{"title":"低温下人工多孔岩石动态力学行为的实验与理论研究","authors":"Ying Xu , Zhedong Xu , Shaoling Zheng , Bangbiao Wu , Zhemin You","doi":"10.1016/j.coldregions.2025.104562","DOIUrl":null,"url":null,"abstract":"<div><div>In cold regions, weathered rocks are subjected to complex geological environments characterized by sub-zero temperatures and dynamic disturbances. Understanding the dynamic compressive behavior of multi-cracked rocks under real-time low-temperature conditions is essential for assessing the stability of rock engineering. To simulate weathered, multi-cracked rocks, a clay-free artificial porous rock (APR) was used as the test material. Dynamic uniaxial compression experiments were performed at five ambient temperatures using a cryogenic-dynamic loading apparatus. Complementary quasi-static experiments were also conducted for comparison. The microscopic characteristics were analyzed through nuclear magnetic resonance (NMR), microstructural imaging, and failure mode evaluation. The results reveal that rate dependency becomes increasingly significant as ambient temperatures decreases. Specifically, when the loading rate is below 560 GPa/s, the dynamic uniaxial compressive strength (DUCS) of APR decreases with decreasing temperature. Beyond this rate, the DUCS exhibits a negative correlation with temperature, highlighting a distinct DUCS trend for APR compared to natural porous rocks. This behavior is primarily attributed to the Stefan effect of unfrozen water and the pressure melting effect during dynamic loading. Furthermore, a dynamic constitutive model based on the classic Ashby-Sammis micromechanical framework was proposed and validated. This model provides theoretical support for predicting the service performance of rock engineering in cold regions.</div></div>","PeriodicalId":10522,"journal":{"name":"Cold Regions Science and Technology","volume":"238 ","pages":"Article 104562"},"PeriodicalIF":3.8000,"publicationDate":"2025-05-26","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"An experimental and theoretical investigation of the dynamic mechanical behavior of artificial porous rock under sub-zero temperatures\",\"authors\":\"Ying Xu , Zhedong Xu , Shaoling Zheng , Bangbiao Wu , Zhemin You\",\"doi\":\"10.1016/j.coldregions.2025.104562\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>In cold regions, weathered rocks are subjected to complex geological environments characterized by sub-zero temperatures and dynamic disturbances. Understanding the dynamic compressive behavior of multi-cracked rocks under real-time low-temperature conditions is essential for assessing the stability of rock engineering. To simulate weathered, multi-cracked rocks, a clay-free artificial porous rock (APR) was used as the test material. Dynamic uniaxial compression experiments were performed at five ambient temperatures using a cryogenic-dynamic loading apparatus. Complementary quasi-static experiments were also conducted for comparison. The microscopic characteristics were analyzed through nuclear magnetic resonance (NMR), microstructural imaging, and failure mode evaluation. The results reveal that rate dependency becomes increasingly significant as ambient temperatures decreases. Specifically, when the loading rate is below 560 GPa/s, the dynamic uniaxial compressive strength (DUCS) of APR decreases with decreasing temperature. Beyond this rate, the DUCS exhibits a negative correlation with temperature, highlighting a distinct DUCS trend for APR compared to natural porous rocks. This behavior is primarily attributed to the Stefan effect of unfrozen water and the pressure melting effect during dynamic loading. Furthermore, a dynamic constitutive model based on the classic Ashby-Sammis micromechanical framework was proposed and validated. This model provides theoretical support for predicting the service performance of rock engineering in cold regions.</div></div>\",\"PeriodicalId\":10522,\"journal\":{\"name\":\"Cold Regions Science and Technology\",\"volume\":\"238 \",\"pages\":\"Article 104562\"},\"PeriodicalIF\":3.8000,\"publicationDate\":\"2025-05-26\",\"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/S0165232X25001454\",\"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/S0165232X25001454","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}
An experimental and theoretical investigation of the dynamic mechanical behavior of artificial porous rock under sub-zero temperatures
In cold regions, weathered rocks are subjected to complex geological environments characterized by sub-zero temperatures and dynamic disturbances. Understanding the dynamic compressive behavior of multi-cracked rocks under real-time low-temperature conditions is essential for assessing the stability of rock engineering. To simulate weathered, multi-cracked rocks, a clay-free artificial porous rock (APR) was used as the test material. Dynamic uniaxial compression experiments were performed at five ambient temperatures using a cryogenic-dynamic loading apparatus. Complementary quasi-static experiments were also conducted for comparison. The microscopic characteristics were analyzed through nuclear magnetic resonance (NMR), microstructural imaging, and failure mode evaluation. The results reveal that rate dependency becomes increasingly significant as ambient temperatures decreases. Specifically, when the loading rate is below 560 GPa/s, the dynamic uniaxial compressive strength (DUCS) of APR decreases with decreasing temperature. Beyond this rate, the DUCS exhibits a negative correlation with temperature, highlighting a distinct DUCS trend for APR compared to natural porous rocks. This behavior is primarily attributed to the Stefan effect of unfrozen water and the pressure melting effect during dynamic loading. Furthermore, a dynamic constitutive model based on the classic Ashby-Sammis micromechanical framework was proposed and validated. This model provides theoretical support for predicting the service performance of rock engineering 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.