Thermodynamic and hydrodynamic constraints on overpressure caused by hydrate dissociation: A pore-scale model
Version of Record online: 21 JUL 2011
Copyright 2011 by the American Geophysical Union.
Geophysical Research Letters
Volume 38, Issue 14, July 2011
How to Cite
2011), Thermodynamic and hydrodynamic constraints on overpressure caused by hydrate dissociation: A pore-scale model, Geophys. Res. Lett., 38, L14308, doi:10.1029/2011GL047937., and (
- Issue online: 21 JUL 2011
- Version of Record online: 21 JUL 2011
- Manuscript Accepted: 4 MAY 2011
- Manuscript Received: 28 APR 2011
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|grl28227-sup-0001-readme.txt||plain text document||2K||readme.txt|
|grl28227-sup-0002-txts01.pdf||PDF document||69K||Text S1. Additional details that justify the assumption of using an isothermal dissociation model and explain the expression of the effective system compressibility that results from the pressure dynamics near the advancing gas-water interface.|
|grl28227-sup-0003-ms01.mp4||MPEG-4 video||2381K||Animation S1. The evolution of pore pressure during hydrate dissociation.|
|grl28227-sup-0004-ms02.mp4||MPEG-4 video||1464K||Animation S2. Expansion and coalescence of gas clusters.|
|grl28227-sup-0005-ms03.mp4||MPEG-4 video||60K||Animation S3. The creation and propagation of a fracture as a result of hydrate dissociation in low-permeability medium.|
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