Compressibility of unconventional gas shale formations: implications for hydrogen geo-storage

IF 5.5 0 ENERGY & FUELS
Kunming Zhang, Shimin Liu
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引用次数: 0

Abstract

Underground hydrogen storage (UHS) offers an effective solution for large-scale and safe hydrogen storage to deploy H2 as a clean energy carrier that accelerates energy transition and decarbonization. Geological H2 storage based on adsorption haven been well-identified but the studies on compressibility-based elastic storage of H2 remain limited. The objective of this study is to evaluate different compressibilities of unconventional gas shale and related implications on geological hydrogen storage. Laboratory measurements were conducted to estimate the compressibilities of shale and adsorption capacity of H2 in shale. Theoretical consideration on elastic storage of H2 through the coefficient of fluid content by a poroelastic framework was developed to compare with the H2 geo-storage based on adsorption mechanism. The results show that shale deforms linearly with gas pressure for helium, while more pronounced compression can be observed with the exposure of H2. The modeled coefficient of fluid content is well able to predict the results calculated from measured data. By extending the framework of fluid content, the elastic storage capacity of H2 was estimated as 0.0526 mmol/g at 8.5 MPa while the excess adsorption amount of H2 in shale was measured as 0.03043 mmol/g at the same pressure. The results reveal that the compressibility-based elastic storage of H2 in unconventional gas shale is not negligible due to its large potential with continuous gas injection. Additionally, strain hysteresis effects were observed after H2 injection and depletion in shale, which is potentially caused by permanent structural alteration of shale. This structural variation promotes the elongation of gas pathway that enhances the permeability and further injectivity and recoverability of H2.
非常规页岩气地层的可压缩性:对储氢的影响
地下储氢(UHS)为大规模安全储氢提供了有效的解决方案,将氢气作为加速能源转型和脱碳的清洁能源载体。基于吸附的地质储氢已经被很好地识别,但基于压缩的弹性储氢研究还很有限。本研究的目的是评价非常规气页岩的不同可压缩性及其对地质储氢的影响。通过实验室测量,估算了页岩的可压缩性和页岩对H2的吸附能力。提出了基于孔隙弹性框架的含液系数对氢气弹性储存的理论考虑,并与基于吸附机理的氢气地质储存进行了比较。结果表明,页岩的变形随氦气压力的增加呈线性变化,而在H2的作用下,页岩的压缩作用更为明显。所建立的流体含量系数能较好地预测实测数据的计算结果。通过扩展流体含量框架,估算出8.5 MPa下页岩中H2的弹性储容量为0.0526 mmol/g,相同压力下页岩中H2的过量吸附量为0.03043 mmol/g。结果表明,非常规气页岩中基于压缩率的H2弹性储层不可忽视,连续注气潜力巨大。页岩注氢枯竭后存在应变滞后效应,这可能是由于页岩的永久性结构改变所致。这种结构变化促进了气路的延伸,从而提高了渗透率,进一步提高了H2的注入性和可采性。
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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来源期刊
CiteScore
11.20
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0.00%
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