A sound understanding of groundwater recharged from various sources occurring at different time scales is crucial for water management in arid and semi-arid riv
Granular mass flows(e.g., debris flows/avalanches) in landslide-prone areas are of great concern because they often cause catastrophic disasters as a result of
This paper describes the application of a three-dimensional lattice Boltzmann method(LBM) to Newtonian and non-Newtonian(Bingham fluid in this work) flows with