The pressure from the presence of gas reservoirs impacts the stability of the hydrate layer.
2.
This free gas may become trapped beneath the overlying hydrate layer forming gas pockets, or reservoirs.
3.
In areas of high geothermal heat flow, the lower limit of the HSZ may become shallower, therefore decreasing the thickness of the HSZ . Conversely, the thickest hydrate layers and widest HSZ are observed in areas of low geothermal heat flow.
मोबाइल