页岩有机质孔隙内纯组分烷烃相态研究

Study on phase behavior of pure alkanes in shale organic nanopores

  • 摘要: 页岩广泛分布的纳米级孔隙使得烷烃相态与常规储层存在差异,且不同矿物表面性质差异会对流体相态产生不同的影响。采用蒙特卡洛分子模拟方法对干酪根和方解石孔隙内纯组分烷烃气液相平衡进行模拟,计算得到相平衡参数和临界参数,通过密度分布分析微尺度效应对气液相平衡和临界参数的影响机制。研究表明:页岩有机质孔隙内流体受吸附和毛细凝聚的影响,气液相平衡时气相密度偏高而液相密度偏低。受平衡相影响,纳米孔隙内烷烃临界温度和临界压力低于体相值。随孔径增大,气液相平衡属性值和临界参数逐渐接近体相值。本文阐明了页岩有机质孔隙内烷烃相态变化规律并进行了临界参数定量表征,为页岩有机孔内相态准确计算提供支撑。

     

    Abstract: The widespread distribution of nanoscale pores in shale makes the phase behavior of alkenes different from that of conventional reservoirs. The differences in surface properties of different minerals will have different effects on fluid phase behavior. Monte Carlo molecular simulation method was used to simulate the gas-liquid phase equilibrium of pure alkanes in the pores of kerogen and calcite. The phase equilibrium parameters and critical parameters were calculated. The mechanism of micro-scale effects on the gas-liquid phase equilibrium and critical parameters was analyzed by density distribution. The phase behavior of the fluid in the shale reservoir is affected by adsorption and capillary condensation, which leads to a higher gas-phase density and a lower liquid-phase density. Under the influence of equilibrium phase, the critical temperature and pressure of alkanes in nanopores are lower than those in bulk phase. With the increase of pore size, the properties and critical parameters of vapor-liquid equilibrium gradually approach the bulk value. The change law of phase behavior of alkanes in shale organic pores is expounded and the critical parameters are quantitatively characterized, which provides support for accurate calculation of phase state in shale organic pores.

     

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