Experimental study on mechanical and permeability properties of subsea granite under cyclic loading with different seepage pressures

被引:2
作者
Qu, Xiao [1 ]
Xu, Wei [1 ,2 ]
Ma, Hongfa [1 ]
Guo, Zhenfei [3 ]
机构
[1] Shandong Univ Sci & Technol, Coll Energy & Min Engn, Qingdao 266590, Peoples R China
[2] Univ Lille, Centrale Lille, CNRS,UMR 9013, LaMcube Lab Mecan Multiphys Multiechelle, F-59000 Lille, France
[3] Shandong Dongfa Guangcheng Construct Corp Ltd, Dongying 257000, Peoples R China
基金
中国国家自然科学基金;
关键词
Different seepage pressures; Triaxial cyclic loading; Damage and energy evolution; Crack propagation permeability property; DAMAGE EVOLUTION; ROCK; SANDSTONE; BEHAVIOR; FRACTURE; FATIGUE;
D O I
10.1007/s10064-025-04094-5
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Cyclic loading and seepage pressure (Pw) have a significant impact on the mechanical properties, crack evolution, and permeability of rocks, making these factors crucial considerations in rock engineering applications. This study presents the results of triaxial monotonic and cyclic loading tests conducted on subsea granite under varying seepage pressures. The findings indicate that both cyclic loading and Pw weaken the mechanical properties of granite. As the number of cycles increases, granite undergoes greater deformation, damage, and energy dissipation. Initially, the elastic modulus (E) increases before decreasing, while Poisson's ratio (upsilon) rises. Under triaxial cyclic loading, granite's stress-strain behavior, crack development, and permeability evolve through distinct stages, including crack closure, initiation, extension, and connection. Higher Pw accelerates crack evolution and enhances permeability, leading to an earlier transition from compaction to dilation, accompanied by increased deformation, accelerated damage, greater energy dissipation, and reduced strength. At higher Pw, macro-failure characteristics include greater fragmentation and surface cracking. Scanning electron microscopy (SEM) and backscattered electron (BSE) analyses show an increase in micro-scale fracture surfaces and deeper fractures after failure, indicating intensified damage and a looser rock structure.
引用
收藏
页数:13
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