2021
DOI: 10.1016/j.ijheatmasstransfer.2020.120758
|View full text |Cite
|
Sign up to set email alerts
|

Simulating natural convection with high Rayleigh numbers using the Smoothed Particle Hydrodynamics method

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
1

Citation Types

0
0
0

Year Published

2021
2021
2024
2024

Publication Types

Select...
6

Relationship

0
6

Authors

Journals

citations
Cited by 15 publications
(1 citation statement)
references
References 50 publications
0
0
0
Order By: Relevance
“…The disparity in density produced due to the temperature change creates a buoyancy force, which propels the movement of fluid flow close to the surface. This process is called free or natural convection, where the fluid behind the heated or cooled layer remains stationary (zero velocity) with a constant temperature [8,18].…”
Section: Natural Convection and Its Boundary Layersmentioning
confidence: 99%
“…The disparity in density produced due to the temperature change creates a buoyancy force, which propels the movement of fluid flow close to the surface. This process is called free or natural convection, where the fluid behind the heated or cooled layer remains stationary (zero velocity) with a constant temperature [8,18].…”
Section: Natural Convection and Its Boundary Layersmentioning
confidence: 99%