Montmorillonite alignment induced by magnetic field: Evidence based on the diffusion anisotropy of water molecules

Diffusion coefficients of water in Na-montmorillonite (Na-mon) suspensions have been determined by pulsed-field gradient spin–echo (PGSE) NMR spectroscopy for three directions (x, y, and z), where x and y mean the directions perpendicular to the static magnetic field, and z the direction parallel to it. Diffusion anisotropy was observed in the suspensions with Na-mon weight fractions of 0.63, 1.82, and 3.32%; i.e., the diffusivity of water in the z direction is faster than that in the x or y direction. The largest diffusion anisotropy of water was observed at the Na-mon fraction of 3.32%. However, diffusion anisotropy disappeared in the suspensions with Na-mon fraction more than 5.02%. The fast diffusivity in the z direction was slightly enhanced in a stronger static magnetic field (14.1 T). These results indicate that the platelike Na-mon particles are aligned with their platelike faces parallel to the static magnetic field of NMR. We also measured diffusion coefficients of water for the z direction in the temperature range from 24 to 85 °C. The plot of diffusion coefficients of water against reciprocal temperature showed a refraction point at 65 °C. This phenomenon explicitly means that the alignment is gradually relaxed at higher temperatures.

Alignment of Na-montmorillonite particles in magnetic fields (B0B0) was revealed based on the diffusion anisotropy of water detected by pulsed-field gradient spin–echo (PGSE) NMR method.Figure optionsDownload as PowerPoint slide