Abstract
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.
| Original language | English |
|---|---|
| Pages (from-to) | 24-35 |
| Number of pages | 12 |
| Journal | Concepts in Magnetic Resonance Part A: Bridging Education and Research |
| Volume | 36 |
| Issue number | 1 |
| DOIs | |
| Publication status | Published - 14 May 2010 |
Keywords
- ADC
- Diffusion-weighted imaging
- Geometry
- NMR
- PGSE
- Restricted diffusion
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