含水层中氢指进行为的数值评价

IF 5.5 0 ENERGY & FUELS
Cunqi Jia , Jinchuan Hu , Kamy Sepehrnoori
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引用次数: 0

摘要

地下储氢是解决大规模、长期和经济上可行的氢保存挑战的一种战略,满足了可再生能源框架的能源需求并平衡了供应差异。本研究旨在研究和评估氢气注入过程中的指法行为。通过数值算例,评价了不同的模拟场景和流体-岩石相互作用参数、地层非均质性等敏感影响因素对指理流动的影响。比较了不同网格放大方案在放大注氢过程中的计算效率。结果表明,由于氢气和盐水流动能力的差异,在注氢过程中确实会产生指动流动。指流特性对含盐含水层的驱氢性能有显著影响。含盐含水层中的氢置换路径对自相关长度的变化高度敏感。与平均升级方案相比,相同统计量的升级方案可以防止数值模拟特性的显著损失。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Numerical evaluation of fingering behavior for hydrogen in aquifers
Underground hydrogen storage emerges as a strategy to address the challenge of large-scale, long-term, and economically viable hydrogen preservation, fulfilling energy demands and balancing supply discrepancies in renewable energy frameworks. This study is motivated to investigate and evaluate the fingering behavior during the hydrogen injection process. Numerical cases are performed to evaluate different simulation scenarios and sensitive influencing factors, such as fluid-rock interaction parameters and formation heterogeneity cases, on the influence of fingering flow. Different mesh upscaling schemes are compared to computational efficiency in the scale-up hydrogen injection process. Results show that fingering flow can indeed be induced during the hydrogen injection process due to the difference in flow capability between hydrogen and saline water. The characteristics of fingering flow significantly impact the performance of hydrogen displacement in saline aquifers. The hydrogen displacement path in the saline aquifer is highly sensitive to variations in the autocorrelation length. Compared to the averaging upscaling scenario, the same-statistic upscaling scenario can prevent a significant loss of numerical simulation characteristics.
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来源期刊
CiteScore
11.20
自引率
0.00%
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