Hui Liu , Mengjie Liu , Gengshe Yang , Xinyue Dai , Yanjun Shen , Bo Liang , Xiao Ding , Yali Xu , Runqi Wang
{"title":"基于声热联合监测的冻融砂岩损伤破坏前兆预警研究","authors":"Hui Liu , Mengjie Liu , Gengshe Yang , Xinyue Dai , Yanjun Shen , Bo Liang , Xiao Ding , Yali Xu , Runqi Wang","doi":"10.1016/j.coldregions.2025.104679","DOIUrl":null,"url":null,"abstract":"<div><div>Freeze-thaw rock damage evolution is crucial for safety assessment and disaster early warning in cold region engineering. This study implements acoustic-thermal monitoring to identify precursors of geotechnical instability. By correlating acoustic emission (AE) parameters (energy, amplitude) with infrared thermography indices (maximum/mean radiation temperature), we dynamically characterize localized damage progression from initiation through shear band formation to ultimate failure. The self-correlation coefficient and coefficient of variation are proposed to quantitatively describe the loading failure process and localization of freeze-thaw sandstone. The spatial failure characteristics of localization are analyzed, and the damage time characteristics are revealed. The research findings demonstrate that AE event nucleation clusters emerge at 0.8<span><math><msub><mi>σ</mi><mi>c</mi></msub></math></span>∼<span><math><msub><mi>σ</mi><mi>c</mi></msub></math></span>, signaling localized deformation initiation. The deformation localization zone of freeze-thaw rock is first formed in the middle, and the initial damage location significantly affects the formation and failure mode of the localization zone. The self-correlation coefficient and the mutation point of the coefficient of variation of the acoustic emission can be used as the criterion of its formation time, and the change rule of the time and space entropy curve reflects the localization stage. The localized failure time of sandstone is advanced with the increase of freeze-thaw times. Comparative analysis of acoustic-thermal indicators reveals that auto-correlation coefficients exhibit superior sensitivity in characterizing deformation localization compared to thermal parameters. The integration of infrared thermography and AE monitoring significantly enhances reliability in identifying precursory signals for rock instability and engineering catastrophes in cold regions.The combination of acoustic emission and thermal imaging technology can realize the advance warning of rock burst in the early warning of tunnel freeze-thaw disaster. In the stability management of frozen soil slope, a three-level risk classification threshold can be constructed to provide theoretical support for the differential support decision of engineering in cold regions. It is more advantageous to improve the reliability of freeze-thaw rock instability and failure and rock engineering disaster precursor identification in cold regions.</div></div>","PeriodicalId":10522,"journal":{"name":"Cold Regions Science and Technology","volume":"241 ","pages":"Article 104679"},"PeriodicalIF":3.8000,"publicationDate":"2025-09-13","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Research on precursory warning of damage and failure in freeze-thaw sandstone based on acoustic-thermal joint monitoring\",\"authors\":\"Hui Liu , Mengjie Liu , Gengshe Yang , Xinyue Dai , Yanjun Shen , Bo Liang , Xiao Ding , Yali Xu , Runqi Wang\",\"doi\":\"10.1016/j.coldregions.2025.104679\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Freeze-thaw rock damage evolution is crucial for safety assessment and disaster early warning in cold region engineering. This study implements acoustic-thermal monitoring to identify precursors of geotechnical instability. By correlating acoustic emission (AE) parameters (energy, amplitude) with infrared thermography indices (maximum/mean radiation temperature), we dynamically characterize localized damage progression from initiation through shear band formation to ultimate failure. The self-correlation coefficient and coefficient of variation are proposed to quantitatively describe the loading failure process and localization of freeze-thaw sandstone. The spatial failure characteristics of localization are analyzed, and the damage time characteristics are revealed. The research findings demonstrate that AE event nucleation clusters emerge at 0.8<span><math><msub><mi>σ</mi><mi>c</mi></msub></math></span>∼<span><math><msub><mi>σ</mi><mi>c</mi></msub></math></span>, signaling localized deformation initiation. The deformation localization zone of freeze-thaw rock is first formed in the middle, and the initial damage location significantly affects the formation and failure mode of the localization zone. The self-correlation coefficient and the mutation point of the coefficient of variation of the acoustic emission can be used as the criterion of its formation time, and the change rule of the time and space entropy curve reflects the localization stage. The localized failure time of sandstone is advanced with the increase of freeze-thaw times. Comparative analysis of acoustic-thermal indicators reveals that auto-correlation coefficients exhibit superior sensitivity in characterizing deformation localization compared to thermal parameters. The integration of infrared thermography and AE monitoring significantly enhances reliability in identifying precursory signals for rock instability and engineering catastrophes in cold regions.The combination of acoustic emission and thermal imaging technology can realize the advance warning of rock burst in the early warning of tunnel freeze-thaw disaster. In the stability management of frozen soil slope, a three-level risk classification threshold can be constructed to provide theoretical support for the differential support decision of engineering in cold regions. It is more advantageous to improve the reliability of freeze-thaw rock instability and failure and rock engineering disaster precursor identification in cold regions.