Résumé
The notion of effective, time-dependent or, equivalently, apparent diffusion coefficient (ADC) and its use for characterization of porous media are revisited. It is argued that the dynamic ADC, quantifying the mean-square displacement of spin-bearing particles, should not be confused with its counterpart measured by a pulsed gradient spin echo technique. The former is an intrinsic characteristic of the medium, independent of the applied magnetic field. In contrast, the spin-echo ADC depends on the experimental setup (e.g., gradient intensity and temporal profile), raising potential ambiguities in the interpretation of diffusion-weighted measurements, which may be strongly misleading when the Gaussian phase approximation (GPA) does not hold. The oversimplified use of a single b-value is criticized. Several fitting models beyond the GPA are discussed.
| langue originale | Anglais |
|---|---|
| Pages (de - à) | 24-35 |
| Nombre de pages | 12 |
| journal | Concepts in Magnetic Resonance Part A: Bridging Education and Research |
| Volume | 36 |
| Numéro de publication | 1 |
| Les DOIs | |
| état | Publié - 14 mai 2010 |
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