Methane hydrate dissociation mechanisms within actual sediment pore structure are revealed.
The hydrate pore habits influence the dissociation mechanisms and upscaling models.
A pore-scale numerical framework for methane hydrate dissociation is established.
A good agreement between pore-scale experiments and numerical simulations is achieved.
Upscaling parameters for the methane hydrate production forecast are provided.
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Upscaling analysis
Comparison of numerical and experimental results
Numerical results of isothermal methane hydrate dissociation
Numerical results of non-isothermal methane hydrate dissociation
Regime analysis