Thermodynamic calculations in the system CH(sub 4)-H(sub 2)O and methane hydrate phase equilibria
Article Abstract:
A classical thermodynamic model, using experimentally determined data for phases in the system CH(sub 4)-H(sub 2)O, was developed and used to calculate the phase equilibria of methane hydrate over a wide range of geologically relevant P (Pressure) and T (temp) conditions. The results from the classical thermodynamic model are wholly consistent with little or no variation in hydrate number over a wide range of P and T conditions and are in agreement with the directly measured compositions between 2 and 10 MPa.
Publication Name: Journal of Physical Chemistry B
Subject: Chemicals, plastics and rubber industries
ISSN: 1520-6106
Year: 2006
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Direct measurement of methane hydrate composition along the hydrate equilibrium boundary
Article Abstract:
The composition of methane hydrate, namely n(sub w) for CH4.n(sub w)H2O, is directly measured along the hydrate equilibrium boundary under conditions of excess methane gas. A hydrate stoichiometry of n(sub w)= 5.81-6.10 H2O describes the entire range of measured values, with an average composition of CH4.5.99(plusmn0.07)H2O along the equilibrium boundary.
Publication Name: Journal of Physical Chemistry B
Subject: Chemicals, plastics and rubber industries
ISSN: 1520-6106
Year: 2005
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The role of water in gas hydrate dissociation
Article Abstract:
The thermal buffering behavior during dissociation of sI carbon dioxide (CO2) hydrate, as well as structure sII methane-ethane hydrate (ClC2) and SII propane (C3) hydrate at 0.1 Mpa are discussed. The relationship between hydrate dissociation and buffering temperature for these various hydrates near T(sub m) is presented.
Publication Name: Journal of Physical Chemistry B
Subject: Chemicals, plastics and rubber industries
ISSN: 1520-6106
Year: 2004
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