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Use of groundwater lifetime expectancy for the performance assessment of a deep geologic radioactive waste repository: Application to a Canadian Shield environment

机译:地下水预期寿命用于深层地质放射性废物处置库性能评估的方法:在加拿大盾构环境中的应用

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摘要

F. J. Cornaton et al. (2008) introduced the concept of lifetime expectancy as a performance measure of the safety of subsurface repositories, on the basis of the travel time for contaminants released at a certain point in the subsurface to reach the biosphere or compliance area. The methodologies are applied to a hypothetical but realistic Canadian Shield crystalline rock environment, which is considered to be one of the most geologically stable areas on Earth. In an approximately 10 × 10 × 1.5 km~3 hypothetical study area, up to 1000 major and intermediate fracture zones are generated from surface lineament analyses and subsurface surveys. In the study area, mean and probability density of lifetime expectancy are analyzed with realistic geologic and hydrologic shield settings in order to demonstrate the applicability of the theory and the numerical model for optimally locating a deep subsurface repository for the safe storage of spent nuclear fuel. The results demonstrate that, in general, groundwater lifetime expectancy increases with depth and it is greatest inside major matrix blocks. Various sources and aspects of uncertainty are considered, specifically geometric and hydraulic parameters of permeable fracture zones. Sensitivity analyses indicate that the existence and location of permeable fracture zones and the relationship between fracture zone permeability and depth from ground surface are the most significant factors for lifetime expectancy distribution in such a crystalline rock environment. As a consequence, it is successfully demonstrated that the concept of lifetime expectancy can be applied to siting and performance assessment studies for deep geologic repositories in crystalline fractured rock settings.
机译:F.J.Cornaton等。 (2008年)基于在地下某一点释放的污染物到达生物圈或合规区域的传播时间,引入了预期寿命的概念,作为衡量地下储存库安全性的一种性能指标。该方法应用于假设但现实的加拿大盾构水晶岩环境,该环境被认为是地球上最稳定的地质区域之一。在大约10×10×1.5 km〜3的假设研究区域中,通过地表岩相分析和地下调查产生了多达1000个大裂缝和中裂缝区域。在研究区域,使用现实的地质和水文盾构设置分析了预期寿命的均值和概率密度,以证明该理论和数值模型可用于最佳地定位深地下储存库以安全存储乏核燃料的适用性。结果表明,一般而言,地下水的预期寿命随着深度的增加而增加,并且在主要基质块内最大。考虑了各种不确定性的来源和方面,特别是渗透性裂缝带的几何参数和水力参数。敏感性分析表明,在这种晶体岩环境中,可渗透裂缝带的存在和位置以及裂缝带渗透率与地表深度之间的关系是预期寿命分布的最重要因素。结果,成功地证明了预期寿命的概念可以用于结晶裂隙岩石环境中深部地质储层的选址和性能评估研究。

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  • 来源
    《Water resources research》 |2008年第4期|W04407-1W04407-14|共14页
  • 作者单位

    Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario, Canada;

    Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario, Canada Now at CHYN, Centre of Hydrogeology, University of Neuchatel, Neuchatel, Switzerland;

    Department of Civil and Environmental Engineering, University of Waterloo, Waterloo, Ontario, Canada;

    Department of Civil and Environmental Engineering, University of Waterloo, Waterloo, Ontario, Canada;

    Department of Earth and Environmental Sciences, University of Waterloo, Waterloo, Ontario, Canada;

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