咸水层CO2埋存动态溶解特性及主控因素研究
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赵嘉(1998—),女,山东诸城人,在读博士研究生,从事油气田开发工程研究工作。E-mail:vickizj_upc@163.com。

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ynamic dissolution characteristics and main controlling factors of CO2 storage in saline aquifers
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    溶解埋存是咸水层CO2埋存的关键机制,而现有研究多基于静态平衡假设,缺乏对储层条件下CO2动态溶解特性的系统认识。实验结合 CO2动态溶解实验与响应面法,采用 Double Boltzmann函数表征了非平衡溶解机制,并基于中心复合设计构建了注入速率、流动单元指数和矿化度对CO2溶解量的二次多项回归模型,旨在揭示CO2动态溶解特性及主控因素。实验表明,CO2动态溶解进程可概括为气体快速排驱、不稳定溶解滞后、溶解传质主控及扩散溶解平衡4个阶段,非平衡溶解指数曲线表明CO2动态溶解量达到平衡溶解度的91%,定量分析揭示了从对流传质主导(衰减因子为3.335,贡献67.7%的溶解量)到扩散传质主导(衰减因子为0.967,贡献32.3%的溶解量)的双阶段溶解机制。响应面分析结果表明,各因素对溶解量的影响程度由强到弱依次为:矿化度、流动单元指数、注入速率,其中矿化度为3 750 mg/L、流动单元指数为7.5、注入速率为0.5 mL/min的组合为最优溶解条件。在实施埋存工程项目时,应优先选择低矿化度(<5 000 mg/L)、中等渗透率(50×10-3~150×10-3 μm2)和适中孔隙度(15%~20%)的储层进行CO2埋存,基于溶解过程的阶段特性应采用分阶段注入策略,初期应采用0.2~0.5 mL/min的低速注入,防止CO2以连续相快速突破,增加气液接触时间;中期可采用脉冲式注入模式,即间歇性调整注入速率以促进CO2与新鲜咸水接触,避免局部矿化度升高导致的溶解效率下降。

    Abstract:

    Dissolution trapping is a critical mechanism for CO2 storage in saline aquifers. However, existing research predominantly relies on static equilibrium assumptions, lacking a systematic understanding of dynamic CO2 dissolution characteristics under reservoir conditions. This study combined dynamic CO2 dissolution experiments with response surface methodology,employing the Double Boltzmann function to characterize the non-equilibrium dissolution mechanism. Using central composite design,we constructed a quadratic polynomial regression model examining the effects of injection rate,flow unit index,and salinity on CO2 dissolution,aiming to reveal the dynamic CO2 dissolution characteristics and main controlling factors. Results demonstrate that the dynamic CO2 dissolution process can be categorized into four stages:rapid gas displacement,unstable dissolution lag,dissolution mass-transfer dominance,and diffusive dissolution equilibrium. Non-equilibrium dissolution index curves indicate that dynamic CO2 dissolution reaches 91% of equilibrium solubility. Quantitative analysis reveals a dual-stage dissolution mechanism transitioning from convection-dominated(decay factor of 3.335,contributing 67.7% of dissolution)to diffusion-dominated(decay factor of 0.967,contributing 32.3% of dissolution)processes. Response surface analysis results show that the influence of factors on solubility in descending order is as follows:salinity,flow unit index,and injection rate,with the optimal dissolution conditions being salinity of 3 750 mg/L,flow unit index of 7.5,and injection rate of 0.5 mL/min. For implementing storage engineering projects,priority should be given to reservoirs with low salinity(<5 000 mg/L),moderate permeability(50×10-3-150×10-3 μm2),and moderate porosity(15%-20%). Based on the stage characteristics of the dissolution process,a phased injection strategy should be adopted. Initially,low injection rates of 0.2-0.5 mL/min should be employed to prevent rapid breakthrough of CO2 as a continuous phase and increase gas-liquid contact time. In the intermediate stage,a pulsed injection mode can be adopted,periodically adjusting injection rates to promote contact between CO2 and fresh brine,avoiding decreased dissolution efficiency caused by localized increases in salt concentration

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赵 嘉,姚传进,宋雨媛,周依然,张秀晴.咸水层CO2埋存动态溶解特性及主控因素研究[J].油气地质与采收率,2025,32(6):108~117

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  • 收稿日期:2025-04-11
  • 最后修改日期:2025-10-27
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  • 在线发布日期: 2025-12-18
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