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Articles

Experimental study on creep deformation and long-term strength of unloading-fractured marble

, , , &
Pages s97-s107 | Received 08 Sep 2014, Accepted 19 Jun 2015, Published online: 25 Sep 2015
 

Abstract

In order to take account of the unloading fractures in rocks due to the excavation, unloading-fractured marble specimens were obtained by the triaxial unloading tests. Then, creep tests on the unloading-fractured marble specimens under different stress levels and confining pressures were performed. Based on the creep tests, the creep deformation characteristics were studied and the results show that the creep curves exhibit the three stages of the idealised creep curve. Special attentions were paid on that the creep deformation and creep rate in lateral direction are far greater than that in axial direction and the lateral creep reaches the accelerated stage earlier than the axial creep. There are stress thresholds correspond to the inflection point of stress–strain relationship in lateral and axial directions, respectively, and the lateral threshold is less than the axial one. The creep failure is mainly caused by the strong expansion in lateral direction. Moreover, both the creep rate and deformation have positive relationships with the axial stress but decrease as confining pressure increases. The failure strain increases with increasing confining pressure. Then, the long-term strengths determined by the axial and lateral isochronous stress–strain curves, respectively, are discussed. Through the comparative analysis, the lateral creep reflects the creep characteristics of unloading-fractured marble more clearly and the long-term strength determined by the lateral isochronous stress–strain curves is safer for engineering applications.

Acknowledgement

The authors wish to offer their gratitude and regards to the colleagues who contributed to this work. The authors also wish to thank the editors and anonymous reviewers for providing critical comments and constructive suggestions in revising this article.

Disclosure statement

No potential conflict of interest was reported by the authors.

Additional information

Funding

The authors are grateful for the financial support from the National Natural Science Foundation of China [grant numbers 51120145001, 51374148], the National Basic Research Projects of China [grant number 2011CB201201], the CERS-China Equipment and Education Resources System [grant number CERS-1-114], and the Fundamental Research Funds for the Central Universities [grant number 2014SCU04A07]. Science and technology project of Sichuan Province [grant number 2015JY0111].

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