在多孔介质中测量速度,使用稳定状态自由前行-用流量分析Bloch-Torrey方程的解析解
Mohammad Sadegh Zamiri1, Naser Ansaribaranghar1, Benedict Newling1
1UNB MRI Centre, Department of Physics, University of New Brunswick, Fredericton, New Brunswick E3B 5A3, Canada.
The Journal of chemical physics
|December 22, 2025
概括
这项研究使用磁共振稳态自由前行 (SSFP) 测量了多孔介质中的流体速度. 通过分析流动诱导的磁化扭曲,SSFP技术可以准确地非侵入性地确定流体速度.
科学领域:
- 地质物理学 地质物理学
- 流体动力学 流体动力学
- 磁共振成像技术 磁共振成像技术
背景情况:
- 在多孔介质中精确测量流体速度对于理解地下过程至关重要.
- 传统的流体速度测量方法可能具有侵入性或缺乏精度.
- 磁共振 (MR) 技术提供了非侵入性成像能力.
研究的目的:
- 开发和验证一种非侵入性方法,用于测量在多孔介质中的流体速度.
- 为了利用磁共振稳态自由前行 (SSFP) 技术来量化流速.
- 分析模拟流体流动对SSFP信号的影响.
主要方法:
- 磁共振稳态自由前行 (SSFP) 技术的应用.
- 使用富里埃数列来模拟流动效应的布洛赫-托雷方程的分析解决方案.
- 在稳定的流量条件下使用本海默砂岩核心插头进行实验验证.
主要成果:
- 在稳定流下的SSFP测量显示定期稳定状态磁化对流量高度敏感.
- 分析解决方案准确地预测了由于流体流动而导致的稳定状态响应的扭曲.
- 精确确定流体速度是通过非侵入性方法实现的.
结论:
- SSFP技术与分析建模相结合,提供了一种准确且非侵入性的方法,用于在多孔介质中测量流体速度.
- 这种方法可以详细描述多孔岩石样本中的流体动力学.
- 这些发现对需要进行地下流量分析的各种领域有影响.
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