非混溶饱和两相渗流与孔隙介质耦合作用的理论研究Ⅰ-数学模型

地震地质 ›› 1999, Vol. 21 ›› Issue (3): 243-252.

非混溶饱和两相渗流与孔隙介质耦合作用的理论研究Ⅰ-数学模型

薛世峰¹, 宋惠珍²

1. 石油大学(华东), 山东东营, 257062;
2. 中国地震局地质研究所, 北京, 100029

收稿日期:1998-08-31 修回日期:1999-06-30 出版日期:1999-09-08 发布日期:2009-11-25

THE THEORY OF IMMISCIBLE SATURATED TWO PHASE FLOW IN DEFORMED POROUS MEDIA Ⅰ-A MATHEMATICAL MODEL

Xue Shifeng¹, Song Huizhen²

1. University of Petroleum (East China), Shandong, Dongying 257062;
2. Institute of Geology, China Seismological Bureau, Beijing 100029

Received:1998-08-31 Revised:1999-06-30 Online:1999-09-08 Published:2009-11-25

摘要/Abstract

摘要： 基于连续介质力学的一般理论,在黑油多相渗流理论模型的基础上,推导了非混溶饱和两相渗流与变形孔隙介质耦合作用的数学模型方程,并对流固耦合效应进行了初步的讨论。

关键词: 数学模型, 液体固体界面, 非混溶饱和两相渗流, 线性与非线性孔隙介质, 流固耦合效应

Abstract: Based on the black-oil model in multiphase fluid and the continuum mechanics theory, a theoretical modeling equation of immiscible saturated two phase seepage coupling with deformed porous media is presented. A simple discussion shows that the coupling effect between seepage and rock deformation may be obvious in some cases.

Key words: Fluid-solid interface, Mathematical model, Immiscible saturated fluid, Linear and nonlinear porous media, Coupling effect of seepage-rock deformation

薛世峰, 宋惠珍. 非混溶饱和两相渗流与孔隙介质耦合作用的理论研究Ⅰ-数学模型[J]. 地震地质, 1999, 21(3): 243-252.

Xue Shifeng, Song Huizhen. THE THEORY OF IMMISCIBLE SATURATED TWO PHASE FLOW IN DEFORMED POROUS MEDIA Ⅰ-A MATHEMATICAL MODEL[J]. SEISMOLOGY AND GEOLOGY, 1999, 21(3): 243-252.