特种油气藏 ›› 2026, Vol. 33 ›› Issue (1): 75-83.DOI: 10.3969/j.issn.1006-6535.2026.01.009

• 油藏工程 • 上一篇    下一篇

CO2压力对羟基化和甲基化石英动态润湿影响的分子动力学研究

闫志明, 王凤娇, 刘义坤, 初明旋, 任梦瑶   

  1. 东北石油大学提高油气采收率教育部重点实验室,黑龙江 大庆 163318
  • 收稿日期:2024-10-29 修回日期:2025-10-26 出版日期:2026-02-25 发布日期:2026-06-22
  • 通讯作者: 刘义坤(1963—),男,教授,博士生导师,1984年毕业于大庆石油学院油气田开发工程专业,1999年毕业于该校油气田开发工程专业,获博士学位,现从事油气渗流机理及提高采收率等方面的研究工作。
  • 作者简介:闫志明(1994—),男,2019年毕业于东北石油大学石油工程专业,现为该校石油与天然气工程专业在读博士研究生,主要从事非常规油气渗流机理方面的研究。
  • 基金资助:
    国家自然科学基金“压裂-渗流-驱油方法多场耦合渗流机理研究”(52074087)、“振击压驱方法孔隙流体瞬时聚能微观力学机制及渗流机理研究”(52374035)

Molecular dynamics study of CO2 pressure effects on dynamic wettability of hydroxylated and methylated quartz

YAN Zhiming, WANG Fengjiao, LIU Yikun, CHU Mingxuan, REN Mengyao   

  1. Key Laboratory of Improving Oil and Gas Recovery, Ministry of Education, Northeast Petroleum University, Daqing, Heilongjiang 163318, China
  • Received:2024-10-29 Revised:2025-10-26 Online:2026-02-25 Published:2026-06-22

摘要: 为了明确非常规储层注CO2开发时石英壁面的润湿性动态变化,采用分子动力学模拟方法,计算不同CO2压力条件下水滴润湿羟基石英和甲基石英壁面的过程。研究表明:羟基石英初始强亲水,甲基石英初始弱亲CO2,随着CO2压力增大,亲水性降低,且羟基石英润湿性变化较小,甲基石英润湿性变化较大;随着CO2压力增大,CO2分子和水分子共同吸附在甲基石英壁面,形成不连续的CO2吸附膜,降低非键相互作用,导致亲水性降低,直至CO2压力达到44.96 MPa,接触角达到180.00°;随着CO2压力增大,接触线区域水分子数量降低,运动空间被压缩,壁面对水分子的束缚作用降低,导致水分子的跳跃频率降低,跳跃距离增大;与甲基石英相比,羟基石英的亲水性更强,水分子的跳跃频率更大,跳跃距离更小。该研究揭示了不同CO2压力下羟基石英和甲基石英的接触角动态变化机制,建立了接触角与渗流速度、CO2压力的关系,提出更加精确的毛管力描述。研究成果不仅为纳米限域流体流动提供了新的理论支持,还为储层评估、产能预测及开发策略制订提供了更为可靠的依据。

关键词: 分子动力学, CO2, 羟基石英, 甲基石英, 动态润湿

Abstract: To clarify the dynamic wettability changes during CO2 injection in unconventional reservoirs,molecular dynamics simulations were performed of water droplets wetting hydroxylated quartz and methylated quartz surfaces at various CO2 pressures.The study shows that hydroxylated quartz is initially strongly hydrophilic,while methylated quartz is initially weakly CO2-affine;as CO2 pressure increased,the water wettability of both decreased,with smaller changes for hydroxylated quartz and larger changes for methylated quartz.With higher CO2 pressure,CO2 and water molecules co-adsorbed on the methylated quartz surface,forming a discontinuous CO2 adsorption film that reduced non-bonded interactions and led to lower hydrophilicity until at 44.96 MPa the water contact angle reaches to 180.00°.As CO2 pressure increases,the number of water molecules in the contact line region decreased and their motion space is compressed,reducing water molecular jump frequency and increasing jump distance.Compared with methylated quartz,hydroxylated quartz remains more hydrophilic with higher water molecule jump frequency and shorter jump distance.This study revealed the dynamic mechanisms of contact angle change for hydroxylated vs. methylated quartz under varying CO2 pressures,established relationships between contact angle,relative permeability and CO2 pressure and then a more accurate description of capillary pressure is proposed.These results provide new theoretical support for nanoscale fluid flow and a more reliable basis for reservoir evaluation,productivity prediction, and development strategy.

Key words: molecular dynamics, CO2, hydroxylated quartz, methylated quartz, dynamic wettability

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