不同岩性气藏注CO2渗流机理

Seepage Mechanism of CO2 Injection in Different Lithological Gas Reservoirs

  • 摘要: 气藏中注入CO2提高采收率技术即CCUS-EGR有望成为支撑“双碳”目标的主体技术。针对常规气藏及致密气藏中注CO2提高采收率的机理尚不清晰的问题,设计不同温压下岩样渗流能力实验,判断不同相态下CO2渗流能力;建立微观数值模拟,对比孔隙空间中注入不同介质驱替CH4的提采效果、波及系数和驱替效率;对含束缚水状态不同岩性样品进行CO2-水-岩反应实验,结合核磁共振设备评价注入CO2前后气藏渗流能力和孔隙结构的变化。结果表明:超临界CO2的黏度接近气态、密度接近液态,具有极高的渗流能力;与N2和H2O相比,CO2扩散系数最高,CO2对孔隙角隅处CH4的微观波及系数最高、驱替效果最好,对应的CH4采收率最高;CO2-水-岩反应导致碳酸盐岩、致密砂岩和火山岩样品致密化以及束缚水含量降低,其中碳酸盐岩样品反应最强烈、反应后大孔体积占比增加,而致密砂岩和火山岩样品反应后大孔体积占比减少,最终含束缚水岩样渗透率由矿物沉淀程度以及束缚水饱和度降低程度共同决定。该研究为现场常规气藏及致密气藏注入CO2先导试验提供了理论支撑,并为实际应用提供了重要参考。

     

    Abstract: Injecting CO2 into gas reservoirs to enhance gas recovery, known as CCUS-EGR (Carbon Capture, Utilization, and Storage for Enhanced Gas Recovery) technology, is poised to become the key technology supporting the strategic goals of the "dual carbon" target. To address the unclear mechanism of CO2 injection for enhancing gas recovery in conventional and tight gas reservoirs, experiments about the permeability of rock samples under different temperatures and pressures were conducted to determine the CO2 permeability across different phase states. Micro-scale numerical simulations were employed to compare the extraction efficiency, sweep efficiency, and displacement efficiency of CH4 when injected with different media in pore spaces. Additionally, CO2-water-rock reaction experiments were performed on samples of various rock types containing bound water, with changes in permeability and pore structure of gas reservoirs before and after CO2 injection assessed using NMR (nuclear magnetic resonance) equipment. The research results reveal that supercritical CO2 exhibits viscosity similar to gas and density close to liquid, along with exceptionally high permeability. Compared to N2 and H2O, CO2 demonstrates the highest diffusion coefficient, the greatest micro-scale sweep efficiency for CH4 in pore corners, the most effective displacement performance, and consequently, the highest CH4 recovery rate. The CO2-water-rock reaction results in the densification of carbonate rocks, tight sandstones, and volcanic rock samples, accompanied by a reduction in bound water content. Among these, carbonate rock samples exhibit the most intense reaction, with an increase in macropore vo-lume proportion post-reaction, whereas tight sandstone and volcanic rock samples show a decrease in macropore volume proportion. Ultimately, the permeability of bound water-containing rock samples is governed by the extent of mineral precipitation and the reduction in bound water saturation. This study provides theoretical support for the pilot test of CO2 injection in conventional and tight gas reservoirs, offering valuable insights for field applications.

     

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