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A discussion on hydrogen migration in rock salt for tight underground storage with an insight into a laboratory setup

机译:岩盐氢迁移探讨了实验室设置

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Hydrogen is being regarded as a primary vector in the energy transition process towards a less polluted planet. The tremendous and increasing energy demands necessitate finding large-scale storage techniques. Underground salt caverns seem to be promising. Nevertheless, the fast solicitations (thermal and mechanical) of these caverns, to reply to the fast demands, imply damage to the ambient rock salt. There is a general scientific ambiguity about the transport mechanisms taking place in the rock salt intact/damaged, particularly for hydrogen. In this paper we provide a detailed review about these transport mechanisms while the cavern undergoes cycling. This review helped us define a mathematical approach to simulate hydrogen migration in the rock salt around underground caverns. We ended up by presenting a patent laboratory setup that we are currently using to define any required model parameters experimentally.
机译:氢被认为是能量过渡过程中的主要载体朝向较少污染的行星。 能源需求的巨大和越来越多的能源需求需要找到大规模的存储技术。 地下盐洞似乎很有前景。 然而,这些洞穴的快速征求(热电和机械),回复了快速要求,暗示对环境岩盐造成损害。 关于岩盐完整/损坏的运输机制存在一般科学歧义,特别是对于氢气。 在本文中,我们在洞穴经历循环时提供关于这些运输机制的详细审查。 该评论帮助我们定义了一种数学方法来模拟地下洞穴周围的岩盐中的氢迁移。 我们通过提出我们目前正在使用的专利实验室设置来确定我们正在通过实验定义任何所需的模型参数。

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