Mechanical and energetic properties of rock-like specimens under water-stress coupling environment

被引:2
作者
Cheng, Xiaoyang [1 ,2 ,3 ]
Sun, Haitao [2 ,3 ,4 ]
Pu, Yang [2 ,3 ]
Guo, Junjie [5 ]
Qiao, Wei [2 ,3 ]
机构
[1] China Coal Res Inst, Beijing 100013, Peoples R China
[2] Chongqing Res Inst, China Coal Technol & Engn Grp, Chongqing 400037, Peoples R China
[3] State Key Lab Coal Mine Disaster Prevent & Control, Chongqing 400037, Peoples R China
[4] Chongqing Univ, Sch Resources & Safety Engn, Chongqing 400044, Peoples R China
[5] Henan Univ Engn, Sch Resources & Safety Engn, Zhengzhou 451191, Henan, Peoples R China
基金
中国国家自然科学基金;
关键词
Water-stress coupling; Rock-like specimens; Mechanical properties; Energy properties; DAMAGE CONSTITUTIVE MODEL; 2-SCALE GEOMECHANICS;
D O I
10.1007/s13202-024-01766-y
中图分类号
TE [石油、天然气工业]; TK [能源与动力工程];
学科分类号
0807 ; 0820 ;
摘要
Soft rock has the properties of low strength, poor integrity, and difficulty in core extraction. In order to study the deformation and failure of soft rock, this study used fine river sand as aggregate, cement and gypsum as bonding materials, and borax as a retarder to produce cylindrical rock-like samples (RLS) with a sand cement ratio of 1:1. Uniaxial compression tests were conducted on RLS under DIT (different immersion times) (0, 4, 8, 12, 24, and 48 h) in the laboratory. The mechanical and energy properties of RLS under water-stress coupling were analyzed. The results showed that the longer the IT of the RLS, the higher their water content (WC). As the moisture time increases, the uniaxial compressive strength, elastic modulus (EM), and softening coefficient (SC) of the sample gradually decrease, while the rate of change of EM is the opposite. The fitted sample SC exhibits a good logarithmic function relationship with WC. During the loading process of the sample, more than 60% of the U (total energy absorbed) during the loading process of the sample is accumulated in the form of U-e (releasable elastic energy), while less than 40% of U is dissipated by the newly formed micro cracks during the compaction, sliding, and yield stages of the internal pores and cracks of the sample. The U before the peak and the U-e of the RLS decrease exponentially with the moisture content; the relationship curves of U-e/U (released elastic energy ratio) and U-d/U (dissipated energy ratio) of RLS during uniaxial compression with the sigma(1)/sigma(max) (axial stress ratio) can be divided into three stages of change, namely the stage of primary fissure compaction and closure (sigma(1)/sigma(max) < 0.25), continuously absorbing energy stage (0.25 < sigma(1)/sigma(max) < 0.8), and energy dissipation stage (sigma(1)/sigma(max) > 0.8); the D (damage variable) was defined by the ratio of U-d (dissipated energy) to the U-dmax (maximum dissipated energy) at failure time of RLS, the fitting of the relationship between the damage variable and axial strain conforms to the logistic equation.
引用
收藏
页码:1113 / 1128
页数:16
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