岩溶区拟建抽蓄上水库渗漏规律及防渗方案研究

    Leakage Pattern of Proposed Reservoirs in Karst Areas and Its Anti-seepage Solution

    • 摘要: 岩溶洼地或冲沟汇集区为抽蓄上水库建设提供了天然的有利地形条件,减少开挖量及建设成本;但此处断层破碎带、岩溶管道系统等发育,孕育着潜在渗漏风险,深入开展岩溶区抽蓄上水库渗漏机制与行为规律研究,识别主要渗漏路径、估算渗漏规模并制定针对性防控对策,是保障工程效能与经济价值的核心科学问题。论文以拟建的天井坪抽蓄工程上水库为研究对象,基于其地质条件、岩溶发育规律及岩体渗透特性,分析其渗漏可能性和渗漏模式,据此对其地层、断层破碎带、岩溶管道系统等关键地质结构进行FEFLOW建模,并通过达西定律和曼宁公式模拟分析天然工况下其地下水位并与实测验证。结果表明:拟建抽蓄上水库渗漏形式主要为岩溶管道导致的管道式渗漏和断层影响的裂隙式渗漏,天然状态下拟建水库地下水位模拟值与实测值的相关性系数R2在0.75以上,1155m高程蓄水位下渗漏量与规范计算结果接近,这些结果验证了本文模拟方法在复杂地质条件区的岩溶渗漏分析的有效性。利用建立的方法,开展拟建上水库蓄水工况模拟,运用Hagen-Poiseuille Law(哈根-泊肃叶定律)描述其岩溶管道(层)流,采用Particle Tracking Workflow模块跟踪与标记库水粒子,揭示该抽蓄上水库渗漏规律,据此提出针对性的防渗方案并评价其防渗效果。结果表明:岩溶管道、F2和F3断层为主要渗漏路径,其中岩溶管道渗漏量最大;在无防渗措施下,预测在天然1155m高程蓄水位蓄水64天后因渗漏而达到空库状态;当采用垂直防渗措施,虽然可减缓渗漏速率,但导致新的渗漏路径产生,进而使得岩溶水库渗漏模式由坝基渗漏转变为坝基与绕坝渗漏;当采用整体水平防渗措施,无论是渗漏路径状况还是渗漏量方面都表现出良好的防漏控渗效果。研究成果可为水库建设提供技术支撑与参考。

       

      Abstract: Karst depressions or confluence areas of gullies provide natural favorable topographic conditions for constructing upper reservoirs in pumped storage projects, reducing excavation volume and construction costs; however, the development of fault fracture zones and karst conduit systems in these areas poses potential seepage risks. Conducting in-depth research on the mechanisms and behavioral patterns of seepage in karst regions for upper reservoirs, identifying main seepage pathways, estimating leakage scales, and formulating targeted prevention strategies are core scientific issues for ensuring project efficiency and economic value. This paper takes a proposed upper reservoir in a karst area as the study object. Based on its geological conditions, karst development laws and rock permeability characteristics, the leakage possibility and leakage pattern are analyzed. Accordingly, FEFLOW modeling is performed for key geological structures such as strata, fault fracture zones, and karst conduit systems. Darcy's Law and Manning's formula are used to simulate the natural groundwater level, which is validated against measured data. The results show that the leakage of the proposed pumped-storage reservoir is mainly caused by pipeline leakage caused by karst pipelines and fissure leakage caused by faults. Under natural conditions, the correlation coefficient R2 between simulated and measured groundwater levels in the proposed karst reservoir exceeds 0.75, and the leakage volume at the storage water level of 1155 m elevation is consistent with normative calculations. These results verify the effectiveness of the simulation method for karst seepage analysis in complex geological conditions. Building on this, simulations for the reservoir impoundment scenario are conducted. The Hagen-Poiseuille Law describes the flow in karst conduits (laminar flow), and the Particle Tracking Workflow module traces and labels reservoir water particles to reveal the seepage patterns. Targeted anti-seepage schemes are then proposed and evaluated. The results indicate that without anti-seepage measures, the reservoir is predicted to reach an empty state after 64 days of impoundment at the natural storage level of 1155 m elevation due to seepage. Vertical anti-seepage measures slow the seepage rate but generate new leakage pathways, altering the seepage pattern. Horizontal anti-seepage measures demonstrate excellent performance in both leakage pathways and volume control. The findings provide technical support and references for reservoir construction.

       

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