AN ANALYTICAL AND EXPERIMENTAL STUDY OF THE MELTING OF BULK SOLIDS ON AN INCLINED PLANE HEATED SURFACE

1970 ◽  
Author(s):  
Owen M. Griffin ◽  
Albin A. Szewczyk
2004 ◽  
Vol 30 (3) ◽  
pp. 231-233 ◽  
Author(s):  
D. V. Zaitsev ◽  
E. A. Chinnov ◽  
O. A. Kabov ◽  
I. V. Marchuk

2009 ◽  
Vol 21 (8) ◽  
pp. 083305 ◽  
Author(s):  
Thomas Ward ◽  
Chi Wey ◽  
Robert Glidden ◽  
A. E. Hosoi ◽  
A. L. Bertozzi

2013 ◽  
Vol 663 ◽  
pp. 477-482
Author(s):  
Bin Ni ◽  
Jie Wen ◽  
Jun Liao ◽  
Hong Wu Deng

On the condition of water multiple jet impingements, a steady-state experimental study had been conducted for boiling heat transfer in an atmospheric pressure. The jet velocity was 0.95~1.59m/s and the sub-cooling degrees of jet fluid were 30~83°C.The results revealed that increasing either jet velocity or sub-cooling degrees would promote the heat flux through heated surface, and the effect was more pronounced in partial boiling regime than fully-developed boiling regime. The heat transfer with multiple jets is enhanced due to disturbance of different impingements. With modification of the factor which related to flow distance of fluid on heated surface, correlation which is applicable to one single impinging jet boiling, can also be used to calculate critical heat flux(CHF) in boiling heat transfer with multiple impinging jets.


1999 ◽  
Vol 400 ◽  
pp. 199-227 ◽  
Author(s):  
EMMANUEL AZANZA ◽  
FRANÇOIS CHEVOIR ◽  
PASCAL MOUCHERONT

The collisional flow of a slightly inelastic granular material down a rough inclined plane is usually described by kinetic theories. We present an experimental study aimed at analysing the assumptions and the quantitative predictions of such theories. A two-dimensional channel coupled to a model granular material and image analysis allow detailed and complete measurement of the kinematics and structure of the flows. We determine the range of inclination and particle flux for which the flow is stationary and uniform. The characteristic profiles of solid fraction, mean velocity and granular temperature are systematically measured. Both the true collisional and the dilute kinetic regimes are examined. We show that a quasi-hydrodynamic description of these regimes seems relevant, and that the pressure and the viscosity terms are in good qualitative agreement with the prediction of the kinetic theory. The profiles are well described by the kinetic theory near the top of the flow, at low solid fraction. Conversely there are large discrepancies near the rough plane, where the material is structured in layers.


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