“…[, ]. Magnetic resonance imaging and X‐Ray computed topography can be used to observe gas hydrate distribution and reorganization in sediment samples in the laboratory [e.g., Kneafsey et al ., ; Stevens et al ., ; Bagherzadeh et al ., ; Rees et al ., ; Seol and Kneafsey , ; Kneafsey et al ., ]. In recent years, many laboratory experiments were conducted to study hydrate growth kinetics [e.g., Bagherzadeh et al ., ; Linga et al ., , ] and the gas production behavior from natural or synthetic hydrate‐bearing sediments using thermal stimulation, depressurization, or inhibitor injection [e.g., Linga et al ., ; Pang et al ., ; Tang et al ., ; Yang et al ., , ; Yuan et al ., , ].…”