge-valley area of eastern Sichuan, as well as for water inrush prediction of karst tunnel and ecological environment protection.

       

    /

    返回文章
    返回