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A Model To Predict Gas Hydrate Equilibrium and Gas Hydrate Saturation in PorousMedia Including Mixed CO2-CH4 Hydrates

机译:包括混合CO2-CH4水合物在内的多孔介质中气体水合物平衡和气体水合物饱和度的预测模型

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Phase equilibrium of gas hydrates is altered in porous mediaas compared to bulk systems. Inside porous media, thethermodynamic potential of chemical components changes dueto molecular interactions with pore walls and due to the energyrequired to maintain capillary equilibrium. A pore-freezingmodel was developed that can be used to predict gas hydrateequilibrium for pure CH4, CO2 and mixed CH4-CO2 systems insaline pore waters for any given pore size distribution. Theimportant feature of this model is that it takes intoconsideration salting out phenomena, I.e. increase in saltconcentration due to gas hydrate and ice formation. It alsogives the gas hydrate saturation in porous medium. A newEOS developed for prediction of bulk gas hydrate equilibriumconditions, based on van der Waals - Platteeuw model, is usedin the pore freezing model and can also be used to calculateheats of formation of these hydrates for a given pore size andpressure. The results obtained from the model are comparedwith experimental results.
机译:与整体系统相比,多孔介质中气体水合物的相平衡发生了变化。在多孔介质内部,由于分子与孔壁的相互作用以及保持毛细管平衡所需的能量,化学成分的热力学势会发生变化。建立了一个孔冻结模型,该模型可用于预测在任何给定的孔径分布下,盐水池中的纯CH4,CO2和混合CH4-CO2系统的气体水合物平衡。该模型的重要特征是考虑了盐析现象,即由于气体水合物和冰的形成而使盐浓度增加。它还使多孔介质中的天然气水合物饱和。基于范德华斯-Platteeuw模型开发的用于预测散装天然气水合物平衡条件的newEOS用于孔冻结模型,还可以用于在给定的孔径和压力下计算这些水合物的形成热。从模型获得的结果与实验结果进行比较。

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