Xuanmei Fan, Zetao Feng, Tao Ni, Yu Deng, Jing Zhang, Lanxin Dai
{"title":"与岩冰分离有关的岩冰雪崩的摩擦行为:来自水槽物理实验的见解","authors":"Xuanmei Fan, Zetao Feng, Tao Ni, Yu Deng, Jing Zhang, Lanxin Dai","doi":"10.1029/2024JF007904","DOIUrl":null,"url":null,"abstract":"<p>Rock-ice avalanches in cold-high mountainous regions exhibit remarkably high mobility, frequently resulting in catastrophic consequences. However, the systematic influence of ice on the mobility of rock-ice avalanches remains poorly understood. This paper addresses this gap by conducting a comprehensive flume experiment in a temperature-controlled room at −10°C, simulating rock-ice avalanches and considering variations in rock-ice particle size ratios and ice contents. Overall mobility and segregation patterns are quantified by analyzing deposition characteristics, while high-speed cameras capture velocity and segregation features during motion. Our investigation reveals a notable rock-ice segregation phenomenon that significantly impacts the mobility of the mixture. Building on insights from prior numerical experiments conducted under nearly-no-base-slip conditions (Feng et al., 2023, https://doi.org/10.1029/2023jf007115), our results underscore that the particle segregation simultaneously influences both internal (bulk) and basal frictions, thereby producing different nonlinear impacts on the mobility of the rock-ice flow. Additionally, an empirical formula is proposed to describe the evolution of the friction coefficient in cases with different rock-ice particle size ratios and ice contents. These findings have significant implications for predicting runout and assessing the risk of rock-ice avalanches.</p>","PeriodicalId":15887,"journal":{"name":"Journal of Geophysical Research: Earth Surface","volume":"130 1","pages":""},"PeriodicalIF":3.5000,"publicationDate":"2025-01-03","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"The Friction Behavior of Rock-Ice Avalanches in Relation to Rock-Ice Segregation: Insights From Flume Physical Experiments\",\"authors\":\"Xuanmei Fan, Zetao Feng, Tao Ni, Yu Deng, Jing Zhang, Lanxin Dai\",\"doi\":\"10.1029/2024JF007904\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<p>Rock-ice avalanches in cold-high mountainous regions exhibit remarkably high mobility, frequently resulting in catastrophic consequences. However, the systematic influence of ice on the mobility of rock-ice avalanches remains poorly understood. This paper addresses this gap by conducting a comprehensive flume experiment in a temperature-controlled room at −10°C, simulating rock-ice avalanches and considering variations in rock-ice particle size ratios and ice contents. Overall mobility and segregation patterns are quantified by analyzing deposition characteristics, while high-speed cameras capture velocity and segregation features during motion. Our investigation reveals a notable rock-ice segregation phenomenon that significantly impacts the mobility of the mixture. Building on insights from prior numerical experiments conducted under nearly-no-base-slip conditions (Feng et al., 2023, https://doi.org/10.1029/2023jf007115), our results underscore that the particle segregation simultaneously influences both internal (bulk) and basal frictions, thereby producing different nonlinear impacts on the mobility of the rock-ice flow. Additionally, an empirical formula is proposed to describe the evolution of the friction coefficient in cases with different rock-ice particle size ratios and ice contents. These findings have significant implications for predicting runout and assessing the risk of rock-ice avalanches.</p>\",\"PeriodicalId\":15887,\"journal\":{\"name\":\"Journal of Geophysical Research: Earth Surface\",\"volume\":\"130 1\",\"pages\":\"\"},\"PeriodicalIF\":3.5000,\"publicationDate\":\"2025-01-03\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"0\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Journal of Geophysical Research: Earth Surface\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://onlinelibrary.wiley.com/doi/10.1029/2024JF007904\",\"RegionNum\":2,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q1\",\"JCRName\":\"GEOSCIENCES, MULTIDISCIPLINARY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Earth Surface","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2024JF007904","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q1","JCRName":"GEOSCIENCES, MULTIDISCIPLINARY","Score":null,"Total":0}
The Friction Behavior of Rock-Ice Avalanches in Relation to Rock-Ice Segregation: Insights From Flume Physical Experiments
Rock-ice avalanches in cold-high mountainous regions exhibit remarkably high mobility, frequently resulting in catastrophic consequences. However, the systematic influence of ice on the mobility of rock-ice avalanches remains poorly understood. This paper addresses this gap by conducting a comprehensive flume experiment in a temperature-controlled room at −10°C, simulating rock-ice avalanches and considering variations in rock-ice particle size ratios and ice contents. Overall mobility and segregation patterns are quantified by analyzing deposition characteristics, while high-speed cameras capture velocity and segregation features during motion. Our investigation reveals a notable rock-ice segregation phenomenon that significantly impacts the mobility of the mixture. Building on insights from prior numerical experiments conducted under nearly-no-base-slip conditions (Feng et al., 2023, https://doi.org/10.1029/2023jf007115), our results underscore that the particle segregation simultaneously influences both internal (bulk) and basal frictions, thereby producing different nonlinear impacts on the mobility of the rock-ice flow. Additionally, an empirical formula is proposed to describe the evolution of the friction coefficient in cases with different rock-ice particle size ratios and ice contents. These findings have significant implications for predicting runout and assessing the risk of rock-ice avalanches.