使用T2-T2放松相关性测量的页岩的表征
Dominic O Couillard1, Mohammad Sadegh Zamiri1, Bruce J Balcom1
1UNB MRI Centre, Department of Physics, University of New Brunswick, 8 Bailey Drive, Fredericton, E3B 5A3, New Brunswick, Canada.
Journal of magnetic resonance (San Diego, Calif. : 1997)
|February 26, 2026
概括
这项研究引入了一种新的T2-T2*相关度测量,用于表征有机页岩. 该技术在多孔介质中区分环境,突出其对复杂系统的分析潜力.
科学领域:
- 地质物理学 地质物理学
- 材料科学 材料科学 材料科学
- 分析化学 分析化学
背景情况:
- 复杂的多孔介质在能源等行业中至关重要.
- 有机页岩是这种介质的关键例子.
- 磁共振放松相关性测量有效地描述了多孔材料.
研究的目的:
- 为了证明有机页岩样本的特征.
- 引入和验证一种新的T2-T2*相关性测量方法.
- 探索这种技术对复合孔隙介质的分析潜力.
主要方法:
- 使用了一种新的T2-T2*磁共振二维放松相关性测量.
- 将该技术应用于有机页岩样本.
- 研究了磁场强度对测量的影响.
主要成果:
- 在T2-T2*测量成功地区分了页岩中的不同环境.
- 观察到的峰值迁移远离恒定的T2/T2*轮表示T2*并不总是异质介质中的T2的直接模拟.
- 证明了用于表征复合体多孔介质的分析潜力.
结论:
- 新的T2-T2*相关性测量方法对于有机页岩的特征是有效的.
- 该技术为复杂的多孔材料中的环境提供了宝贵的见解.
- 结果突出了在异质系统中使用T2*作为T2模拟的局限性,特别是在变化的磁场下.
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