“…They typically form under high pressure (more than 0.6 MPa) and low temperatures (less than 300 K) [1,2], naturally occurring in marine and permafrost environments. Due to the huge reserves and high energy density [3][4][5], natural methane hydrates are potentially regarded as a strategic energy resource, which have attracted increasing interest worldwide [6][7][8]. To exploit CH 4 form the hydrates, several methods such as thermal treatment, depressurizing, and the addition of inhibitors into the hydrate layer, have been proposed [7,9,10].…”