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Impact of Water Consumption and Saturation- Dependent Corrosion Rate on Hydrogen Generation and Migration from an Intermediate-Level Radioactive Waste Repository

机译:耗水量和饱和度相关的腐蚀速率对氢在中级放射性废物处置库中产生和迁移的影响

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The corrosion of metals contained in intermediate-level long-lived waste (ILW) under reduced chemical condition will lead to the production of hydrogen gas during the post-closure phase of a deep geological repository for radioactive waste. According to previous investigations by Talandier et al. (Proceedings of TOUGH symposium 2006, Berkeley, 2006), the period of concern covers several 1,000 years after closure of a repository in a clay host rock (Callovo-Oxfordian). The limited hydrogen transport efficiency of the host rock will lead to significant saturation of the concrete waste canister pore space and voids with a gas phase and pressure build-up within the emplacement drifts. On the other hand, the water availability is limited as a result of (i) the low permeability of the clay host rock and (ii) the desaturation of the rock mass close to the drift wall due to the ventilation of the drifts during the operational phase of the repository. In former numerical simulations it was assumed that under the reducing chemical conditions prevailing in the repository, the corrosion rate would be a function of the available metal surface and the temperature only. In this paper, simulation results based on new phenomenological functions are presented, which were implemented in T0UGH2. These allow taking into account (i) a water saturation dependency of the hydrogen generation rate, (ii) the water consumption due to the corrosion process, and (iii) the total metal mass available for corrosion. The paper presents results of ID radial and 2D vertical simulations of a typical cross-section of a waste emplacement drift and the surrounding rock mass. The interactions between water availability from the low permeable clay, the dependency of the hydrogen generation rates from the water saturation of the waste package and the hydrogen migration in the host rock are demonstrated.
机译:在化学条件降低的情况下,中级长寿命废物(ILW)中所含金属的腐蚀将导致在放射性废物深层地质处置库的关闭后阶段产生氢气。根据Talandier等人先前的调查。 (2006年TOUGH研讨会论文集,伯克利,2006年),所关注的时期涵盖了在粘土基质岩石中(Callovo-Oxfordian)封闭储层之后的1000年。母岩有限的氢传输效率将导致混凝土废料罐的孔隙空间和空隙显着饱和,并且在位移区内会形成气相和压力。另一方面,由于(i)粘土基质岩石的低渗透性和(ii)在运行期间由于漂移的通风而使靠近漂移壁的岩体的饱和度降低,限制了水的可用性。存储库的阶段。在以前的数值模拟中,假设在储存库中普遍存在的化学还原条件下,腐蚀速率将仅是可用金属表面和温度的函数。本文提出了基于新现象学功能的仿真结果,并在T0UGH2中实现。这些允许考虑(i)氢生成速率的水饱和度依赖性,(ii)由于腐蚀过程而消耗的水,以及(iii)可用于腐蚀的总金属量。本文介绍了废物填埋场漂移和周围岩体的典型横截面的ID径向和二维垂直模拟结果。证明了低渗透性粘土的水有效性,废物包的水饱和度对氢生成速率的依赖性以及基质岩石中氢迁移之间的相互作用。

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