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Thermodynamic and hydrodynamic constraints on overpressure caused by hydrate dissociation: A pore-scale model
R. Holtzman
, R. Juanes
Faculty Research Centre in Fluid and Complex Systems
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Article
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peer-review
31
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2
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Physics & Astronomy
overpressure
hydrates
scale models
dissociation
hydrodynamics
porosity
thermodynamics
sediments
fracturing
entry
heat of dissociation
landslides
venting
multiphase flow
thresholds
drainage
kinetics
gases
permeability
low pressure
actuators
dissipation
expansion
Earth & Environmental Sciences
overpressure
thermodynamics
hydrodynamics
sediment
heat supply
submarine landslide
geomechanics
kinetics
venting
multiphase flow
capillary pressure
phase equilibrium
gas
pore pressure
methane
drainage
timescale
permeability
rate