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甲烷水合物在石英砂中生成过程研究

Research of Methane Hydrate Formation Process in Quartz Sand

  • 摘要: 在初始压力Pin=13.0 MPa±0.2 MPa,过冷度Tsup=14.2 K±0.1 K条件下,研究了7种不同粒径石英砂中甲烷水合物生成诱导期、生成时间以及孔隙水“记忆效应”的影响。结果显示,石英砂中诱导期较纯水中明显缩短;石英砂粒径减小,诱导期变长。孔隙水“记忆效应”极大缩短甲烷水合物诱导期,并表现出随机性。石英砂中甲烷水合物生成时间与石英砂粒径、孔隙水“记忆效应”的关系与诱导期类似。分析认为石英砂颗粒提供更多成核中心,而孔隙减小阻碍了甲烷的扩散。

     

    Abstract: The induction time, formation time and pore water "memory effect" of methane hydrate were investigated in seven kinds of quartz sand with different particle sizes under initial pressure Pin=13.0±0.2MPa with supercooling degree Tsup=14.2±0.1K. The results show that the induction time reduces significantly than that in bulk water, and the induction time increases with the decrease of particle size. Also, the induction time is greatly reduced when subjected to pore water "memory effect" and the results are random. The influences of particle size and pore water "memory effect" on formation time of methane hydrate are similar to those on induction time. The quartz sand particles provide more nucleation cores, while methane diffusion is hindered by small pore size.

     

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