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Permeability is a critical parameter describing flows of methane gas and water through hydrate-bearing sediments. It is also one of the most critical parameters to estimate gas production rate, which determines whether expensive deepwater drilling to produce gas from hydrate deposit is economically feasible. However, studies on permeability in hydrate-bearing sediments are limited, in part due to experimental difficulties and the phenomena per se is complex and scale dependent. This presentation discusses the basic physical processes involved in mixed fluids transport in sediments, the impacts of hydrate formation and dissociation on mixed fluids flow, and the challenges and potential solutions to enhanced understanding of the core-scale permeability in hydrate-bearing sediments.
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