Discrete and continuum modelling of rock-ice avalanches: vertical segregation and its feedback on flow mobility-Reference-Cited by-同舟云学术

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Discrete and continuum modelling of rock-ice avalanches: vertical segregation and its feedback on flow mobility

Published:2024-11 Issue: Volume:175 Page:106691
ISSN:0266-352X
Container-title:Computers and Geotechnics
language:en
Short-container-title:Computers and Geotechnics

Author:

Cui Kahlil F.E.,Zhou Gordon G.D.,Jing Lu^ORCID

Funder

National Natural Science Foundation of China

Alliance of International Science Organizations

Institute of Mountain Hazards and Environment Chinese Academy of Sciences

Sichuan Province Science and Technology Support Program

Ministry of Science and Technology of the People's Republic of China

Publisher

Elsevier BV

Reference72 articles.

1. Ice avalanches: some empirical information about their formation and reach;Alean;J. Glaciol.,1985

2. Bartelt, P., Christen, B., Buhler, Y., & Buser, O. (2018). Thermomechanical modelling of rock avalanches with debris, ice, and snow entrainment. Numerical Methods in Geotechnical Engineering IX. Volume 2: Proceedings of the 9th European Conference on Numerical Methods in Geotechnical Engineering (NUMGE 2018), 1047–1054.

3. Non-local rheology in dense granular flows: Revisiting the concept of fluidity;Bouzid;European Physical Journal E,2015

4. The basal friction coefficient of granular flows with and without excess pore pressure: implications for pyroclastic density currents, water-rich debris flows, and rock and submarine avalanches;Breard;J. Geophys. Res. Solid Earth,2020

5. Generalized friction and dilatancy laws for immersed granular flows consisting of large and small particles;Cui;Phys. Fluids,2020

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