Elastic modulus evolution of rocks under heating–cooling cycles
Rocks decay significantly during or after heating–cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse. Nevertheless, the deterioration mechanisms are unclear. This paper presents a simple and reliable method to explore the mechanical property evolutions of...
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| Published in | Scientific reports Vol. 10; no. 1; p. 13835 |
|---|---|
| Main Authors | , , |
| Format | Journal Article |
| Language | English |
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Nature Publishing Group UK
14.08.2020
Nature Publishing Group |
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| Abstract | Rocks decay significantly during or after heating–cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse. Nevertheless, the deterioration mechanisms are unclear. This paper presents a simple and reliable method to explore the mechanical property evolutions of representative sandstones during heating–cooling cycles. It was found that rock decay takes place in both heating and cooling processes, and dramatic modulus changes occurred near the
α
−
β
phase transition temperature of quartz. Our analysis also revealed that the rock decay is mainly attributed to the internal cracking. The underlying mechanism is the heterogeneous thermal deformation of mineral grains and the
α
–
β
phase transition of quartz. |
|---|---|
| AbstractList | Rocks decay significantly during or after heating–cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse. Nevertheless, the deterioration mechanisms are unclear. This paper presents a simple and reliable method to explore the mechanical property evolutions of representative sandstones during heating–cooling cycles. It was found that rock decay takes place in both heating and cooling processes, and dramatic modulus changes occurred near the α − β phase transition temperature of quartz. Our analysis also revealed that the rock decay is mainly attributed to the internal cracking. The underlying mechanism is the heterogeneous thermal deformation of mineral grains and the α – β phase transition of quartz. Rocks decay significantly during or after heating–cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse. Nevertheless, the deterioration mechanisms are unclear. This paper presents a simple and reliable method to explore the mechanical property evolutions of representative sandstones during heating–cooling cycles. It was found that rock decay takes place in both heating and cooling processes, and dramatic modulus changes occurred near the α − β phase transition temperature of quartz. Our analysis also revealed that the rock decay is mainly attributed to the internal cracking. The underlying mechanism is the heterogeneous thermal deformation of mineral grains and the α – β phase transition of quartz. Rocks decay significantly during or after heating-cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse. Nevertheless, the deterioration mechanisms are unclear. This paper presents a simple and reliable method to explore the mechanical property evolutions of representative sandstones during heating-cooling cycles. It was found that rock decay takes place in both heating and cooling processes, and dramatic modulus changes occurred near the α - β phase transition temperature of quartz. Our analysis also revealed that the rock decay is mainly attributed to the internal cracking. The underlying mechanism is the heterogeneous thermal deformation of mineral grains and the α - β phase transition of quartz.Rocks decay significantly during or after heating-cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse. Nevertheless, the deterioration mechanisms are unclear. This paper presents a simple and reliable method to explore the mechanical property evolutions of representative sandstones during heating-cooling cycles. It was found that rock decay takes place in both heating and cooling processes, and dramatic modulus changes occurred near the α - β phase transition temperature of quartz. Our analysis also revealed that the rock decay is mainly attributed to the internal cracking. The underlying mechanism is the heterogeneous thermal deformation of mineral grains and the α - β phase transition of quartz. |
| ArticleNumber | 13835 |
| Author | Liu, Weidong Luo, Ning Zhang, Liangchi |
| Author_xml | – sequence: 1 givenname: Weidong surname: Liu fullname: Liu, Weidong organization: Laboratory for Precision and Nano Processing Technologies, School of Mechanical and Manufacturing Engineering, University of New South Wales – sequence: 2 givenname: Liangchi surname: Zhang fullname: Zhang, Liangchi email: zhanglc@sustech.edu.cn organization: Department of Mechanics and Aerospace Engineering, Southern University of Science and Technology – sequence: 3 givenname: Ning surname: Luo fullname: Luo, Ning organization: Laboratory for Precision and Nano Processing Technologies, School of Mechanical and Manufacturing Engineering, University of New South Wales, State Key Laboratory for Geo-Mechanics and Deep Underground Engineering, School of Mechanics and Civil Engineering, China University of Mining and Technology |
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| CitedBy_id | crossref_primary_10_1038_s41598_022_19160_1 crossref_primary_10_1016_j_tafmec_2022_103641 crossref_primary_10_1016_j_compstruc_2021_106730 crossref_primary_10_3390_app14199122 crossref_primary_10_1038_s41598_024_71111_0 crossref_primary_10_3390_en14164773 crossref_primary_10_1016_j_lithos_2023_107097 crossref_primary_10_1038_s41598_024_68388_6 crossref_primary_10_1080_00102202_2024_2335268 |
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| Snippet | Rocks decay significantly during or after heating–cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse.... Rocks decay significantly during or after heating-cooling cycles, which can in turn lead to hazards such as landslide and stone building collapse.... |
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| SubjectTerms | 639/166/988 639/301/1023/303 Cooling Decay Heating Humanities and Social Sciences Landslides Mechanical properties multidisciplinary Phase transitions Quartz Rocks Science Science (multidisciplinary) Transition temperatures |
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| Title | Elastic modulus evolution of rocks under heating–cooling cycles |
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