Exploration activities around the world have confirmed that in situ hydrate
s are widely available in permafrost and oceanic sediments. These hydrocarb
on deposits have stimulated worldwide efforts to understand gas production
from hydrate dissociation in a porous media. This work is a contribution to
wards these efforts. The present study uses depressurization-driven in situ
hydrate dissociation, incorporates decomposition kinetics into the radial
diffusivity equation, and develops a model to predict the performance of na
turally occurring hydrates. The proposed model is simple yet useful and it
does not require any empirical correlation. The model-predicted performance
compares well with the published experimental studies on the hydrate disso
ciation in porous media. (C) 2001 Elsevier Science B.V. All rights reserved
.