Natural gas hydrates are a significant potential energy source and key player in global geological climate dynamics, with our all understandings on both sides basing on hydrate stability conditions consisting of pressure (P) and temperature (T). Considering important significance of theoretical researches in two sides, whether there is another factor playing same role with P or T is worth being answered. Using molecular dynamics simulations, changes of non-clathrated water structures and gas bubbles during mechanical deformation processes of methane hydrates were investigated to characterize their destabilizing natures and the deformation is then identified as this new factor. Similar to P-T profile but at a new level of complexity, deformation also characterizes hydrates stability but in three-dimensional space form while combining with T, reflecting deeper influences of specific temperature values, hydrate purities and deformation modes on hydrates stability. Over two tensile andcompressive deformations, the mechanisms responsible for hydrate destabilization vary, with stretching favoring formation of gas bubbles and compressing damaging internal hydrogen-bond structures. Once alternating, such two to-and-fro continuing deformations can act as a piston-like accelerator as well as one-way valve for dissociation of hydrates, destabilizing them rapidly. In summary, P and T act as the prerequisite of hydrate existences, but cannot accurately account for the influence of such dynamic events as earthquakes, ocean tides, and changes of ice shelves on dissociations. This research sheds a new light on the reasonable explanation to dynamic hydrate dissociations, e.g. some abnormal disappearances of reservoirs within appropriate P-T conditions. Stronger, current bottleneck of hydrate exploitation efficiency might also be broken down; likewise, the ultra-rapid dissociation performance during the terminal procedure of hydrate-based natural gas storage/transportation technology might achieve success.
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