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Gas Hydrate Formation in a Variable Volume Bed of Silica Sand Particles

机译:可变体积硅砂颗粒中气体水合物的形成

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Gas hydrate formation was studied in a new apparatus designed to accommodate three different size volume beds of silica sand particles. The sand particles have an average diameter equal to 329μm. The hydrate was formed in the water, which occupied the interstitial space of the water-saturated silica sand bed. A bulk gas phase was present above the bed (gas cap). Gas uptake measurements were carried out during experiments at constant temperature. More than 74.0% of water conversion to hydrate was achieved in all experiments conducted with methane at 4.0 and 1.0 ℃. An initial slow growth was followed by a rapid hydrate growth rate of equal magnitude for nearly all experiments until 43-53% of water was converted to hydrate. During the third and Final growth stage, the final conversions were between 74 and 98% and the conversion dynamics changed. Independent verification of hydrate formation in the sand was achieved via Raman spectroscopy and morphology observations in experiments using the same sand/water system.
机译:在一种新设备中研究了天然气水合物的形成,该设备设计用于容纳三个不同体积的硅砂颗粒床。沙粒的平均直径等于329μm。水合物在水中形成,占据了水饱和硅砂床的间隙空间。床上方存在大量气相(气顶)。在恒定温度下的实验过程中进行气体吸收测量。在4.0和1.0℃下使用甲烷进行的所有实验中,水转化为水合物的转化率均超过74.0%。在最初的缓慢增长之后,几乎所有实验都遵循相同幅度的快速水合物生长速率,直到43-53%的水转化为水合物为止。在第三阶段和最终增长阶段,最终转化率在74%到98%之间,转化动态有所变化。在使用相同的砂/水系统的实验中,通过拉曼光谱和形态学观察可以独立验证砂中水合物的形成。

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