Abstract
A new approach for monitoring diffusion in anisotropic phases is proposed and demonstrated. The method relies on the observation of dilute spins (e.g., 13C) in the presence of heteronuclear high-power dipolar decoupling, a procedure which can yield time-domain nuclear magnetic resonance (NMR) signals lasting over three orders of magnitude longer than their 1H counterparts. This allows one to apply conventional 90–180 ° pulsed-gradient spin-echo (PGSE) schemes on organic systems without having to employ complex and highly sensitive multiple-pulse 1H irradiation schemes. Instrumental aspects of this 13C method are discussed, and an application to the variable-temperature determination of anisotropic self-diffusion in a thermotropic liquid crystal is illustrated.
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