Kinetics of hydrate formation, dissociation and reformation
Hydrates in natural sediments are never able to reach thermodynamic equilibrium because of in balance between number of independent thermodynamic variables and constraints (conservation and equilibrium conditions). In this work I present a consistent thermodynamic approach in which all components in...
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| Format: | Article |
| Language: | English |
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Elsevier
2021-03-01
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| Series: | Chemical Thermodynamics and Thermal Analysis |
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| Online Access: | http://www.sciencedirect.com/science/article/pii/S266731262100002X |