Experimental Investigation of Turbulence Transition of Natural Convection Boundary Layer Along a Vertical Plate in Water With Sub-Millimeter-Bubble Injection

Author(s):  
Atsuhide Kitagawa ◽  
Hiroki Endo ◽  
Yoshimichi Hagiwara

This paper presents an experimental investigation of the turbulence transition of the natural convection boundary layer along a vertical plate in water with sub-millimeter-bubble injection. In this study, we focus on the relationship between the bubble injection position L and the turbulence transition of the boundary layer. Temperature and velocity measurements show that sub-millimeter-bubble injection for L = 1.6 mm suppresses the turbulence transition of the natural convection boundary layer, while that for L = 3.6 mm enhances the turbulence transition of the boundary layer. For L = 1.6 mm, the appearance region of the bubble-induced liquid velocity fluctuation at the upstream unheated section is restricted near the wall, though the peak value of the liquid velocity fluctuation is high. In contrast, in the case of L = 3.6 mm, the relatively large liquid velocity fluctuation induced by bubbles at the upstream unheated section distributes widely over the laminar boundary layer width. Therefore, we expect that the turbulence transition of the natural convection boundary layer for the case with bubble injection depends on the magnitude and appearance region of the bubble-induced liquid velocity fluctuation at the upstream unheated section.

Author(s):  
Yasuo Hattori ◽  
Hitoshi Suto

A turbulent natural-convection boundary layer in air near the upper surface of a heated round plate is experimentally investigated. The heated round plate, the diameter of which is 300 mm, is horizontally placed in a test section of chamber. The upper-surface temperature is 473 K. Instantaneous temperature and two-dimensional velocity vectors near the upper surface are measured by using a cold wire and a particle image velocimetry, respectively. The measurements reveal a multi-layer structure near the upper surface. In the lower layer, velocity fluctuation of horizontal component is active compared with that of vertical component. This intermittently causes the incursion of low temperature fluids. On the other hand, in the upper layer, the intensity of vertical velocity fluctuation with high temperature fluid is much larger than that of horizontal velocity fluctuation. This multi-layer structure is mainly generated by the large-scale fluid motions, such as winding of high temperature fluids and entrainment of low temperature fluids.


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