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Role of capillary forces in vapour extraction from low-permeability, water-saturated geothermal reservoirs

机译:毛细作用力在低渗透水饱和地热油藏中抽汽的作用

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摘要

The aim of this work is to formulate a mathematical model of water vaporization at a moving front in porous media, taking into account capillary forces. The complete system of boundary conditions at the boiling front is presented. A similarity analytical solution is then derived for the one-dimensional non-linear problem of mass extraction from a contact boundary between a hydrothermal reservoir and impermeable rocks. In this case the problem leads to a system of transcendental equations that is solved numerically. The model provides qualitative and quantitative information on the influence of capillary forces on the water vaporization process in geothermal reservoirs. It is shown that two different regimes of water vaporization exist: (1) with formation of a two-phase transition zone and (2) with formation of a sharp vaporization front. An increase in capillary forces in water wettable media leads to the extension of the domain of the frontal regime and to an intensification of the vaporization process; vice versa in non-wettable media.
机译:这项工作的目的是在考虑毛细作用力的情况下,在多孔介质的运动前沿建立水汽化的数学模型。介绍了沸腾前沿的边界条件的完整系统。然后从水热储层和不可渗透岩石之间的接触边界中提取质量的一维非线性问题的相似性解析解。在这种情况下,问题导致了先验方程组被数值求解。该模型提供了有关毛细作用力对地热储层中水汽化过程影响的定性和定量信息。结果表明,存在两种不同的水汽化形式:(1)形成两相过渡区;(2)形成尖锐的汽化前沿。水可湿性介质中毛细作用力的增加导致额叶范围的扩展和汽化过程的增强。反之亦然。

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