Technical Papers
Apr 26, 2017

Numerical Investigation of Damage Evolution and Localized Fracturing of Brittle Rock in Compression

Publication: Journal of Performance of Constructed Facilities
Volume 31, Issue 5

Abstract

In the present paper, a numerical model for deformation and fracturing of brittle rocks is used to study the damage evolution and localized fracturing of brittle rocks based on statistical mesoscopic damage mechanics. In the model, material heterogeneity and the mesoscopic renormalization concept are introduced to consider the interaction among microcracks in rock. The temporal and spatial evolution of acoustic emissions in the stressed rock are also described. Correspondingly, numerical tests on rock specimens with different heterogeneities, porosities, and scales are performed to investigate the damage evolution and localized fracturing of brittle rocks. The localized damage and fracturing of brittle rocks induced by microstructural damage is investigated. The study shows that heterogeneity, porosities, and scales of rock specimen have significant impact on damage evolution and localized fracturing mode. In addition, the study reveals that the postpeak response of stress-strain curve is due to the deformation of the structural elements, and localization means that the descending branch of the stress-strain curve of the rock specimen is size dependent, and the stress-strain curve can therefore not be regarded as a pure material property.

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Acknowledgments

The joint support provided by NSFC (Grant Nos. 51474051, 41672301, and 51404067) and the National Basic Research Program of China (2013CB227900 and 2014CB047100), Fundamental Research Funds for the Central Universities (N150102002 and L1501004), and Partenariats Hubert Curien (PHC) grant—Programme Cai Yuanpei (Grant No. 36605ZB) is highly acknowledged.

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Go to Journal of Performance of Constructed Facilities
Journal of Performance of Constructed Facilities
Volume 31Issue 5October 2017

History

Received: Mar 21, 2016
Accepted: Feb 6, 2017
Published online: Apr 26, 2017
Discussion open until: Sep 26, 2017
Published in print: Oct 1, 2017

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Professor, Center for Rock Instability and Seismicity Research, Northeastern Univ., Shenyang 110819, China (corresponding author). E-mail: [email protected]
Shengqi Yang [email protected]
Professor, State Key Laboratory for Geomechanics and Deep Underground Engineering, School of Mechanics and Civil Engineering, China Univ. of Mining and Technology, Xuzhou 221116, China. E-mail: [email protected]
Chongfeng Chen [email protected]
Ph.D. Student, Center for Rock Instability and Seismicity Research, Northeastern Univ., Shenyang 110819, China. E-mail: [email protected]
Tianhong Yang [email protected]
Professor, Center for Rock Instability and Seismicity Research, Northeastern Univ., Shenyang 110819, China. E-mail: [email protected]
Penghai Zhang [email protected]
Postdoctoral, Center for Rock Instability and Seismicity Research, Northeastern Univ., Shenyang 110819, China. E-mail: [email protected]
Honglei Liu [email protected]
Lecturer, School of Resources and Civil Engineering, Northeastern Univ., Shenyang 110819, China. E-mail: [email protected]

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