“…In this work, the low‐field NMR technique is used to monitor the formation and dissociation processes of gas hydrate in sedimentary rocks with different pore size distribution. Methane is used to form gas hydrate, instead of tetrahydrofuran (Gao et al, ; Song et al, ), carbon dioxide (Chen et al, ; Chernov et al, ; Falenty et al, ; Yang et al, ), and Freon (Elistratov et al, ; WitteBolle & Sego, ), which can simulate the real gas hydrate conditions beneath the Earth. Four samples with different pore size distributions are used in our experiments, aiming to consider the effect of pore structure on the formation and dissociation behaviors of the gas hydrate.…”