Application of Nonlinear Systems in Nanomechanics and Nanofluids 2015
DOI: 10.1016/b978-0-323-35237-6.00006-6
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Natural, Mixed, and Forced Convection in Nanofluid

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Cited by 3 publications
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“…[18b] Poiseuille flow (also called convective flow) is the pressure-induced pore flow model generally adopted to describe the transport in a capillary or a porous medium. [99] In Poiseuille flow when the pores are very small and the mean free path of the gases and ions is larger than the pore diameter, collisions with the pore will occur and the lighter molecules will then preferentially pass through the membrane.…”
Section: Transport Mechanismmentioning
confidence: 99%
“…[18b] Poiseuille flow (also called convective flow) is the pressure-induced pore flow model generally adopted to describe the transport in a capillary or a porous medium. [99] In Poiseuille flow when the pores are very small and the mean free path of the gases and ions is larger than the pore diameter, collisions with the pore will occur and the lighter molecules will then preferentially pass through the membrane.…”
Section: Transport Mechanismmentioning
confidence: 99%
“…Mixed convection flows, which are also known as combined free and forced convection flows, occur in many technological and industrial applications and are driven by both external force and density difference 1 . In a reactor core, during the accident conditions, the passive decay heat removal system in the reactor becomes active, throughout the long‐term cooling phase, circulation of the coolant in fuel assembly is driven by buoyancy, and a mixed convection regime may occur under such conditions with a low flow rate 2 .…”
Section: Introductionmentioning
confidence: 99%
“…Ramachandran et al (1988) conducted a study related to the mixed convection in stagnation point flow. The mixed convection flow is a combination of forced and free convection flows that arise in many industrial processes such as in the cooling process of electronic devices and nuclear reactors, solar receivers and in heat exchangers (Ganji and Kachapi, 2015). This flow, which was first investigated by Merkin (1969), was characterized by the buoyancy parameter l = Gr/Re n (in his paper) where Gr is the Grashof number, Re is the Reynolds number and n(> 0) is a constant that depends on the surface heating conditions and flow configuration (Pop and Ingham, 2001).…”
mentioning
confidence: 99%