The mode I fracture toughness alternation and crack propagation behavior evolution due to long-term Sc-CO2 saturation

断裂韧性 材料科学 断裂力学 复合材料 饱和(图论) 水力压裂 岩土工程 地质学 数学 组合数学
作者
Zijie Xu,Yiyu Lu,Jiren Tang,Jianfeng Xiao,Honglian Li,Yunzhong Jia,Xiayu Chen,Qi Cheng
出处
期刊:Engineering Fracture Mechanics [Elsevier]
卷期号:263: 108259-108259 被引量:12
标识
DOI:10.1016/j.engfracmech.2022.108259
摘要

The mode I fracture toughness is a critical parameter which defines the rock's resistance to crack propagation, especially in hydraulic fracturing. Recently, Supercritical carbon dioxide (Sc-CO2) has been proposed as a fracturing fluid candidate in hydraulic fracturing stimulations of shale reservoirs. However, its effects on fracture toughness transition and crack propagation behaviors have not been understood well. In this study, we performed a series of semicircular bend specimens (SCB) before the Longmaxi shale specimens' saturation. Three-point bending tests along divider orientation showed that after Sc-CO2 saturation, mode I fracture toughness (KIC), elastic modulus (E) and absorbed energy (Ue) of shale were decreased by 22.1%, 24.5% and 44.3%, respectively. High speed camera images indicated that after Sc-CO2 saturation, mode I crack directly propagated straight along artificial pre-crack direction, decreasing the degree of crack deviation as in KIC. The results of Cronos high-precision 3D scanning system and scanning electron microscopy (SEM) revealed complicated fracture mechanisms (transgranular, intergranular and mutual coupling crack mechanisms) of shale after Sc-CO2 saturation, which reduced the roughness and area of fracture crack surface. The generation of pore and cracks was the main reason for the decrease of shale resistance to fracture. Furthermore, Sc-CO2 saturated shale specimens only needed to absorb less energy to more rapidly cause the initiation and propagation of mode I cracks with the main fracture mode being transgranular cracks.

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