Document Type

Article

Publication Date

2015

Abstract

Gravity currents occur when fluids of different density are brought together. When gravity currents travel down a uniform slope, buoyancy effects become more important and changes the physical dynamics of its motion. In the present paper, we report data from full three-dimensional direct numerical simulation of gravity currents propagating down a uniform slope. Our data shows that in most cases, the gravity current evolve to a shape that is similar to a triangular wedge. The physical mechanisms leading to formation of this triangular shape and the dynamics of such a structure is presented

Comments

Under a Creative Commons license http://creativecommons.org/licenses/by-nc-nd/4.0/

Publication Title

Procedia Engineering

DOI

https://doi.org/10.1016/j.proeng.2015.11.216

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