Crack Initiation and Coalescence Behavior of Two Non-parallel Flaws

• Published in: Geotechnical and geological engineering Vol. 36; no. 1; pp. 105 - 133
• Main Authors: Afolagboye, Lekan Olatayo, He, Jianming, Wang, Sijing
• Format: Journal Article
• Language: English
• Published: Cham Springer International Publishing 01.02.2018; Springer Nature B.V
• Subjects: Civil Engineering; Coalescence; Coalescing; Compression; Compression tests; Configurations; Crack initiation; Cracks; Earth and Environmental Science; Earth Sciences; Geotechnical Engineering & Applied Earth Sciences; Hydrogeology; Investigations; Ligaments; Original Paper; Rocks; Shear; Terrestrial Pollution; Waste Management/Waste Technology; Non-parallel flaws; Molded gypsum; Primary cracks; Crack coalescence; Crack initiation
• ISSN: 0960-3182; 1573-1529
• DOI: 10.1007/s10706-017-0310-0

Crack initiation and coalescence behavior of rock or rock-like specimens containing artificial flaws under uniaxial compression have been subjects of intensive investigation in the past. Most of these investigations however focused on crack initiation and coalescence between two or more parallel flaws. Although there have been few experimental studies on non-parallel flaws, these studies did not address the influence of geometrical factors such as ligament length and ligament angle on the crack initiation and coalescence behavior of non-parallel flaws. To investigate whether the individual geometrical factors have similar effects on the crack initiation and coalescence behavior of both parallel and non-parallel flaws, we conducted uniaxial compression tests to investigate crack cracking and coalescence processes in rock like material containing two non-parallel flaws. The paper presents the influence of individual geometrical factors on the crack initiation process and coalescence pattern of non-parallel flaws. Initiation of primary first cracks from all the tips of the two flaws did not occur simultaneously in all the flaw configurations. The flaw configuration of the non-parallel flaws influences the crack initiation, crack trajectories and coalescence behavior. The crack coalescence pattern changes with an increasing ligament angle from indirect to shear crack or mixed tensile-shear crack to tensile crack coalescence. The chance of direct coalescence is reduced with an increase in ligament length. In conclusion, the crack initiation and coalescence behavior of prismatic rock-like specimens with non-parallel flaws, as influenced by the geometrical factors, are analogous to the cracking and coalescence pattern observed in specimens with parallel flaws.