Jialun Zhang , Qiang Ma , Fengxi Zhou , Zhenning Ba
{"title":"饱和冻土与饱和土交界面平面纵波传播特性研究","authors":"Jialun Zhang , Qiang Ma , Fengxi Zhou , Zhenning Ba","doi":"10.1016/j.coldregions.2025.104643","DOIUrl":null,"url":null,"abstract":"<div><div>Due to global warming and intensified human activities, the thawing of permafrost in some regions during summer has resulted in the formation of a saturated soil–saturated frozen soil geological interface. In response, this study establishes a wave propagation model for elastic waves at the interface between saturated frozen soil and saturated soil media, based on elastic wave propagation theory in porous media. Numerical calculations and three-dimensional visualization techniques are employed to analyze the influence of various parameters—such as incident frequency, incident angle, porosity, Poisson's ratio, and temperature in the saturated frozen soil, as well as porosity and Poisson's ratio in the saturated soil—on the amplitude transmission/reflection coefficients and energy flux at the interface. The results show that higher wave velocities enhance the resistance of transmission and reflection coefficients and energy flux to changes in incident frequency. Variations in the parameters of the saturated frozen soil medium, such as temperature, Poisson's ratio, and porosity, have a greater impact on reflected waves than on transmitted waves. Conversely, changes in the parameters of the saturated soil medium have a greater effect on transmitted waves than on reflected waves. When porosity or Poisson's ratio is varied within the same range in both media, some transmission/reflection waveforms exhibit completely opposite trends in amplitude coefficients and energy flux with respect to parameter variation.</div></div>","PeriodicalId":10522,"journal":{"name":"Cold Regions Science and Technology","volume":"240 ","pages":"Article 104643"},"PeriodicalIF":3.8000,"publicationDate":"2025-08-18","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":"{\"title\":\"Study on the propagation of plane longitudinal waves at the interface between saturated frozen soil and saturated soil\",\"authors\":\"Jialun Zhang , Qiang Ma , Fengxi Zhou , Zhenning Ba\",\"doi\":\"10.1016/j.coldregions.2025.104643\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"<div><div>Due to global warming and intensified human activities, the thawing of permafrost in some regions during summer has resulted in the formation of a saturated soil–saturated frozen soil geological interface. In response, this study establishes a wave propagation model for elastic waves at the interface between saturated frozen soil and saturated soil media, based on elastic wave propagation theory in porous media. Numerical calculations and three-dimensional visualization techniques are employed to analyze the influence of various parameters—such as incident frequency, incident angle, porosity, Poisson's ratio, and temperature in the saturated frozen soil, as well as porosity and Poisson's ratio in the saturated soil—on the amplitude transmission/reflection coefficients and energy flux at the interface. The results show that higher wave velocities enhance the resistance of transmission and reflection coefficients and energy flux to changes in incident frequency. Variations in the parameters of the saturated frozen soil medium, such as temperature, Poisson's ratio, and porosity, have a greater impact on reflected waves than on transmitted waves. Conversely, changes in the parameters of the saturated soil medium have a greater effect on transmitted waves than on reflected waves. When porosity or Poisson's ratio is varied within the same range in both media, some transmission/reflection waveforms exhibit completely opposite trends in amplitude coefficients and energy flux with respect to parameter variation.</div></div>\",\"PeriodicalId\":10522,\"journal\":{\"name\":\"Cold Regions Science and Technology\",\"volume\":\"240 \",\"pages\":\"Article 104643\"},\"PeriodicalIF\":3.8000,\"publicationDate\":\"2025-08-18\",\"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/S0165232X25002265\",\"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/S0165232X25002265","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}
Study on the propagation of plane longitudinal waves at the interface between saturated frozen soil and saturated soil
Due to global warming and intensified human activities, the thawing of permafrost in some regions during summer has resulted in the formation of a saturated soil–saturated frozen soil geological interface. In response, this study establishes a wave propagation model for elastic waves at the interface between saturated frozen soil and saturated soil media, based on elastic wave propagation theory in porous media. Numerical calculations and three-dimensional visualization techniques are employed to analyze the influence of various parameters—such as incident frequency, incident angle, porosity, Poisson's ratio, and temperature in the saturated frozen soil, as well as porosity and Poisson's ratio in the saturated soil—on the amplitude transmission/reflection coefficients and energy flux at the interface. The results show that higher wave velocities enhance the resistance of transmission and reflection coefficients and energy flux to changes in incident frequency. Variations in the parameters of the saturated frozen soil medium, such as temperature, Poisson's ratio, and porosity, have a greater impact on reflected waves than on transmitted waves. Conversely, changes in the parameters of the saturated soil medium have a greater effect on transmitted waves than on reflected waves. When porosity or Poisson's ratio is varied within the same range in both media, some transmission/reflection waveforms exhibit completely opposite trends in amplitude coefficients and energy flux with respect to parameter variation.
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.