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对破裂多孔介质中巴里特沉的核化速率和向速率的控制
Qiu-Rong Jiang1,2, Ran Hu1,2, Hang Deng3
1State Key Laboratory of Water Resources Engineering and Management, Wuhan University, Wuhan 430072, China.
Langmuir : the ACS journal of surfaces and colloids
|January 9, 2025
概括
这项研究揭示了破裂岩石中两种不同的矿物沉模式,影响透性和污染物传输. 了解这些系统对于在各种应用中准确的反应式运输建模至关重要.
科学领域:
- 地质化学 地质化学
- 环境科学 环境科学
- 石油工程是石油工程中的一个.
背景情况:
- 矿物沉会改变地下的透性,影响流体流动和污染物运输.
- 之前对破裂介质中的巴里特沉的研究缺乏在不同条件下对孔尺度机制的理解.
研究的目的:
- 在破裂的多孔系统中调查孔尺度矿物沉动态.
- 识别和描述不同的降水模式及其控制因素.
主要方法:
- 进行了真实岩石微流体实验.
- 使用X射线衍射 (XRD) 和扫描电子显微镜与能量分散式X射线光谱学 (SEM-EDS) 来量化巴里特沉动态.
- 导向和核化速率的理论分析定义了一个无维数 (Da).
主要成果:
- 确定了两种不同的降水模式:在断裂表面 (模式I) 和变化区域 (模式II).
- 定义了一个无维数 (Da),根据流量和降水率来区分这两种模式.
- 模式I (表面降水) 在高Da数 (高降水率相对于流速) 时是最受欢迎的.
结论:
- 降水模式显著影响破碎的多孔介质的透性,质量转移和污染物分布.
- 这些发现对于准确建模各种应用中的反应式运输至关重要,例如碳捕获和污染物修复.
- 这项研究提供了对破裂系统中孔尺度降水动态的机制性理解.
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