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Self-diffusion in periodic porous media: a comparison of numerical simulation and eigenvalue methods
L M Schwartz1, D J Bergman, K J Dunn
1Schlumberger-Doll Research, Ridgefield, CT 06877-4108, USA.
Magnetic Resonance Imaging
|January 1, 1996
Summary
Random walk simulations aid magnetic resonance in porous media. Comparing pulsed field gradient spin echo (PGSE) data with eigenvalue expansions in simple geometries offers valuable insights into water diffusion.
Area of Science:
- Physics
- Chemistry
- Materials Science
Background:
- Magnetic resonance measurements are crucial for studying porous media.
- Random walk computer simulations are widely used to understand these measurements.
- Pulsed Field Gradient Spin Echo (PGSE) experiments measure molecular displacement over time.
Purpose of the Study:
- To describe PGSE experiments and analyze water diffusion in porous media.
- To compare simulation data with exact eigenvalue expansions for improved accuracy.
- To focus on time-dependent magnetization and particle return probability.
Main Methods:
- Utilizing random walk computer simulations.
- Employing simple periodic geometries for analysis.
- Comparing simulation results with exact eigenvalue expansions.
- Analyzing wavevector and time-dependent magnetization (M(k, t)).
- Calculating normalized probability of particle return (Ps(delta R, t)).
Main Results:
- PGSE simulations in simple periodic geometries provide valuable insights.
- Comparison with eigenvalue expansions enhances understanding of diffusion.
- The study analyzes magnetization decay and particle displacement probabilities.
Conclusions:
- Random walk simulations combined with eigenvalue expansions offer a robust method for studying diffusion in porous media.
- This approach improves the understanding of magnetic resonance measurements.
- The findings are applicable to various fields utilizing diffusion measurements in complex environments.