</div></div>\",\"PeriodicalId\":10522,\"journal\":{\"name\":\"Cold Regions Science and Technology\",\"volume\":\"241 \",\"pages\":\"Article 104679\"},\"PeriodicalIF\":3.8000,\"publicationDate\":\"2025-09-13\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Cold Regions Science and Technology\",\"FirstCategoryId\":\"5\",\"ListUrlMain\":\"https://www.sciencedirect.com/science/article/pii/S0165232X25002629\",\"RegionNum\":2,\"RegionCategory\":\"工程技术\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"ENGINEERING, CIVIL\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Cold Regions Science and Technology","FirstCategoryId":"5","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0165232X25002629","RegionNum":2,"RegionCategory":"工程技术","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"ENGINEERING, CIVIL","Score":null,"Total":0}
Research on precursory warning of damage and failure in freeze-thaw sandstone based on acoustic-thermal joint monitoring
Freeze-thaw rock damage evolution is crucial for safety assessment and disaster early warning in cold region engineering. This study implements acoustic-thermal monitoring to identify precursors of geotechnical instability. By correlating acoustic emission (AE) parameters (energy, amplitude) with infrared thermography indices (maximum/mean radiation temperature), we dynamically characterize localized damage progression from initiation through shear band formation to ultimate failure. The self-correlation coefficient and coefficient of variation are proposed to quantitatively describe the loading failure process and localization of freeze-thaw sandstone. The spatial failure characteristics of localization are analyzed, and the damage time characteristics are revealed. The research findings demonstrate that AE event nucleation clusters emerge at 0.8∼, signaling localized deformation initiation. The deformation localization zone of freeze-thaw rock is first formed in the middle, and the initial damage location significantly affects the formation and failure mode of the localization zone. The self-correlation coefficient and the mutation point of the coefficient of variation of the acoustic emission can be used as the criterion of its formation time, and the change rule of the time and space entropy curve reflects the localization stage. The localized failure time of sandstone is advanced with the increase of freeze-thaw times. Comparative analysis of acoustic-thermal indicators reveals that auto-correlation coefficients exhibit superior sensitivity in characterizing deformation localization compared to thermal parameters. The integration of infrared thermography and AE monitoring significantly enhances reliability in identifying precursory signals for rock instability and engineering catastrophes in cold regions.The combination of acoustic emission and thermal imaging technology can realize the advance warning of rock burst in the early warning of tunnel freeze-thaw disaster. In the stability management of frozen soil slope, a three-level risk classification threshold can be constructed to provide theoretical support for the differential support decision of engineering in cold regions. It is more advantageous to improve the reliability of freeze-thaw rock instability and failure and rock engineering disaster precursor identification in cold regions.
期刊介绍:
Cold Regions Science and Technology is an international journal dealing with the science and technical problems of cold environments in both the polar regions and more temperate locations. It includes fundamental aspects of cryospheric sciences which have applications for cold regions problems as well as engineering topics which relate to the cryosphere.
Emphasis is given to applied science with broad coverage of the physical and mechanical aspects of ice (including glaciers and sea ice), snow and snow avalanches, ice-water systems, ice-bonded soils and permafrost.
Relevant aspects of Earth science, materials science, offshore and river ice engineering are also of primary interest. These include icing of ships and structures as well as trafficability in cold environments. Technological advances for cold regions in research, development, and engineering practice are relevant to the journal. Theoretical papers must include a detailed discussion of the potential application of the theory to address cold regions problems. The journal serves a wide range of specialists, providing a medium for interdisciplinary communication and a convenient source of reference.