Evidence map›Paper›PMID 38710758›Full record

ArticleScientific reports2024

Experimental study on I/II/III mixed mode fracture characteristics of a combined rock mass under creep loading.

Shuai Li, Chao Zheng, Peng Li, Shuo Zhang

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Article in Scientific reports, 2024. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Not yet cited in PubMed.

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4 · The record

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5 · Who and what money

Authors and funding

4 authors.

Shuai LiSchool of Civil and Transportation Engineering, Henan University of Urban Construction, Pingdingshan, People's Republic of China. li-82.28@163.com.
Chao ZhengSchool of Civil and Transportation Engineering, Henan University of Urban Construction, Pingdingshan, People's Republic of China. zhengchao@huuc.edu.cn.
Peng LiSchool of Civil and Transportation Engineering, Henan University of Urban Construction, Pingdingshan, People's Republic of China.
Shuo ZhangSchool of Civil and Transportation Engineering, Henan University of Urban Construction, Pingdingshan, People's Republic of China.

Funding

the Key Scientific Research Projects of Colleges and Universities in Henan Province No. 23A560019the Science and Technology Research Projects of Henan Province No. 232102320017the Science and Technology Research Projects of Henan Province (No. 232102320241), 2023 Academic Technology Leaders (No. YCJXSJSDTR202302), and 2022 School-Level Young Backbone Teachers (No. YCJQNGGJS202201) No. 232102320241;(No. YCJXSJSDTR202302;No. YCJQNGGJS202201
6 · The paper itself

Abstract

I/II/III mixed mode fractures of intersecting joint fissures often occur in natural rock masses, and jointed rock masses are prone to rockbursts in deep underground engineering when subjected to long-term crustal stresses. However, most studies of the mechanical mechanisms of these intersected joints have been conducted by simplifying two-dimensional joint model tests. Furthermore, the fracture mechanisms of two-dimensional intersected joints under tension and compression are completely different from those of three-dimensional joints. This paper presents a novel prefabricated specimen with combinations of intersecting joints capable of detecting the failure behaviours of rock I/II/III mixed mode fractures under creep loading. Uniaxial compression and multistage creep tests are performed on prefabricated sandstone specimens with intersecting joints of 0°/0°, 0°/30°, 0°/60°, and 0°/90°. The experimental results show that with the increase in the number of prefabricated intersecting joints, the uniaxial compressive strength and elastic modulus values of the sandstone specimens gradually decrease. In addition, the sandstone specimens experience relatively few AE events and minor axial strain variations in the first creep stage and the second creep stage of the multistage creep test. The axial strain increases sharply due to the sharp increase in the number of AE events in the third creep stage. The 0°/60° sandstone specimen undergoes accelerated creep failure, resulting in mixed X-shaped tensile‒shear rupture. The RA value is high based on the quantification of the creeping cracks using the acoustic emission parameters of the rise angle (RA) and average frequency (AF). The AF values of the 0°/0°, 0°/30°, and 0°/90° sandstone specimens are high. The experimental results show that a larger joint intersection angle leads to greater mutual restraints and greater effects of prefabricated crack propagation in the rock specimens, thus increasing the final failure strength. Finally, based on the acoustic emission count, a characteristic variable D suitable for characterizing the creep damage evolution of a joint rock mass is established. The findings of this paper can facilitate an effective understanding of the creep effect of I/II/III mixed mode fracture and its micromechanism. The research results will have a certain reference value for the detection and risk mitigation of instantaneous and time-delayed rockbursts.

Indexed as

Acoustic emission (AE)Creep experimentFracture patternSandstoneTwo sets of persistent joints

Identifiers

PMID38710758
PMCPMC11639735

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