使用H核磁共振光谱学评估砂岩储存库中的储量
Son T Dang1, Sidi Mamoudou1, Chandra S Rai1
1Mewbourne School of Petroleum and Geological Engineering, The University of Oklahoma, Norman, OK 73019, USA. dangthaison@ou.edu.
Physical chemistry chemical physics : PCCP
|December 23, 2024
概括
这项研究使用1H核磁共振 (NMR) 光谱评估了比利亚沙岩中的储存. 作为一种自由气体,不论水和度如何,都会填充孔隙空间,在循环过程中没有观察到过歇斯底里.
科学领域:
- 地质科学 地质科学
- 储能 储能 储能 储能 储能 储能
- 材料科学 材料科学 材料科学
背景情况:
- 地下储 (UHS) 是可再生能源整合的关键技术.
- 了解在多孔介质中的行为对于高效和安全的UHS至关重要.
- 像砂岩这样的多孔岩石是潜在的地下储存储库.
研究的目的:
- 为了评估比利亚砂岩的气储存能力.
- 在不同的水和度条件下描述的行为和储存机制.
- 为了研究在注入和生产周期期间潜在的歇斯底里作用.
主要方法:
- 使用了1H核磁共振 (NMR) 光谱.
- 在比利亚砂岩样本上进行实验.
- 多种水和水平来模拟不同的水库条件.
主要成果:
- 成功描述了多孔岩石中的反应.
- 确定了储存机制,证实它表现为自由气相.
- 证明注入的占据空孔体积,无论水和状态如何.
- 在注入和生产周期中没有观察到歇斯底里.
结论:
- 伯利亚砂岩有效地将气作为一种自由气体储存起来.
- 在这种岩石类型中,气储存能力并没有受到水和的显著限制.
- 缺失歇斯底里表明,在储存和提取过程中,可以预测的行为.
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