对控制CO2泄漏机制的地下过程进行批判性审查
Haidar Ali AlAhmad1, Shiqi Liu1, Ali Alabdrabulrasul1
1Physical Science and Engineering Division, King Abdullah University of Science and Technology, Thuwal, Saudi Arabia.
Advances in colloid and interface science
|December 30, 2025
概括
地质二氧化碳 (CO2) 在盐水层中的储存是有希望的,但面临泄漏风险. 本次审查澄清了不同的盐水和二氧化碳泄漏机制,并评估了安全地下封闭的模型.
科学领域:
- 地球科学 地球科学 地球科学
- 环境科学 环境科学
- 地质地质地质地质地质地
背景情况:
- 二氧化碳 (CO2) 的地质储存是减少大气度的一个关键策略.
- 由于其广泛的可用性,封闭的盐水层受益于二氧化碳的封存.
- 人们仍然担心二氧化碳储存的安全性,特别是可能泄漏到淡水含水层.
研究的目的:
- 从地质储存场所中批判性地审查和区分盐水和二氧化碳泄漏的机制.
- 检查二氧化碳制各种建模方法的假设,适用性和局限性.
- 识别知识缺口,以提高地下二氧化碳储存的安全性.
主要方法:
- 关于二氧化碳和盐水泄漏现有研究的文献综述.
- 分析分析,半分析和数值建模技术用于泄漏评估.
- 批判性评估模型假设及其对预测流体迁移的影响.
主要成果:
- 盐水泄漏主要是由压力差异驱动的,而二氧化碳泄漏是由和动态控制的.
- 泄漏也可能发生在地质缺陷中,如微碎裂和密封不良的井.
- 现有的模型在准确表现这些不同的泄漏过程的能力上有所不同.
结论:
- 清晰地区分盐水和二氧化碳泄漏机制对于准确的风险评估至关重要.
- 需要进一步的研究来完善模型,以解释盐水层中复杂的水文挑战.
- 改进的建模将提高地质二氧化碳储存的安全性和可靠性.
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