关于CO2溶解和矿化储存的数值模拟 - - 考虑到CO2在含水层中的水-岩石反应
Qingying Zuo1,2, Yizhong Zhang1,2, Maolin Zhang1,2
1Petroleum Engineering School, Yangtze University, Wuhan 430100, China.
ACS omega
|November 25, 2024
概括
深层盐水层中的二氧化碳 (CO2) 储存对于减缓气候变化至关重要. 最佳的储存效率取决于储特性和注入策略,而底孔穿孔是最有效的.
科学领域:
- 地质工程是地质工程.
- 环境科学 环境科学
- 化学工程是化学工程的重要组成部分.
背景情况:
- 在深层盐水层中储存二氧化碳 (CO2) 是缓解气候变化的关键策略.
- 二氧化碳在含水层中经历溶解和矿化等反应,影响储存的持久性.
- 了解二氧化碳-水-岩石相互作用对于优化储存效率至关重要.
研究的目的:
- 调查水库条件和注入方案对二氧化碳溶解和矿化的影响.
- 开发和应用一个数值模型来模拟长期的二氧化碳储存.
- 为了确定有效和安全的二氧化碳封存的最佳参数.
主要方法:
- 实验测定二氧化碳溶解度和适合二氧化碳-水-岩石反应参数.
- 使用CMG的GEM模块与奥尔多斯盆地含水层数据开发数值机制模型.
- 模拟80年的二氧化碳注入 (注入期20年) 以分析储存行为.
主要成果:
- 增加的多孔性有利于二氧化碳的储存,而过高的透性是有害的.
- 较高的二氧化碳注入速度导致储存量增加.
- 与其他方案相比,底层穿孔证明了二氧化碳溶解和矿化效率优于其他方案.
结论:
- 储水池的多孔性和透性显著影响二氧化碳储存的有效性.
- 注射速率和穿孔策略是最大限度地减少二氧化碳的关键因素.
- 底孔穿孔是增强盐水层中二氧化碳溶解和矿化最有利的配置.
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