非等温多相流模型中岩石-流体混合体传热系数的确定方法

Anastasia S. Ovchinnikova, M. Persova, Daryana A. Leonovich
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引用次数: 0

摘要

本文提出了一种确定油藏中流体混合物与基质岩石之间传热速率的系数的计算方法。该系数对于油田开发过程中流体动力和热过程的进一步联合建模是必要的,例如,使用热方法来提高石油采收率。为了模拟非等温多相流的过程,采用了基于有限元法的隐式压力计算和显式相饱和度计算的方法。确定传热系数的方法是基于求解多孔介质通道及其周围部分基质岩石所对应区域的热问题。在这种情况下,已知温度值(不同于通道和基质岩石的初始温度)的流体混合物以给定的速率进入通道。用有限元法在轴对称形式下求解二维问题。在通道尺寸、孔隙度、介质初始温度、进入通道的混合物温度、流体混合物和岩石的热性质等不同值的模型上进行了数值实验,以确定传热系数。研究发现,通道尺寸和孔隙度对换热系数的影响最为显著,因为这些特性决定了基质-岩石的体积,当通道内流体混合物的温度发生变化时,基质-岩石的体积会“变热/变冷”。此外,所获得的系数值相当大,因为通道中岩石和混合物之间的热交换发生在几分钟内,这实际上相当于现场开发过程的瞬时传热,其中时间步长为几天和几个月。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Approach to the determination of the heat transfer coefficient between rock and fluid mixture for modeling non-isothermal multiphase flow
The paper presents an approach to calculation of the coefficient determining the rate of heat transfer between a fluid mixture in oil reservoir and a matrix-rock. This coefficient is necessary for further joint modeling of hydrodynamic and thermal processes that occur in the field reservoir during its development using, for example, thermal methods for enhanced oil recovery. To model the processes of a non-isothermal multiphase flow, an approach based on implicit pressure calculation using the finite element method and explicit calculation of phase saturations is used. The approach to determining the heat transfer coefficient is based on solving the thermal problem in an area corresponding to a channel of a porous medium and a part of the matrix-rock around it. In this case, a fluid mixture with a known temperature value, different from the initial temperature in the channel and matrix-rock, enters the channel at a given rate. A two-dimensional problem is solved in an axisymmetric formulation by the finite element method.Numerical experiments to determine the heat transfer coefficient were carried out on models for various values of the channel size, porosity, initial temperatures of the medium, temperature of the mixture entering the channel, thermal properties of the fluid mixture and rock. As a result of the study, it was found that the channel size and porosity have the most significant effect on the value of the heat transfer coefficient, since these characteristics determine the volume of the matrix-rock, which should “warm up / cool down” when the temperature of the fluid mixture in the channel changes. Also, the coefficient values obtained were quite large, since the heat exchange between the rock and the mixture in the channel occurs in minutes, which practically corresponds to instantaneous heat transfer when it comes to modeling field development processes, where time steps are days and months.
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