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Development of approaches for modelling coupled thermal-hydraulic-mechanical-chemical processes in single granite fracture experiments

机译:花岗岩破裂实验中热-水-力-化学-化学过程耦合建模方法的发展

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The geological formation immediately surrounding a nuclear waste disposal facility has the potential to undergo a complex set of physical and chemical processes starting from construction and continuing many years after closure. The DECOVALEX project (DEvelopment of COupled models and their VALidation against EXperiments) was established and maintained by a variety of waste management organizations, regulators and research organizations to help improve capabilities in experimental interpretation, numerical modelling and blind prediction of complex coupled systems. In the present round of DECOVALEX (D-2015), one component of Task C1 has considered the detailed experimental work of Yasuhara et al. (Appl Geochem 26: 2074-2088, 2011), wherein three natural fractures in Mizunami granite are subject to variable fluid flows, mechanical confining pressure and different applied temperatures. This paper presents a synthesis of the completed work of six separate research teams, building on work considering a single synthetic fracture in novaculite. A range of approaches are presented including full geochemical reactive transport modelling and 2D and 3D high-resolution coupled thermohydro- mechanical-chemical (THMC) models. The work shows that reasonable fits can be obtained to the experimental data using a variety of approaches, but considerable uncertainty remains as to the relative importance of competing process sets. The work also illustrates that a good understanding of fracture topography, interaction with the granite matrix, a good understanding of the geochemistry and the associated multi-scale THMC process behaviours is a necessary pre-cursor to considering predictive models of such a system.
机译:紧邻核废料处置设施的地质构造有可能经历一系列复杂的物理和化学过程,这些过程从建造开始到关闭后持续多年。 DECOVALEX项目(耦合模型的开发及其对性能的验证)是由各种废物管理组织,监管机构和研究组织建立和维护的,以帮助提高复杂耦合系统的实验解释,数值建模和盲目预测的能力。在本轮DECOVALEX(D-2015)中,任务C1的一个组成部分考虑了Yasuhara等人的详细实验工作。 (Appl Geochem 26:2074-2088,2011),其中水波花岗岩中的三个天然裂缝要经受可变的流体流动,机械围压和不同的施加温度。本文介绍了六个独立研究小组已完成工作的综合情况,并以考虑了新云母的单个合成裂缝为基础进行了研究。提出了一系列方法,包括完整的地球化学反应输运模型以及2D和3D高分辨率耦合热流体力学化学(THMC)模型。这项工作表明,可以使用多种方法对实验数据进行合理拟合,但是在竞争性工艺组的相对重要性方面仍存在相当大的不确定性。这项工作还表明,对裂缝形貌,与花岗岩基体的相互作用,对地球化学以及相关的多尺度THMC过程行为的良好理解是考虑这种系统的预测模型的必要先兆。

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