通过酶诱导碳酸盐沉 (EICP) 方法对断裂密封的孔尺度研究表明它对CO2存储管理的潜力
Mohammad Hemayati1,2, Hamed Aghaei3, Alireza Daman Shokouh1
1Department of Civil and Environmental Engineering, School of Engineering, Shiraz University, P.O.Box 71348-51156, Shiraz, Iran.
Scientific reports
|August 1, 2024
概括
酶诱导的碳酸盐沉有效地封闭了地质裂,大大减少了二氧化碳泄漏. 这一孔尺度研究显示,仅仅在一个处理周期后,导电性就显著降低了.
科学领域:
- 地质化学 地质化学
- 地质地质地质地质地质地
- 环境科学 环境科学
背景情况:
- 地质断层作为关键的地下流道.
- 卡普罗克的断裂可能导致不良的气体泄漏,造成环境和安全问题.
- 控制通过裂的地下流动对于碳捕获等应用至关重要.
研究的目的:
- 为了研究在岩石断裂中酶诱导碳酸盐沉的孔尺度动态.
- 为了评估这种降水对二氧化碳 (CO2) 泄漏的影响.
- 为了提供这个现象的第一个孔尺度视角.
主要方法:
- 使用岩石微流体流动细胞进行实验.
- 采用实时光学和扫描电子显微镜进行监测.
- 进行流量模拟以评估二氧化碳导电性变化.
主要成果:
- 观察到由酶诱导的碳酸盐沉动态,主要是在前三次注射周期内.
- 在第六个注射周期时,骨折孔完全关闭.
- 流量模拟预测,在第一个处理周期后,二氧化碳导电率降低了25%.
结论:
- 酶诱导的碳酸盐沉是一种可行的方法,可以减轻通过地质断层的二氧化碳泄漏.
- 显著的密封效应迅速发生,即使在初始处理后也观察到导电率的大幅降低.
- 建议进行进一步的研究,以探索不同的分辨率,测试条件和3D调查.
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