Coupled Effects of Initial Water Saturation and Water Film on Spontaneous Imbibition of Overmature Shale: Insights from Nuclear Magnetic Resonance and Water Vapor Adsorption Analysis

渗吸 饱和(图论) 油页岩 吸附 水蒸气 相对湿度 保水性 体积热力学 毛细管作用 毛细管冷凝 蒸发 材料科学 化学 水力压裂 矿物学 相对渗透率 磁导率 多孔介质 湿度 水分 含水量 多孔性 润湿 含水饱和度 束缚水 分析化学(期刊) 地质学 脱水 毛细管压力
作者
Yanming Zhao,Ping Gao,Peng Cheng,Yijie Xing,Wei Liu,Guangming Meng,Jinku Li,Yineng Tan,Xianming Xiao
出处
期刊:Spe Journal [Society of Petroleum Engineers]
卷期号:: 1-21
标识
DOI:10.2118/236588-pa
摘要

Summary Fracturing fluid retention and the resulting water blocking, both major challenges in shale gas production using hydraulic fracturing methods, are significantly governed by the initial water saturation (Swi) because it controls spontaneous imbibition (SI) behavior. However, this issue remains poorly understood, especially in overmature shales. In this study, we prepared Lower Cambrian overmature shale into three shale samples with different Swi using saturated saline solutions. The water adsorption behavior and flow process of a Lower Cambrian overmature shale was investigated, respectively, using water vapor adsorption (WVA) experiments and the SI experiments under the monitoring of nuclear magnetic resonance (NMR). The results show that the SI proceeds through the rapid SI stage, transition stage, and balanced stage. A higher Swi corresponds to a weaker capillary force, with lower imbibition volume and rate. Initial water primarily resides in small pores and gradually adsorbs on larger pores to form water films as Swi increases. These thin water films are prone to be interpreted by NMR as small pores to overestimate the volume of smaller pores. During the SI process, the water film effect gradually disappears, and the true pore size is reflected. The water film effect develops obviously within a relative humidity (RH) range of 0.59–0.75, and the T2 ranges of strong water film and weak water film effects are 0.2–0.52 ms and 1.86–5.8 ms, respectively. The critical water saturation of the shale sample for effective self-sealing ranges from 31.59% to 45.94% (corresponding to an RH value of 0.59), with a sharp decrease in gas permeability. Moreover, the gas flow becomes almost blocked at water saturation of 60.17– 64.85% (corresponding to an RH value of 0.75), with the gas permeability loss rate exceeding 95%. Therefore, the low Swi layers represent preferable sweet spots for shale gas development.
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