Transverse relaxation times T2 spectra for models of thawing hydrate-bearing sediment have been studied in this work. The samples were prepared from aqueous THF solution and powders of quartz microspheres or their mixtures with kaolin. It was shown that individual bands in the spectra of T2 times are traced, they correspond to proton relaxation in solid hydrate, aqueous solution of THF and to a thin layer of liquid located at the boundary between hydrate and solid particles. It was experimentally established that the low-field NMR may be applied to study the formation/melting kinetics of THF hydrates in porous media and as a tool to investigate phase transformations in porous media.
