首页> 外文期刊>Hydrogeology journal >Trends, prospects and challenges in quantifying flow and transport through fractured rocks
【24h】

Trends, prospects and challenges in quantifying flow and transport through fractured rocks

机译:定量分析裂隙岩石中的流动和输运的趋势,前景和挑战

获取原文
获取原文并翻译 | 示例
           

摘要

Among the current problems that hydrogeologists face, perhaps there is none as challenging as the characterization of fractured rock (Faybishenko and Benson 2000). This paper discusses issues associated with the quantification of flow and transport through fractured rocks on scales not exceeding those typically associated with single- and multi-well pressure (or flow) and tracer tests. As much of the corresponding literature has focused on fractured crystalline rocks and hard sedimentary rocks such as sandstones, limestones (karst is excluded) and chalk, so by default does this paper. Direct quantification of flow and transport in such rocks is commonly done on the basis of fracture geometric data coupled with pressure (or flow) and tracer tests, which therefore form the main focus. Geological, geophysical and geochemical (including isotope) data are critical for the qualitative conceptualization of flow and transport in fractured rocks, and are being gradually incorporated in quantitative flow and transport models, in ways that this paper unfortunately cannot describe but in passing. The hydrogeology of fractured aquifers and other earth science aspects of fractured rock hydrology merit separate treatments. All evidence suggests that rarely can one model flow and transport in a fractured rock consistently by treating it as a uniform or mildly nonuniform isotropic continuum. Instead, one must generally account for the highly erratic heterogeneity, directional dependence, dual or multicomponent nature and multiscale behavior of fractured rocks. One way is to depict the rock as a network of discrete fractures (with permeable or impermeable matrix blocks) and another as a nonuniform (single, dual or multiple) continuum. A third way is to combine these into a hybrid model of a nonuniform continuum containing a relatively small number of discrete dominant features. In either case the description can be deterministic or stochastic. The paper contains a brief assessment of these trends in light of recent experimental and theoretical findings, ending with a short list of prospects and challenges for the future.
机译:在水文地质学家当前面临的问题中,也许没有比裂隙岩的鉴定更具挑战性(Faybishenko和Benson 2000)。本文讨论了与不超过单井和多井压力(或流量)和示踪剂测试通常不相关的,通过裂隙岩的流动和输运量化相关的问题。由于许多相应的文献都集中在破裂的晶体岩和坚硬的沉积岩上,例如砂岩,石灰石(不包括岩溶)和白垩,因此默认情况下本文也不做。通常在此类岩石中直接定量分析流量和运移,是基于裂缝的几何数据,压力(或流量)和示踪剂测试,因此成为重点。地质,地球物理和地球化学(包括同位素)数据对于定性裂隙岩石中的流动和输运的概念化至关重要,并且正逐渐被纳入定量流动和输运模型中,这是本文不幸地无法描述但只能通过的方式。裂隙含水层的水文地质学和裂隙岩石水文学的其他地球科学方面值得单独处理。所有证据表明,很少有人能够通过将裂隙岩视为均匀或轻微不均匀的各向同性连续体来始终如一地模拟裂隙岩中的流动和运移。取而代之的是,通常必须考虑裂缝岩的高度不稳定的非均质性,方向依赖性,双组分或多组分性质以及多尺度行为。一种方法是将岩石描述为离散裂缝的网络(具有可渗透或不可渗透的基质块),而另一种则可以描述为不均匀的(单,双或多)连续体。第三种方法是将它们组合成包含相对较少的离散主导特征的不均匀连续体的混合模型。在任何一种情况下,描述都可以是确定性的或随机的。本文根据最近的实验和理论发现对这些趋势进行了简要评估,最后列出了对未来的展望和挑战。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号