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Differential scanning calorimetry research of hydrates phase equilibrium in porous media

机译:多孔介质水合物相平衡水合物相平衡的差分扫描量热法研究

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In this paper, we focused on the determination of phase equilibrium conditions of hydrates formed in the pore water and porous media from South China Sea. High pressure differential scanning calorimetry (HP DSC), a relatively new thermo-analytical technique was applied to this research. During the study, nitrogen hydrates and methane hydrates phase equilibrium conditions were determined in the-water-hydrates-gas (W-H-G) system. Then a series of experiments were carried on using core sample drilled from South China Sea to determine the phase equilibrium properties in pore water and porous media systems. It show that the hydrates phase equilibrium point is about 2K lower than in pure water from pressure range 10 to 30 MPa, due to the thermodynamic inhibition effect of brine solution.
机译:在本文中,我们专注于从南海孔水和多孔介质中形成的水​​合物的相平衡条件的测定。高压差扫描量热法(HP DSC),对该研究应用了相对较新的热分析技术。在研究期间,在水 - 水合物 - 气体(W-H-G)系统中测定氮水合物和甲烷水合物相平衡条件。然后使用从南海钻探的核心样品进行一系列实验,以确定孔隙水和多孔介质系统中的相平衡性能。结果表明,由于盐水溶液的热力学抑制效果,水合物相平衡点大约比从压力范围为10至30MPa的纯水中低2k。

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