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水流路径分析:瑞典一个潜在地质处置库的方法及示例计算

Analysis of water flow paths: methodology and example calculations for a potential geological repository in Sweden.

作者信息

Werner Kent, Bosson Emma, Berglund Sten

机构信息

Golder Associates AB, Stockholm, Sweden.

出版信息

Ambio. 2006 Dec;35(8):425-34. doi: 10.1579/0044-7447(2006)35[425:aowfpm]2.0.co;2.

DOI:10.1579/0044-7447(2006)35[425:aowfpm]2.0.co;2
PMID:17334050
Abstract

Safety assessment related to the siting of a geological repository for spent nuclear fuel deep in the bedrock requires identification of potential flow paths and the associated travel times for radionuclides originating at repository depth. Using the Laxemar candidate site in Sweden as a case study, this paper describes modeling methodology, data integration, and the resulting water flow models, focusing on the Quaternary deposits and the upper 150 m of the bedrock. Example simulations identify flow paths to groundwater discharge areas and flow paths in the surface system. The majority of the simulated groundwater flow paths end up in the main surface waters and along the coastline, even though the particles used to trace the flow paths are introduced with a uniform spatial distribution at a relatively shallow depth. The calculated groundwater travel time, determining the time available for decay and retention of radionuclides, is on average longer to the coastal bays than to other biosphere objects at the site. Further, it is demonstrated how GIS-based modeling can be used to limit the number of surface flow paths that need to be characterized for safety assessment. Based on the results, the paper discusses an approach for coupling the present models to a model for groundwater flow in the deep bedrock.

摘要

与深层基岩中乏核燃料地质处置库选址相关的安全评估,需要确定潜在的水流路径以及源自处置库深度的放射性核素的相关运移时间。本文以瑞典的拉克塞马尔候选场址为例,描述了建模方法、数据整合以及由此得到的水流模型,重点关注第四纪沉积物和基岩上部150米。示例模拟确定了到地下水排放区的水流路径以及地表系统中的水流路径。尽管用于追踪水流路径的粒子是在相对较浅的深度以均匀的空间分布引入的,但大多数模拟的地下水水流路径最终都流向主要地表水和沿海岸线区域。计算得出的地下水运移时间决定了放射性核素衰变和滞留的可用时间,平均而言,到达沿海湾的时间比到达该场址其他生物圈对象的时间更长。此外,还展示了如何使用基于地理信息系统的建模来限制安全评估中需要表征的地表水流路径数量。基于这些结果,本文讨论了一种将当前模型与深部基岩中地下水流动模型耦合的方法。

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