首页 | 本学科首页   官方微博 | 高级检索  
     检索      


A depth average SPH model including μ(I) rheology and crushing for rock avalanches
Authors:Alberto Longo  Manuel Pastor  Lorenzo Sanavia  Diego Manzanal  Miguel Martin Stickle  Chuan Lin  Angel Yague  Saeid Moussavi Tayyebi
Institution:1. DICEA, Università degli Studi di Padova, Padova, Italy;2. Department of Applied Mathematics, ETSI Caminos, Universidad Politécnica de Madrid, Madrid, Spain;3. College of Water Conservancy and Hydropower, Hohai University, Nanjing, China
Abstract:Classical depth-integrated smoothed particle hydrodynamics (SPH) models for avalanches are extended in the present work to include a μ(I)− rheological model enriched with a fragmentation law. With this improvement, the basal friction becomes grain distribution dependent. Rock avalanches, where grain distribution tends to change with time while propagating, are the appropriate type of landslide to apply the new numerical proposal. The μ(I)− rheological models considered in the present work are those of Hatano and Gray, combined with two different fragmentation laws, a hyperbolic and a fractal-based law. As an application, Frank avalanche, which took place in Canada in 1903, is analyzed under the scope of the present approach, focusing in the influence of the rheological and fragmentation laws in the evolution of the avalanche.
Keywords:depth-integrated models  Frank rock avalanche  inertia number  rheology  rock avalanches  rock fragmentation  SPH
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号