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Transient Numerical Analysis of Natural Convection in Partially Open Cavities Filled with Water near the Density Inversion Point
by
da Silva, A.
, Capeletto, C. A.
, Mariani, V. C.
, Fontana, E.
in
Buoyancy
/ Convection
/ Creasing
/ Free convection
/ Freezing
/ Heat sources
/ Heat transfer
/ Heated water
/ Holes
/ Numerical analysis
/ Physical properties
/ Qualitative analysis
/ Thermal plumes
2020
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Transient Numerical Analysis of Natural Convection in Partially Open Cavities Filled with Water near the Density Inversion Point
by
da Silva, A.
, Capeletto, C. A.
, Mariani, V. C.
, Fontana, E.
in
Buoyancy
/ Convection
/ Creasing
/ Free convection
/ Freezing
/ Heat sources
/ Heat transfer
/ Heated water
/ Holes
/ Numerical analysis
/ Physical properties
/ Qualitative analysis
/ Thermal plumes
2020
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While trying to remove the title from your shelf something went wrong :( Kindly try again later!
Do you wish to request the book?
Transient Numerical Analysis of Natural Convection in Partially Open Cavities Filled with Water near the Density Inversion Point
by
da Silva, A.
, Capeletto, C. A.
, Mariani, V. C.
, Fontana, E.
in
Buoyancy
/ Convection
/ Creasing
/ Free convection
/ Freezing
/ Heat sources
/ Heat transfer
/ Heated water
/ Holes
/ Numerical analysis
/ Physical properties
/ Qualitative analysis
/ Thermal plumes
2020
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Transient Numerical Analysis of Natural Convection in Partially Open Cavities Filled with Water near the Density Inversion Point
Journal Article
Transient Numerical Analysis of Natural Convection in Partially Open Cavities Filled with Water near the Density Inversion Point
2020
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Overview
A transient numerical analysis of natural convection of near-freezing water in a cavity with lateral openings and internal heat sources is carried out to investigate the influence of the heat dissipation rate in the flow configuration. The heat sources were positioned to create buoyancy-opposing and buoyancy-assisted conditions simultaneously and the top and bottom walls are kept at 0◦C. The non-linear dependence of the physical properties with temperature is considered in the governing equations. Based on the heat dissipation rate, six different regimes were observed and classified through a qualitative analysis of the temporal evolution of the velocity and temperature fields. The characteristics of heat transfer for each regime are analyzed to define the most important mechanisms of heat removal. In the upper layer (heated from below), the buoyancy forces eventually overcome the viscous forces and unsteady thermal plumes are formed, in-creasing the heat removal through the openings, while the heat transfer with the top wall is not significant. In the lower layer, the development of wave-like instabilities leads to oscillatory regimes for intermediate heat dissipation rates, while for high dissipation rates a steady convective regime is observed. This behavior increases the heat transfer with the bottom wall, making it much more significant when compared with the upper layer.
Publisher
Isfahan University of Technology
Subject
MBRLCatalogueRelatedBooks
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