中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Failure modes of basal-ice moraine slopes under combined hydrothermal conditions: laboratory evidence

文献类型:期刊论文

作者Cao, Jingxuan1,2; Wang, Jiao1,2,3; Cui, Peng1,2,3; Liu, Zhenxing1,4; Yang, Can1,2; Wang, Hao2; Shu, Tao1,2
刊名CATENA
出版日期2026-04-01
卷号265页码:109906
关键词Basal-ice moraine slopes Hydrothermal conditions Laboratory flume modeling Failure modes
ISSN号0341-8162
DOI10.1016/j.catena.2026.109906
产权排序3
文献子类Article
英文摘要The stability of basal-ice moraine slopes (BIMS) is increasingly threatened by climate warming, posing a significant geohazard in high-altitude regions. The degradation of buried basal ice, coupled with intense rainfall, induces complex thermo-hydro-mechanical (THM) interactions, yet the specific failure mechanisms remain insufficiently understood. This study provides direct experimental evidence using instrumented laboratory flume experiments to investigate the failure characteristics of BIMS under controlled thermal and rainfall conditions. By systematically analyzing volumetric water content, soil pressure, pore water pressure and deformation, we clarify the regulatory role of the ice-soil interface in slope instability. Results demonstrate this interface is the primary control, governing heat transfer and meltwater redistribution. We identify two distinct failure pathways: temperature-driven instability is progressive, evolving from initial slope-toe failure to large-scale misaligned sliding, where rising temperatures accelerate meltwater accumulation. In stark contrast, rainfall-induced instability is abrupt, characterized by rapid slope disintegration and surface flow-slips, with intense rainfall showing the potential to trigger debris flows. These findings elucidate the coupled THM failure mechanisms of BIMS, providing a robust scientific basis for process-based hazard assessment and risk mitigation in cold-region mountainous environments.
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WOS关键词TIBETAN PLATEAU ; CRUST FORMATION ; CLIMATE-CHANGE ; DEBRIS FLOWS ; GLACIER ; DYNAMICS
WOS研究方向Geology ; Agriculture ; Water Resources
语种英语
WOS记录号WOS:001690359700001
出版者ELSEVIER
源URL[http://ir.igsnrr.ac.cn/handle/311030/220883]  
专题陆地表层格局与模拟院重点实验室_外文论文
通讯作者Wang, Jiao
作者单位1.Univ Chinese Acad Sci, Beijing 100049, Peoples R China
2.Chinese Acad Sci, Inst Mt Hazards & Environm, Key Lab Mt Hazards & Engn Resilience, Chengdu 610041, Peoples R China;
3.CAS HEC, China Pakistan Joint Res Ctr Earth Sci, Islamabad 45320, Pakistan;
4.Chinese Acad Sci, Inst Geog Sci & Nat Resources Res, Key Lab Land Surface Pattern & Simulat, Beijing 100101, Peoples R China;
推荐引用方式
GB/T 7714
Cao, Jingxuan,Wang, Jiao,Cui, Peng,et al. Failure modes of basal-ice moraine slopes under combined hydrothermal conditions: laboratory evidence[J]. CATENA,2026,265:109906.
APA Cao, Jingxuan.,Wang, Jiao.,Cui, Peng.,Liu, Zhenxing.,Yang, Can.,...&Shu, Tao.(2026).Failure modes of basal-ice moraine slopes under combined hydrothermal conditions: laboratory evidence.CATENA,265,109906.
MLA Cao, Jingxuan,et al."Failure modes of basal-ice moraine slopes under combined hydrothermal conditions: laboratory evidence".CATENA 265(2026):109906.

入库方式: OAI收割

来源:地理科学与资源研究所

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