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首页> 外文期刊>Bulletin of engineering geology and the environment >Seepage field analysis and evaluation of seepage control effect at the dam foundation of Baihetan Hydropower Station
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Seepage field analysis and evaluation of seepage control effect at the dam foundation of Baihetan Hydropower Station

机译:白鹤滩水电站坝基渗流场分析及防渗效果评价

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摘要

With a large catchment area, stratified groundwater on the left and right bank, developed unloading fissures in the damfoundation rock, and prominent permeability anisotropy in columnar jointed basalt, the dam site of Baihetan HydropowerStation possesses complex seepage control measures. Moreover, the water head difference between the upstream and downstreamcan reach 235 m after impoundment, and thus, the seepage field of the dam site area will be extremely intricate. Inthis study, we analyzed the seepage field characteristics of the dam foundation during impoundment with field measurementdata, and conducted numerical simulation of seepage field under normal water level condition with steady seepagecalculation method. With the field measurement data and the numerical simulation results, we evaluated the performanceof the seepage control system and revealed the movement process of the seepage flow in the dam foundation. The analysisresults show that the impervious curtain can effectively stop the reservoir water from flowing to downstream side of thedam through the rock masses in the dam foundation, the drainage holes of the dam foundation can successfully mitigate theuplift pressure, and thus, the stability of the dam body has been guaranteed by the current seepage control system. Besides,driven by high water head difference, the reservoir water penetrates downstream through the deficient area of the impermeablecurtain and flows along the micro-cracks developed in rock layers P_2β_3~(2?2) and P_2β_3~(2?1), then discharges through thedrainage holes in the dam foundation.
机译:白鹤滩水电站坝址集水面积大,右岸地下水层状,坝基岩卸载裂缝发育,柱状节理玄武岩渗透各向异性突出,具有复杂的渗流控制措施。此外,蓄水后上下游水头差可达235 m,因此坝址区域的渗流场将极为复杂。本研究利用现场测量数据分析了蓄水过程中坝基的渗流场特征,并采用稳态渗流计算方法对正常水位条件下的渗流场进行了数值模拟。利用现场实测数据和数值模拟结果,对渗流控制系统的性能进行了评价,揭示了大坝基础中渗流的运动过程。分析结果表明,不透水帷幕可以有效阻止水库水通过坝基中的岩体流向坝下游,坝基的排水孔可以成功地缓解抬升压力,从而保证了坝体的稳定性。此外,在高水头差的带动下,水库水通过不透水幕的不足区向下游渗透,沿着岩层P_2 β_3~(2?2)和P_2 β_3~(2?1)形成的微裂缝流动,然后通过坝基的排水孔排出。

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