Behaviors
of gas and water production from a gas hydrate
reservoir
are based on fully coupled Thermal–Hydraulic–Chemical
(THC) processes in porous media. Studies using experiments and mathematical
models could be improved in hydrate-bearing sediments in the laboratory.
The experiment of depressurization-induced methane hydrate dissociation
via a single vertical well was carried out in quartz sands in a pilot-scale
hydrate simulator (PHS). The multi-stage hydrate dissociation process,
including the free liquid release, well shutdown, depressurization,
and constant pressure, was achieved by complex manual operation of
the production well in the experiment. A full implicit simulator of
hydrate (FISH), a four-component, three-phase mathematical model,
was developed and employed to reproduce the hydrate dissociation experiment.
The kinetics of the hydrate reaction, heat/mass transfer in porous
media, and mass conservation in the pressure vessel were validated
by the experimental results. The key finding of this study is the
acquisition of a group of unified parameters in a suitable mathematical
model that could clearly elucidate the hydrate dissociation process
in all stages. The mean absolute percentage error (MAPE) values of
the gas and aqueous production are, respectively, as low as 2.338
and 9.630%. The strong confidence of the accuracy of the numerical
simulator has been built up after the analysis of the experiment and
the numerical simulation in this study, which could be used to evaluate
gas recovery from marine hydrate reservoirs.