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多孔介质中油气体系相平衡规律研究
引用本文:张茂林,梅海燕,李闽,孙良田,李士伦 吴清松.多孔介质中油气体系相平衡规律研究[J].西南石油大学学报(社会科学版),2017,24(6):18.
作者姓名:张茂林  梅海燕  李闽  孙良田  李士伦 吴清松
作者单位:1. 西南石油学院石油工程学院,四川南充637001 ; 2. 中国科学技术大学,安徽合肥230026
摘    要:油气体系和储层多孔介质是一个相互作用的系统,当地层压力低于饱和压力时,储层中同时存在气、液、固(指岩石) 三相。在多孔介质中,由于孔隙半径小,因而毛细管压力应予以考虑。在建立了考虑毛细管压力的相平衡计算模型之后,针对二个凝析气藏,一个黑油油藏和一个挥发油藏,分别对其油气体系的毛细管压力、饱和压力和恒组成膨胀过程中液相含量进行了相态模拟计算,并总结出毛细管压力对油气体系相平衡的影响规律。

关 键 词:多孔介质    油气藏    相平衡    毛细管压力
收稿时间:2002-02-21

THE PHASE EQUILIBRIUM OF THE OILOGAS SYSTEM IN THE POROUS MEDIA
ZHANG Ma-lin MEI Hai-yan LI Min LI Shi-lun WU Qing-song.THE PHASE EQUILIBRIUM OF THE OILOGAS SYSTEM IN THE POROUS MEDIA[J].Journal of Southwest Petroleum University(Social Sciences Edition),2017,24(6):18.
Authors:ZHANG Ma-lin MEI Hai-yan LI Min LI Shi-lun WU Qing-song
Institution:Southwest Petroleum Institute , Nanchong Sichuan 637001 , China
Abstract:The oilOgas system and the porous media are interaction system. The three phases of vapor , liquid and solid (rock) will coOexist in the porous media when the pressure is under the sat uration pressure. Since the pore radius is very tiny in the porous media , the capillary pressure should be considered. The phase equilibrium calculation model concerning capillary pressure is established in this paper. The capillary pressure , the saturation pressure , and the liquid content of the constant compositional expansion are calculated by using this model for one black oil reservoir , one volatile oil reservoir and two gas condensate reservoirs. The conclusion of the capillary pressure effect on the ilOgas system is summerized at the end of this paper.
Keywords:porous media                                                                                                                        oil and gas reservoir                                                                                                                        phase equilibrium                                                                                                                        capillary pressure
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