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超临界CO2在低渗透煤层中渗流规律的实验研究
引用本文:孙可明,任硕,张树翠,陈治宇,吴迪,岳立新,李赞.超临界CO2在低渗透煤层中渗流规律的实验研究[J].实验力学,2013,28(1):117-120.
作者姓名:孙可明  任硕  张树翠  陈治宇  吴迪  岳立新  李赞
作者单位:辽宁工程技术大学力学与工程学院,辽宁,123000
基金项目:国家自然科学基金(11072103、50874057)资助
摘    要:利用自主研发的THM三场耦合渗流实验系统,进行不同孔隙压力和温度条件下的超临界CO2在低渗透煤层中的渗流实验,得出不同温度下流速和压力梯度之间的关系,从而得到了低渗透煤层注入超临界CO2的非达西渗流规律,即流速与压力梯度变化规律呈现正指数关系.随着压力梯度的增大,渗透系数也不断的增大,且呈现正指数关系;在同一体积应力和压力梯度的条件下,温度越高,流速越快;温度在临界点附近,流速和渗透系数增加很快.

关 键 词:超临界CO2  低渗透煤层  渗流

Experimental Study of Supercritical Carbon Dioxide Seepage Flow in Low Permeability Coal Seam
SUN Ke-ming,REN Shuo,ZHANG Shu-cui,CHEN Zhi-yu,WU Di,YUE Li-xin and LI Zan.Experimental Study of Supercritical Carbon Dioxide Seepage Flow in Low Permeability Coal Seam[J].Journal of Experimental Mechanics,2013,28(1):117-120.
Authors:SUN Ke-ming  REN Shuo  ZHANG Shu-cui  CHEN Zhi-yu  WU Di  YUE Li-xin and LI Zan
Institution:Liaoning Technical University,Mechanics and Engineering, Liaoning 123000, China;Liaoning Technical University,Mechanics and Engineering, Liaoning 123000, China;Liaoning Technical University,Mechanics and Engineering, Liaoning 123000, China;Liaoning Technical University,Mechanics and Engineering, Liaoning 123000, China;Liaoning Technical University,Mechanics and Engineering, Liaoning 123000, China;Liaoning Technical University,Mechanics and Engineering, Liaoning 123000, China;Liaoning Technical University,Mechanics and Engineering, Liaoning 123000, China
Abstract:A series of seepage experiments of supercritical CO2 were carried out under different conditions of pore pressure and temperature based on a self-developed THM three field coupled seepage experiment system. Relationship among the flow velocity and the pressure gradient at different temperatures were obtained. That is non-Darcy seepage regulation of supercritical CO2 in low permeability seam, which means a positive exponential relation between the flow velocity and pressure gradient. The permeability coefficient increases along with the pressure gradient increase, and presents a positive exponential relationship; under the same volume stress and pressure gradient conditions, the higher the temperature is, the faster the flow velocity; when temperature approaches the critical point, the flow velocity and the permeability coefficient increase faster.
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