2014
DOI: 10.1017/jfm.2014.207
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Dynamics of line plumes on horizontal surfaces in turbulent convection

Abstract: We study the dynamics of line plumes on the bottom plate in turbulent convection over six decades of Rayleigh number $(10^5 Show more

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Cited by 16 publications
(24 citation statements)
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“…The predicted average interplume area is in good agreement with the peaks of the statistical distributions for the three cases discussed here. The expression (3.15) therefore provides a reasonable estimate of the average plume separation (Puthenveettil & Arakeri 2005;Puthenveettil et al 2011;Gunasegarane & Puthenveettil 2014). The comparable observed plume density at both thermal boundary layers thus yields…”
Section: Conservation Of the Average Plume Density In Spherical Shellsmentioning
confidence: 56%
“…The predicted average interplume area is in good agreement with the peaks of the statistical distributions for the three cases discussed here. The expression (3.15) therefore provides a reasonable estimate of the average plume separation (Puthenveettil & Arakeri 2005;Puthenveettil et al 2011;Gunasegarane & Puthenveettil 2014). The comparable observed plume density at both thermal boundary layers thus yields…”
Section: Conservation Of the Average Plume Density In Spherical Shellsmentioning
confidence: 56%
“…They are formed in the vicinity of the heated (cooled) plate, then rise (fall) into the bulk of the turbulent convection layer and provide the major contribution to the near-wall turbulent heat transfer and its local fluctuations. Their dynamics and size have been studied, for example, in experiments [15][16][17] and direct numerical simulations [18][19][20][21]. Here, we will describe the formation of thermal plumes by the vertical temperature derivatives in connection to the two-dimensional velocity gradient vector field directly at the heated (cooled) plate.…”
Section: Introductionmentioning
confidence: 99%
“…given by Gunasegarane & Puthenveettil (2014). The corresponding large-scale flow velocity is U LS = 0.42 cm s −1 .…”
Section: Declaration Of Interestsmentioning
confidence: 99%
“…The light green lines in the image are the line plumes created by the instability of the natural convection boundary layers in between these plumes, which are subjected to a transpiration through the membrane. In addition to the fact that the boundary layer lengths are spatially random, the flow induced by these plumes causes these plumes to keep merging (Gunasegarane & Puthenveettil 2014) so that the random pattern in figure 6( a ) keeps evolving spatially and temporally with time. These boundary layers then form and are destroyed by the plume motion at various random locations and at various temporal instants above a horizontal porous surface.…”
Section: Theoretical Profilesmentioning
confidence: 99%
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