基于孔隙尺度多物理场耦合模型的高温高压储层流动与传热模拟

Hongwei Chen, Zheng Sun, Yang Li, Haoyu Su
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摘要

利用不规则孔隙尺度模型研究具有高温、高压和高应力特征的重油储层是有效的。以往的研究通常侧重于规则模型和常规环境油藏,对极端环境下的不规则模型和油藏的探索有限。在研究孔隙尺度高温、高压、高应力条件下油藏内水置换重油的过程时,利用四参数法创建了一个微尺度不规则多孔介质模型。该模型系统地考虑了岩石和重油的物理性质随温度的变化。结果表明,适当提高注水率或减小储层接触角将提高采收率、温度和储层应力。在位移时间为 0.3 s 时,注水速度从 0.004 m ∙ s-1 增加到 0.01 m ∙ s-1,油藏的采收率增加了 0.091。同时,储层的平均温度和平均应力分别增加了 29.66 K 和 1.9464 × 109 N - m-2。当位移时间为 0.3 s,接触角从 2π/3 减小到 π/3 时,储层的恢复度增加了 0.44537,储层的平均温度和平均应力分别增加了 2.87 K 和 1.86 × 108 N - m-2。
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Simulation of flow and heat transfer in high‐temperature and high‐pressure reservoir based on multi‐physical field coupling model at pore scale
The use of irregular pore‐scale models to study heavy oil reservoirs with high‐temperature, high‐pressure, and high‐stress characteristics is effective. Previous studies have typically focused on regular models and conventional environmental reservoirs, with limited exploration of irregular models and reservoirs in extreme environments. In investigating the process of water displacing heavy oil within reservoirs under high‐temperature, high‐pressure, and high‐stress conditions at the pore scale, the utilization of the four‐parameter method creates a micro‐scale irregular porous media model. The model systematically considers the variation of physical properties of rocks and heavy oil with temperature. The results indicate that an appropriate increase in water injection rate or a decrease in reservoir contact angle will increase the recovery rate, temperature, and stress of the reservoir. At a displacement time of 0.3 s, with the water injection rate increasing from 0.004 to 0.01 m ∙ s−1, the reservoir's recovery degree experiences an increase of 0.091. Simultaneously, the average temperature and average stress of the reservoir increase by 29.66 K and 1.9464 × 109 N · m−2, respectively. At a displacement time of 0.3 s and with the contact angle decreasing from 2π/3 to π/3, the reservoir's recovery degree increases by 0.44537, and the average temperature and average stress of the reservoir increase by 2.87 K and 1.86 × 108 N · m−2, respectively.
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