加利福尼亚州米奥森史蒂文斯砂岩中的三维孔径网络:对CO2地质储存的影响
1Department of Geological Sciences, School of Natural Sciences Mathematics and Engineering, California State University Bakersfield, Bakersfield, California 93311, United States.
概括
加利福尼亚州的史蒂文斯砂岩为二氧化碳 (CO2) 地质储存提供了显著的潜力. 孔腔结构和可湿性影响二氧化碳的注入性和捕获性,而微孔性降低了储存效率.
科学领域:
- 地质地质地质地质地质地
- 石油工程是石油工程中的一个.
- 环境科学 环境科学
背景情况:
- 米奥森史蒂文斯砂岩是加利福尼亚州二氧化碳地质储存的关键目标.
- 它的储能,密封完整性和现有基础设施使其具有吸引力.
- 了解孔隙几何和湿透性对于有效的二氧化碳注入和储存至关重要.
研究的目的:
- 研究孔隙几何和湿度如何影响史蒂文斯砂岩中的二氧化碳注入性和残留捕获.
- 分析微孔性在这种形成中的二氧化碳储存中的作用.
主要方法:
- 计算机微断层扫描图像被用来分析毛孔结构.
- 采用了孔网建模和双相流动模拟.
- 模拟考虑了各种可湿性条件:水湿,弱水湿和中性湿.
主要成果:
- 微孔区域显著增加孔隙空间,但对透度的影响有限.
- 二氧化碳注入主要通过巨孔发生,微孔稍后填充.
- 微性降低了初始和剩余的二氧化碳和,可湿性影响了这种减少的程度.
- 与湿水条件相比,中性湿水条件显示出较高的二氧化碳流动性和较低的残留捕获率.
结论:
- 孔状几何和水泥分布的异质性可能导致二氧化碳流量分层,使注射性能预测复杂化.
- 史蒂文斯砂岩对二氧化碳储存具有前景,但详细的孔隙结构特征是必不可少的.
- 集成反应性流体流是必要的,以解决矿物溶解和细菌迁移的成功实施.
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