气驱水与水驱气流体微观分布特征研究
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汪周华(1979—),男,湖北公安人,教授,博士,从事气田与凝析气田开发、注气提高采收率技术及非常规油气开发等方面的研究工作。E-mail:wangzhouhua@126.com。

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Characterization of microscopic distribution of fluids during gas displacing water and water displacing gas
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    摘要:

    气水相渗测试是描述有水气藏储层渗流过程的常用方法,但不同测试方法和不同类型岩心的相渗测试结果均存在较大差异。为了加深对气水渗流过程中的流体微观分布特征及渗流机理的认识,以四川盆地YB气田为研究对象,利用核磁共振技术定量描述气水两相在相渗测试前后的微观分布,并结合前人利用可视化模型得到的气水两相渗流机理对分布结果进行解释。结果表明:2种测试方法相比,水驱气与气驱水过程中微米级(>1 μm)孔隙驱替程度基本一致,但水驱气过程中亚微米级(0.1~1 μm)与纳米级(<0.1 μm)孔隙驱替程度相对较高,而气驱水过程中亚微米级与纳米级孔隙内水相大部分未被动用。裂缝型与孔隙型岩心相比,裂缝型岩心微米级孔隙驱替程度相对较低,而亚微米级与纳米级孔隙驱替程度则相对较高。2种测试方法下流体微观分布的差异主要是由于孔隙内部毛管力的作用形式不同,而 2类岩心存在差异的原因是其主要渗流通道不同。

    Abstract:

    Gas-water relative permeability measurement is a common method to describe the flow process in gas reservoirs with wa‐ter. However,the results of relative permeability measurements vary significantly between different test methods and types of cores.To deepen the understanding of the microscopic distribution characteristics of fluid and flow mechanism during the gas-water flow process,this paper took YB Gas Field in Sichuan Basin as the research object and used nuclear magnetic resonance(NMR)technol‐ogy to quantitatively describe the microscopic distribution of the two phases before and after relative permeability test. The distribu‐tion results were explained based on the gas-water two-phase flow mechanism obtained by the previous researchers with the visual‐ization model. The results showed that the displacement efficiencies of micron-scale(>1 μm)pores during the water displacing gas and gas displacing water are basically the same with the two test methods,but the displacement efficiency in submicron-scale(0.1–1 μm)and nanoscale(<0.1 μm)pores during water displacing gas is relatively higher. Moreover,the water in the submicron-scale and nanoscale pores is not mainly produced during the gas displacing water. For fractured and porous cores,the displacement effi‐ciencies in micron-scale pores of fractured cores are relatively low,while the displacement efficiencies in submicron-scale and na‐noscale pores are relatively high. The difference in the microscopic distribution of fluids with the two test methods is mainly caused by the different capillary forces inside the pores,while the difference between the two types of cores is primarily due to the differ‐ence in their main flow channels.

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汪周华,张鸿宇,张 娟,廖浩奇,黄仕林.气驱水与水驱气流体微观分布特征研究[J].油气地质与采收率,2025,32(3):163~169

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  • 收稿日期:2023-10-18
  • 最后修改日期:2024-09-19
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  • 在线发布日期: 2025-04-17
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