2010
DOI: 10.1016/s1001-6058(09)60050-0
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Transition to Taylor Vortex Flow Between Rotating Conical Cylinders

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Cited by 15 publications
(8 citation statements)
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“…Furthermore, Taylor vortices can appear in the flow field when the Taylor number (Ta) exceeds some critical value (Ta cr ), which depends on the Reynolds number of flow. Taylor vortices have been experimentally observed for Reynolds number above 800 (Li et al, 2010). Simple calculations show that our emulsions prepared at 10 and 30 wt% oil will break due to Taylor vortices (Almeida-Rivera and Bongers, 2010) and not due to shearing in simple shear flow ( Fig.…”
Section: Drop Breakage and Coalescence In Colloid Millsmentioning
confidence: 58%
“…Furthermore, Taylor vortices can appear in the flow field when the Taylor number (Ta) exceeds some critical value (Ta cr ), which depends on the Reynolds number of flow. Taylor vortices have been experimentally observed for Reynolds number above 800 (Li et al, 2010). Simple calculations show that our emulsions prepared at 10 and 30 wt% oil will break due to Taylor vortices (Almeida-Rivera and Bongers, 2010) and not due to shearing in simple shear flow ( Fig.…”
Section: Drop Breakage and Coalescence In Colloid Millsmentioning
confidence: 58%
“…So far, the studies of the flow in RLFR have not been given due attention. However, for the upside down device of with the inner one rotating and the outer one at rest have been experimentally studied by Wimmer [4,5] and numerically by Noui-Mehidi et al [6,7], Xu et al [8,9] and Li et al [10]. In [4,5] Wimmer studied the stability of basic flow and the transition to Taylor vortices, as well as the occurrence of Taylor vortex at different geometries.…”
Section: R Rmentioning
confidence: 99%
“…Such exchange processes are largely controlled by the chemical composition and physical properties of particles (Fu et al, 2009). Hydrodynamic-induced turbulence in shallow lakes appears to have a significant influence on the exchange between sediment and water and it can increase the suspension of sediment particles and even promote the outward movement of P dissolved in pore water (Bowes et al, 2008;Li et al, 2010). The P release from the sediment to the lake water occurs either as the mobilization of P from suspended sediment particles or after mobilization into the dissolved P-pool in sediment pore water and the subsequent upward transport of the dissolved species into the water (Sun et al, 2009).…”
Section: Introductionmentioning
confidence: 99%