Dipeng Zhu, Zhiyong Hu, Shuguang Zhang, Wei Qiu, Yijie Wang, Donglan Chen, Fan Mingzhuo, Shutian Zhao, Ye Sun, Wenbo Liu
{"title":"考虑硬化效应的岩石非线性蠕变本构模型","authors":"Dipeng Zhu, Zhiyong Hu, Shuguang Zhang, Wei Qiu, Yijie Wang, Donglan Chen, Fan Mingzhuo, Shutian Zhao, Ye Sun, Wenbo Liu","doi":"10.1155/gfl/2982047","DOIUrl":null,"url":null,"abstract":"<p>The creep of rock is a complex mechanical phenomenon driven by internal stress adjustment and the interplay between hardening and damage effects. To precisely capture the nonlinearity of rock creep and the law of accelerated deformation, a hardening function and a damage variable are introduced. Based on traditional rheological models, creep mechanisms, and damage laws, an accelerated creep constitutive model integrating hardening and damage effects is established. This model uses nonlinear functions and physical parameters to describe the coupling of hardening and damage throughout the creep process. The results show that the model can accurately reproduce the entire creep curves of rock specimens under different stress levels, with correlation coefficients exceeding 0.90. Further verification with diverse test data confirms its ability to describe the whole creep process and reflect the hardening–damage mechanisms, enabling accurate prediction of the transition to the failure-prone tertiary creep stage. Overall, this constitutive model provides a more accurate theoretical tool for understanding rock creep, offering significant value for rock engineering design and stability analysis in projects like underground mining and tunneling.</p>","PeriodicalId":12512,"journal":{"name":"Geofluids","volume":"2025 1","pages":""},"PeriodicalIF":1.2000,"publicationDate":"2025-08-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1155/gfl/2982047","citationCount":"0","resultStr":"{\"title\":\"Nonlinear Creep Constitutive Model of Rock Considering Hardening Effect\",\"authors\":\"Dipeng Zhu, Zhiyong Hu, Shuguang Zhang, Wei Qiu, Yijie Wang, Donglan Chen, Fan Mingzhuo, Shutian Zhao, Ye Sun, Wenbo Liu\",\"doi\":\"10.1155/gfl/2982047\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>The creep of rock is a complex mechanical phenomenon driven by internal stress adjustment and the interplay between hardening and damage effects. To precisely capture the nonlinearity of rock creep and the law of accelerated deformation, a hardening function and a damage variable are introduced. Based on traditional rheological models, creep mechanisms, and damage laws, an accelerated creep constitutive model integrating hardening and damage effects is established. This model uses nonlinear functions and physical parameters to describe the coupling of hardening and damage throughout the creep process. The results show that the model can accurately reproduce the entire creep curves of rock specimens under different stress levels, with correlation coefficients exceeding 0.90. Further verification with diverse test data confirms its ability to describe the whole creep process and reflect the hardening–damage mechanisms, enabling accurate prediction of the transition to the failure-prone tertiary creep stage. Overall, this constitutive model provides a more accurate theoretical tool for understanding rock creep, offering significant value for rock engineering design and stability analysis in projects like underground mining and tunneling.</p>\",\"PeriodicalId\":12512,\"journal\":{\"name\":\"Geofluids\",\"volume\":\"2025 1\",\"pages\":\"\"},\"PeriodicalIF\":1.2000,\"publicationDate\":\"2025-08-18\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"https://onlinelibrary.wiley.com/doi/epdf/10.1155/gfl/2982047\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geofluids\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1155/gfl/2982047\",\"RegionNum\":4,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q3\",\"JCRName\":\"GEOCHEMISTRY & GEOPHYSICS\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geofluids","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1155/gfl/2982047","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q3","JCRName":"GEOCHEMISTRY & GEOPHYSICS","Score":null,"Total":0}
Nonlinear Creep Constitutive Model of Rock Considering Hardening Effect
The creep of rock is a complex mechanical phenomenon driven by internal stress adjustment and the interplay between hardening and damage effects. To precisely capture the nonlinearity of rock creep and the law of accelerated deformation, a hardening function and a damage variable are introduced. Based on traditional rheological models, creep mechanisms, and damage laws, an accelerated creep constitutive model integrating hardening and damage effects is established. This model uses nonlinear functions and physical parameters to describe the coupling of hardening and damage throughout the creep process. The results show that the model can accurately reproduce the entire creep curves of rock specimens under different stress levels, with correlation coefficients exceeding 0.90. Further verification with diverse test data confirms its ability to describe the whole creep process and reflect the hardening–damage mechanisms, enabling accurate prediction of the transition to the failure-prone tertiary creep stage. Overall, this constitutive model provides a more accurate theoretical tool for understanding rock creep, offering significant value for rock engineering design and stability analysis in projects like underground mining and tunneling.
期刊介绍:
Geofluids is a peer-reviewed, Open Access journal that provides a forum for original research and reviews relating to the role of fluids in mineralogical, chemical, and structural evolution of the Earth’s crust. Its explicit aim is to disseminate ideas across the range of sub-disciplines in which Geofluids research is carried out. To this end, authors are encouraged to stress the transdisciplinary relevance and international ramifications of their research. Authors are also encouraged to make their work as accessible as possible to readers from other sub-disciplines.
Geofluids emphasizes chemical, microbial, and physical aspects of subsurface fluids throughout the Earth’s crust. Geofluids spans studies of groundwater, terrestrial or submarine geothermal fluids, basinal brines, petroleum, metamorphic waters or magmatic fluids.