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R. Holtzman and R. Juanes Thermodynamic and hydrodynamic constraints on overpressure caused by hydrate dissociation: A pore-scale model Geophysical Research Letters 38

Article first published online: 21 JUL 2011 | DOI: 10.1029/2011GL047937

Key Points

  • Dissociation-induced overpressure is governed by thermodynamics & hydrodynamics
  • Rapid pressure buildup by dissociation can only be sustained by continuous heating
  • The overpressure is constrained by the capillary/fracturing thresholds

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