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    非均质多孔介质中CO2非混相驱替层间分流特征研究

    Interlayer Diversion Characteristics of CO2 Immiscible Displacement in Heterogeneous Porous Media

    • 摘要: 强非均质多孔介质中,高、低渗区域流动能力差异显著,CO2易沿高渗区域优先运移,造成低渗区域动用不足及层间波及失衡。为揭示不同渗透区域的动态分流规律,构建双渗透率并联多孔介质模型,采用相场法研究毛细管数和润湿性对分层采出、波及效率、动态分流及CO2突破行为的影响。结果表明:低毛细管数(Ca)下,CO2优先沿高渗区域运移,低渗层波及效率仅为5.6%~5.8%;Ca增至10−4时,低渗层波及效率提高至39.8%~45.0%,相对波及指数由0.071~0.085增至0.574~0.585,层间波及差异显著减小。Ca为10−6~10−5时,界面推进、停滞及优势路径切换持续改变两层瞬时流动阻力,引起净流量分流比显著波动;Ca增至10−4后,分流波动明显减弱,高渗层净流量分流比稳定在0.85~0.90。润湿性主要通过改变局部界面运移和剩余油赋存形态影响驱替过程,其作用随毛细—黏滞竞争状态发生变化。Ca为10−6时,接触角由105°增至150°,突破烃类孔隙体积(Hydrocarbon Pore Volume,HCPV)由0.346降至0.311;Ca为10−4时则由0.403增至0.461。低Ca下油湿性增强使CO2更易沿优势路径选择性侵入;高Ca下黏滞作用增强,大孔隙滞留油更易被重新动用,而细小孔喉中的界面约束与剩余油滞留促使突破前发生更多路径调整。研究表明,毛细管数主要控制层间分流状态及波及均衡,润湿性进一步调节局部界面行为和CO2突破特征。

       

      Abstract:
      Background Strong heterogeneity in porous media creates pronounced differences in flow capacity between high- and low-permeability regions. During immiscible CO2 displacement, this contrast promotes preferential migration through high-permeability pathways, leading to insufficient utilization of low-permeability regions and a pronounced interlayer sweep imbalance. Clarifying how flow is dynamically partitioned between layers under different capillary and wettability conditions is therefore important for understanding displacement behavior in heterogeneous porous media.
      Methods To elucidate the dynamic flow-partitioning behavior between regions with contrasting permeabilities, a parallel dual-permeability porous-medium model was established. The Navier–Stokes/Cahn–Hilliard phase-field model was employed to investigate the effects of the capillary number (Ca) and wettability on layered oil recovery, sweep efficiency, dynamic flow partitioning, and CO2 breakthrough.
      Results At low capillary numbers, CO2 preferentially migrated through the high-permeability region, and the sweep efficiency of the low-permeability layer was only 5.6%–5.8%. When Ca increased to 10−4, the sweep efficiency of the low-permeability layer increased to 39.8%–45.0%, and the relative sweep index increased from 0.071–0.085 to 0.574–0.585, indicating a marked reduction in the interlayer sweep disparity. At Ca = 10−6–10−5, interface propagation, stagnation, and preferential path switching continuously altered the instantaneous flow resistance of the two layers, causing pronounced fluctuations in the net flow partitioning ratio. When Ca increased to 10−4, these fluctuations weakened substantially, and the net flow fraction of the high-permeability layer stabilized at 0.85–0.90. Wettability mainly influenced the displacement process by modifying local interface migration and remaining-oil distribution, and its effect varied with the capillary–viscous competition regime. At Ca = 10−6, increasing the contact angle from 105° to 150° reduced the breakthrough hydrocarbon pore volume (HCPV) from 0.346 to 0.311, whereas at Ca = 10−4, it increased from 0.403 to 0.461. Under low-Ca conditions, stronger oil-wetness enhanced selective CO2 invasion along preferential pathways, favoring earlier breakthrough. Under high-Ca conditions, stronger viscous forces promoted the remobilization of trapped oil in larger pores, while interfacial constraints and remaining-oil trapping persisted in smaller pore throats, inducing additional pathway adjustments before breakthrough. These results show that the influence of wettability on breakthrough is not monotonic but depends on the prevailing balance between capillary and viscous forces.
      Conclusions The capillary number primarily controls the overall evolution of interlayer flow partitioning and sweep balance, whereas wettability further regulates local interfacial behavior and CO2 breakthrough characteristics. Increasing the capillary number promotes the participation of low-permeability regions, reduces interlayer sweep imbalance, and drives the flow-partitioning state from strongly unsteady competition toward a more stable regime. The results further demonstrate that the roles of the capillary number and wettability are distinct but coupled during immiscible displacement in heterogeneous porous media.

       

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