在凝灰岩和海藻酸盐中的宏观扩散,mri测量

Michel Letellier , Barbara Brunet-Imbault , Sabrina Mariez , Simone Prigent
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引用次数: 2

摘要

虽然脉冲场梯度实验允许在不同的时间和长度尺度上测量扩散系数,但使用宏观方法可能会有一些兴趣。通过质子核磁共振观察宏观扩散的结果。对于石灰石中的水,分析表面涂层后的浓度曲线可以提供精确的测量。对于在藻酸盐凝胶或初始藻酸盐溶液中扩散的二价离子,反应前沿位置允许进行扭曲度比较。最后一部分的创新之处在于将协同现象形象化。此外,它还可以估计螯合的最大反应时间(1 ms)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Diffusion macroscopique dans un tuffeau et un alginate, mesure IRM

Although Pulsed Field Gradient experiments allow measuring a diffusion coefficient at different time and length scales, it may be of some interest to use macroscopic methods. The result of a macroscopic diffusion is viewed here by proton MRI. For water in a limestone, analysing a concentration profile following a superficial coating gives a precise measure. For a divalent ion diffusing in an alginate gel or in the initial alginate solution, the reaction front position allows a tortuosity comparison. The originality of the last part is to visualize the syneresis phenomenon. Moreover, it makes it possible to estimate the maximum reaction time for the chelation (1 ms).

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