考利尼特-地流体接口的分子行为:与地质碳封存有关的边缘缺陷的作用
Jiangtao Pang1,2, Hongye Xu3,4, Qi Li1,2
1State Key Laboratory of Geomechanics and Geotechnical Engineering Safety, Institute of Rock and Soil Mechanics, Chinese Academy of Sciences, Wuhan 430071, China.
Langmuir : the ACS journal of surfaces and colloids
|June 30, 2025
概括
地质碳捕集采用高利尼特作为顶岩. 分子动力学揭示了CO2扩散因考利尼特表面而异,影响碳捕获和储存策略以实现净零目标.
科学领域:
- 地质化学 地质化学
- 材料科学 材料科学 材料科学
- 环境科学 环境科学
背景情况:
- 地质碳捕获 (GCS) 对于净零目标至关重要.
- 考利尼特石对GCS的有效性至关重要.
- 了解二氧化碳-高化物相互作用是安全储存的关键.
研究的目的:
- 调查二氧化碳在高岩-水界面上的行为.
- 分析二氧化碳扩散动力学在高酸盐缺陷附近,如纳米.
- 阐明影响二氧化碳保留和转移在富含粘土的系统中的因素.
主要方法:
- 采用了分子动力学模拟.
- 专注于二氧化碳在高利尼特-水接口的行为.
- 检查了与西洛,吉布石和边缘表面的相互作用,包括纳米.
主要成果:
- 碳二氧化碳扩散系数在考利尼特表面上有所不同 (西洛<基布石/边缘).
- 疏水性锡洛干表面表现出更高的二氧化碳亲和力和保留.
- 纳米谷主要通过中央和西洛相邻区域进入;纳米泡的形成受到压力屏障的限制.
结论:
- 考利尼特的表面特性显著影响了 GCS 中的 CO2 流动性和保留.
- 缺陷结构,如纳米,对二氧化碳的进入构成障碍.
- 通过改进的GCS,研究结果为可持续化学和碳中和战略提供了信息.
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