Generalized analytical solutions of imbibition characteristic behavior in shale matrix blocks under different boundary conditions

0 ENERGY & FUELS
Guanqun Li , Yong Yang , Xiaopeng Cao , Shiming Zhang , Qi Lv , Yuliang Su
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Abstract

Continental shale reservoirs are rich in reserves, imbibition is an essential mechanism for enhancing the oil recovery of the shale matrix system. The pores of shale matrix are divided into organic pores, brittle mineral pores and clay pores. The clay pores have the osmosis of the semi-permeable membrane, which increases the driving force of imbibition, while the non-semi-permeable membrane components are mixed-wet. Based on this, the 1-D mathematical models under different boundary conditions (including Two Ends Open, TEO; One End Open, OEO; and TEO-Oil-Water, TEO-OW) are established using the analytical solution method, and the water saturation distribution and oil recovery characteristics of matrix blocks are studied, revealing distinct imbibition phenomena: (1) Under OEO boundary conditions, counter-current imbibition dominates, with oil recovery proportional to the square root of time before the imbibition front reaches the block end. (2) For TEO boundary conditions, spontaneous imbibition exhibits symmetric counter-current flows from both ends, resulting in approximately twice the oil recovery of OEO. (3) Under TEO-OW conditions, a hybrid process of counter-current and co-current imbibition occurs, with delayed saturation evolution near the outlet. Additionally, forced imbibition under TEO demonstrates co-current flow dominated by oil-water interaction, showing earlier breakthrough with increased oil viscosity. The imbibition models of shale matrix blocks under different boundary conditions effectively reveal the control mechanism of SI and FI, and provide practical guidance for determining shut-in time and optimizing fracturing parameters.
不同边界条件下页岩基质区块渗吸特征行为的广义解析解
陆相页岩储层储量丰富,渗吸是提高页岩基质体系采收率的重要机制。页岩基质孔隙分为有机孔隙、脆性矿物孔隙和粘土孔隙。粘土孔隙具有半透膜的渗透性,增加了吸胀的驱动力,而非半透膜组分则是混湿的。在此基础上,建立了不同边界条件下的一维数学模型(包括两端开放、TEO;一端开,OEO;采用解析解法建立了基质区块的含水饱和度分布和采收率特征,研究了基质区块的含水饱和度分布和采收率特征,揭示了明显的吸胀现象:(1)在OEO边界条件下,逆流吸胀为主,采收率与吸胀前缘到达区块端前时间的平方根成正比;(2)在TEO边界条件下,自发渗吸表现为两端对称的逆流流动,使OEO的采收率提高了约2倍。(3)在正流-低流条件下,发生逆流和共流渗吸的混合过程,在出口附近的饱和演化延迟。此外,TEO条件下的强制渗吸表现为油水相互作用主导的共流,随着油粘度的增加,突破时间越早。不同边界条件下页岩基质区块的渗吸模型有效揭示了SI和FI的控制机理,为确定关井时间和优化压裂参数提供了实践指导。
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