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Self-organization and shock waves in underground methanation reactors and hydrogen storages

机译:地下甲烷化反应器和氢存储中的自组织和冲击波

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We consider coupled hydrodynamic and biochemical phenomena that occur in an underground porous reservoir, in which a mixture of hydrogen with other gases has been injected. The presence of methanogenic bacteria in geological strata initiates the natural underground methanation, i. e., the conversion of the mixture of H-2 and CO2 into methane. Such a transformation increases the energy of the stored gas, as the energy potential of methane is higher than that of hydrogen. Consequently, such an underground methanation can represent the basis of a new industrial technology of energy storing and enrichment. In the present paper, we give the mathematical model of bacterial kinetics, closely related to the metabolism of bacteria. We formulate the mathematical model of the process and give qualitative mathematical analysis of various scenarios of gas behavior. In practice, the mixture of hydrogen with other gases is produced by the underground coal gasification, which gives syngas (H-2, CO and CO2) or town gas (H-2, CO, CH4 and CO2). After storing, the enriched mixture can be extracted and used as fuel or transformed into electricity in gas-fired turbines. The same processes also occur when pure hydrogen is injected in underground storage of natural gas. Such technique is applied to store exceedingly produced electricity: electricity is converted to hydrogen by electrolyzers and injected into geological strata.
机译:我们考虑在地下多孔储层中发生的流体动力学和生化耦合现象,其中注入了氢气和其他气体的混合物。地质层中产甲烷细菌的存在引发了自然地下甲烷化,即例如,将H-2和CO2的混合物转化为甲烷。由于甲烷的势能比氢的势能高,因此这种转变增加了所存储气体的能量。因此,这种地下甲烷化可以代表能量存储和富集的新工业技术的基础。在本文中,我们给出了细菌动力学的数学模型,它与细菌的代谢密切相关。我们制定了过程的数学模型,并对各种气体行为情景进行了定性数学分析。实际上,氢气与其他气体的混合物是通过地下煤气化产生的,这产生了合成气(H-2,CO和CO2)或城市煤气(H-2,CO,CH4和CO2)。储存后,富集的混合物可被提取并用作燃料,或在燃气轮机中转化为电能。当将纯氢气注入地下天然气时,也会发生相同的过程。这种技术用于存储大量产生的电能:电能通过电解槽转化为氢气,然后注入地质层。

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