Mérési módszer a hidrogén porózus formációkban történő tárolhatóságának vizsgálatára

Roland Dócs, Marianna Vadászi, István Szunyog
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Abstract

Összefoglalás. A Nemzeti Hidrogénstratégia kiemelt célja a villamosenergia- és földgáz-infrastruktúra együttműködésével a szezonális áramtárolási képesség megvalósítása. A villamos energia ilyen mértékű tárolása csak fizikai formában (gázmolekula) föld alatti tárolókban lehetséges. A Megújuló Energiák Nemzeti Laboratórium projekt keretében egy egyedi tervezésű és építésű kőzetvizsgáló berendezés segítségével a hidrogénnel kevert földgáz föld alatti formációkban történő elhelyezhetőségét vizsgálja. A már kiforrott API RP 40 szabványban leírt metodikát követve az eszköz újszerűsége abban rejlik, hogy a hidrogén helyett egy kontrollgáz segítségével határozzuk meg a kőzet kiinduló és megváltozott paramétereit. A cikkben bemutatásra kerül a mérési módszer szakirodalmi előzménye és maga a módosított eljárás. Summary. Hungary’s National Hydrogen Strategy is giving a priority to the seasonal storage capacity of electricity in cooperation of the existing electrical- and natural gas infrastructure. Although there are solutions for electricity storage in energy form, such as battery packs, none of them are on the scale of the needed capacity. However, the problem of seasonal storage could be solved with a different method, by converting the energy into a physically storable form via gas molecule, which can be inserted in large quantities into underground structures, thus, the problem of hydrogen storage is important (Bent 2007). In numerous papers written regarding this topic, salt domes were found to be the most potential formations for underground storage (Małachowska et al. 2022). Several existing cases can be found where hydrogen underground storage tanks were made artificially in such formations with success. In the country no salt domes are present, therefore depleted porous hydrocarbon reserves as the second most favorable solution are available for storage. However, before such actions in such formations can be taken, further research is needed regarding the long-term hydrogen storage at high pressure and temperature. One of the major concerns of hydrogen storage is the possibility of migration through the cap rock, geochemical modifications, or even structural damage of the bearing rock material. The Mining and Energy Institute of the University of Miskolc, within the framework of the National Renewable Energy Laboratory project, takes part in answering these questions. During the research, the effects of hydrogen-mixed natural gas storage are examined on rock samples taken from the potential underground porous formations. Experiments are carried out using custom-designed and built rock testing equipment with a newly developed measurement procedure. The method is based on the measurement of steady state permeability according to the well-established API RP 40 standard and is novel in that it uses a control gas rather than hydrogen itself to determine the rock parameters before and after the hydrogen treatment. The method relies on the principle presented in the experimental work made by Klinkenberg (1941), who found that permeability as a property of rock could be determined by any fluid. In theory changes developed in the samples after the hydrogen treatment can be measured and detected by the control gas. In the paper, the authors present the literature history of the measurement method and outline their proposed modified procedure.
测试多孔地层储氢能力的测量方法
Összefoglás. 在大型发电站的发电过程中,将产生大量的热量,这些热量将被转化为电能。Megújuló Energiák Nemzeti Laboratórium项目的目标是,通过对高热量、高湿度环境的监控,提高对热能的利用率。API RP 40 是一种先进的测量方法,可用于对测量数据进行分析,从而对测量参数进行精确控制。通过对控制面板的控制,可提高控制面板的性能,并可提高控制面板的稳定性。 摘要。 匈牙利的国家氢能战略优先考虑与现有的电力和天然气基础设施合作,提高季节性电力储存能力。虽然有电池组等能源形式的电力储存解决方案,但都没有达到所需容量的规模。然而,季节性储存问题可以用另一种方法来解决,即通过气体分子将能量转化为物理上可储存的形式,并将其大量植入地下结构,因此,氢气储存问题非常重要(Bent,2007 年)。在有关这一主题的众多论文中,盐穹被认为是最有潜力的地下储藏形式(Małachowska 等人,2022 年)。现有的一些案例表明,在此类地层中人工制造氢气地下储罐取得了成功。我国没有盐穹,因此枯竭的多孔碳氢化合物储量是第二种最有利的储存方案。不过,在对此类地层采取此类行动之前,还需要对高压和高温下的长期氢储存进行进一步研究。氢气储存的主要问题之一是可能通过盖岩迁移、地球化学变化,甚至对承载岩材料的结构造成破坏。米什科尔茨大学矿业与能源研究所在国家可再生能源实验室项目框架内参与回答了这些问题。在研究过程中,从潜在的地下多孔地层中提取的岩石样本对混合氢天然气储存的影响进行了研究。实验使用定制设计和制造的岩石测试设备以及新开发的测量程序进行。该方法是根据成熟的 API RP 40 标准测量稳态渗透率,其新颖之处在于使用控制气体而不是氢气本身来确定氢气处理前后的岩石参数。该方法依赖于克林肯伯格(1941 年)在实验工作中提出的原理,克林肯伯格发现作为岩石属性的渗透性可由任何流体确定。理论上,样品在氢气处理后发生的变化可以通过控制气体来测量和检测。在本文中,作者介绍了该测量方法的文献历史,并概述了他们提出的修改程序。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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