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基于二維孔隙網絡模型的懸浮顆粒微觀尺度滯留規律及滲流場特征

Nanomicron heterogeneous topic: Pore size suspended particle retention law and seepage field characteristics

  • 摘要: 油氣田開發是典型的多相滲流過程,在長期并持續的開發過程中,注水、氣驅、化學驅及壓裂等技術都會導致攜帶來的礦物顆粒及儲層內原有喉道的砂體顆粒逐漸松散并脫落,造成儲層孔隙中的遷移及堵塞,繼而影響儲層的動用及最終采收率. 因此,研究懸浮顆粒在多孔介質中遷移與滯留過程及流場特征有重要意義. 然而,現有針對懸浮顆粒在多孔介質中遷移與滯留的研究主要關注顆粒的遷移和滯留對滲透率的損害,沒有體現顆粒運移的過程,也不能反應孔隙網絡中顆粒堵塞和流場變化的關系. 為探究懸浮顆粒在多孔介質內的流場特征,本研究利用微觀可視化模型及微觀粒子圖像測速技術(Micro-Particle image velocimetry,簡稱為Mirco-PIV)分析了在二維孔隙網絡中懸浮顆粒的滯留特征及相互關系,并揭示了流場的變化規律. 實驗結果表明,初期主通道流速更高,但由于主通道顆粒滯留量(6.5 μg·μm?2)比邊界區更多(2.4 μg·μm?2),顆粒續注入導致主通道流速降低,擾亂原有流場導致“斑”狀流場出現,也使主通道(110 μm·s?1降低至41 μm·s?1)在中期流速低于邊界區(67 μm·s?1降低至45 μm·s?1). 這也表明高流速區更有效的輸運了顆粒. 滯留的分布特征觀察到主要滯留在了邊壁附近,較高濃度條件下還會在主通道內產生聚集現象,這些都導致了對孔隙的有效封堵. 本文首次提供了顆粒和流場互動過程,給出二維孔隙條件下可視化的直接的證據. 此外,本文還得出了顆粒分布特征,并總結出滯留靠近邊壁、流動有效半徑變窄及主通道高濃度的聚集問題,是導致封堵的核心機理,為進一步顆粒滯留理論的完善提供參考.

     

    Abstract: The development of oil and gas fields involves a typical multiphase percolation process. Over time, techniques such as injection, gas flooding, chemical flooding, and fracturing can cause mineral and sand particles in the original reservoir throat to gradually loosen and fall off. This particle loosening can adversely affect reservoir exploitation and reduce recovery efficiency. Therefore, studying the migration and flow field of suspended particles within porous media is considerable. However, current studies mainly address how particle migration and retention affect permeability and often overlook the dynamics of particle migration and their impact on flow fields within pore networks. The microscopic visualization model and microparticle image velocimetry (Mirco-PIV) technology were used to analyze particle retention and flow field changes in the main channel and boundary region of the two-dimensional porous glass model, and the laws were summarized. Results show that while initial flow velocity is higher in the main channel, particle retention in the main channel is more pronounced than that in the boundary region. Continuous particle injection reduces the flow velocity in the main channel, disturbing the original flow field and creating a “spot” flow field. Eventually, the main channel experiences a lower flow rate in the medium term than the boundary region, indicating that particles are transported more efficiently in high-flow zones. Retention mainly occurs near side walls, with high concentrations, leading to aggregation in the main channel, effectively plugging pores. Previous studies did not account for retention, aggregation, and interweaving. To our knowledge, this paper provides new insights into the interaction between particles and flow fields, offering direct visual evidence for two-dimensional conditions. As particles are injected, high flow rates transport a larger number of particles, increasing the possibility of retention and subsequently decreasing flow rates. This illustrates the interaction mechanism between particles and flow fields over time and space. Regarding flow velocity, the trends in the main channel and boundary region are inconsistent. As particles are continuously injected, the trunk road of the main channel changes, whereas the boundary region remains unaffected. In addition, particle distribution characteristics show that the core mechanism of blockage involves retention near the side wall, a reduction in the effective flow radius, and high concentration areas in the main channel. Current theories do not adequately address these issues and should be revised accordingly. The study used a combination of microscopy and micro-PIV to explore the retention and flow field of suspended particles in porous media, uncovering critical variations in these processes.

     

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