Lyu Qiao, Ranjith Pathegama Gamage, Long Xinping, Ji Bin
Wuhan University, Wuhan 430072, China.
Key Laboratory of Hubei Province for Water Jet Theory & New Technology, Wuhan 430072, China.
Materials (Basel). 2016 Aug 6;9(8):663. doi: 10.3390/ma9080663.
The effects of CO₂-water-rock interactions on the mechanical properties of shale are essential for estimating the possibility of sequestrating CO₂ in shale reservoirs. In this study, uniaxial compressive strength (UCS) tests together with an acoustic emission (AE) system and SEM and EDS analysis were performed to investigate the mechanical properties and microstructural changes of black shales with different saturation times (10 days, 20 days and 30 days) in water dissoluted with gaseous/super-critical CO₂. According to the experimental results, the values of UCS, Young's modulus and brittleness index decrease gradually with increasing saturation time in water with gaseous/super-critical CO₂. Compared to samples without saturation, 30-day saturation causes reductions of 56.43% in UCS and 54.21% in Young's modulus for gaseous saturated samples, and 66.05% in UCS and 56.32% in Young's modulus for super-critical saturated samples, respectively. The brittleness index also decreases drastically from 84.3% for samples without saturation to 50.9% for samples saturated in water with gaseous CO₂, to 47.9% for samples saturated in water with super-critical carbon dioxide (SC-CO₂). SC-CO₂ causes a greater reduction of shale's mechanical properties. The crack propagation results obtained from the AE system show that longer saturation time produces higher peak cumulative AE energy. SEM images show that many pores occur when shale samples are saturated in water with gaseous/super-critical CO₂. The EDS results show that CO₂-water-rock interactions increase the percentages of C and Fe and decrease the percentages of Al and K on the surface of saturated samples when compared to samples without saturation.
二氧化碳 - 水 - 岩石相互作用对页岩力学性质的影响对于评估在页岩储层中封存二氧化碳的可能性至关重要。在本研究中,进行了单轴抗压强度(UCS)测试,并结合声发射(AE)系统以及扫描电子显微镜(SEM)和能谱分析(EDS),以研究黑色页岩在气态/超临界二氧化碳溶解水中不同饱和时间(10天、20天和30天)下的力学性质和微观结构变化。根据实验结果,在气态/超临界二氧化碳水中,随着饱和时间的增加,UCS值、杨氏模量和脆性指数逐渐降低。与未饱和样品相比,30天饱和导致气态饱和样品的UCS降低56.43%,杨氏模量降低54.21%;超临界饱和样品的UCS降低66.05%,杨氏模量降低56.32%。脆性指数也从未饱和样品的84.3%大幅降至气态二氧化碳水中饱和样品的50.9%,再降至超临界二氧化碳(SC - CO₂)水中饱和样品的47.9%。SC - CO₂对页岩力学性质的降低作用更大。从AE系统获得的裂纹扩展结果表明,饱和时间越长,峰值累积AE能量越高。SEM图像显示,当页岩样品在气态/超临界二氧化碳水中饱和时会出现许多孔隙。EDS结果表明,与未饱和样品相比,二氧化碳 - 水 - 岩石相互作用增加了饱和样品表面C和Fe的百分比,降低了Al和K的百分比。