基于 PNM 的低渗透储层地下储气库多循环气水置换机理研究

Energy Storage Pub Date : 2024-05-21 DOI:10.1002/est2.643
Rui Song, Shuaida Wang, Guihong Pei, Jianjun Liu
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引用次数: 0

摘要

深入了解低渗透储层气水系统孔隙尺度多循环两相渗流机理,对于提高油气采收率和优化地下储气库运行条件至关重要。利用中国大港油田低渗透岩心样品的显微 CT 图像重建了孔隙网络模型。在考虑气体可压缩性和滑移效应的基础上,基于普瓦塞耶定律和准静态位移理论,建立了孔隙尺度模型中气水流动的数学模型。利用孔隙网络模拟计算了油水和气水的孔隙度、孔径、绝对渗透率和相对渗透率(Kr),并与相同样品的实验基准数据进行了验证。模拟并分析了多循环位移、岩石润湿性和平均孔隙压力对气水两相流的影响。结果表明,在考虑气体压缩性和滑移效应的情况下,相同含水饱和度下的气体相对渗透率(Krg)显著增加。随着气水置换循环次数的增加,同一饱和水位下的 Krg 呈下降趋势,表明气体渗流能力下降。Krg 随水接触角的增大而减小。随着平均孔隙压力的增加,Krg 下降,当平均压力超过 25 兆帕时,Krg 逐渐增加。
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Study on multi-cycle gas-water displacing mechanism in underground gas storage of low-permeability reservoir based on PNM

A deep understanding of the pore-scale multi-cycle two-phase seepage mechanism of gas-water systems in low-permeability reservoirs is crucial for enhancing oil and gas recovery and optimizing the operating conditions of underground gas storage. A pore network model was reconstructed using micro-CT images of low-permeability core samples from the Dagang Oilfield, China. The mathematical models of gas-water flow in the pore-scale models were established based on Poiseuille's law and the quasi-static displacement theory, considering the gas compressibility and slip effects. The porosity, pore size, absolute permeability, and relative permeability (Kr) of oil-water and gas-water were calculated using pore network simulations and validated against experimental benchmark data of the same samples. The effects of multi-cycle displacement, rock wettability, and average pore pressure on the gas-water two-phase flow were simulated and analyzed. The results showed that the relative permeability of gas (Krg) at the same water saturation level significantly increased when the gas compressibility and slip effects were considered. With an increase in the number of gas-water displacement cycles, Krg at the same water saturation level showed a decreasing trend, indicating a reduction in the gas seepage capability. Krg decreased with increasing water contact angle. With an increase in the average pore pressure, Krg decreased and gradually increased when the average pressure exceeded 25 MPa.

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