A vertically non-uniform temperature approach for the friction term computation in depth-averaged viscoplastic lava flows
DOI10.1016/J.JCP.2024.113378MaRDI QIDQ6639293
P. García-Navarro, S. Martínez-Aranda, J. Fernández-Pato, J. Ortega-Moya
Publication date: 15 November 2024
Published in: Journal of Computational Physics (Search for Journal in Brave)
finite volume methodsBingham modeltemperature exchangedepth-averaged non-Newtonian modelsliquefied lava flowsviscoplastic shallow flows
Basic methods in fluid mechanics (76Mxx) Multiphase and multicomponent flows (76Txx) Geophysics (86Axx)
Cites Work
- Depth averaged models for fast landslide propagation: mathematical, rheological and numerical aspects
- Wave Riemann description of friction terms in unsteady shallow flows: application to water and mud/debris floods
- The space-time CESE scheme for shallow water equations incorporating variable bottom topography and horizontal temperature gradients
- Modified shallow water model for viscous fluids and positivity preserving numerical approximation
- The Riemann problem for the shallow water equations with horizontal temperature gradients
- A depth-integrated, coupled SPH model for flow-like landslides and related phenomena
- Numerical modelling of the propagation of fast landslides using the finite element method
- The Dynamics of Lava Flows
- Finite Volume Models and Efficient Simulation Tools (EST) for Shallow Flows
- A depth-averaged debris-flow model that includes the effects of evolving dilatancy. I. Physical basis
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