Effects of chemical reaction, heat and mass diffusion in natural convection flow from an isothermal sphere with temperature dependent viscosity

DOI10.1108/02644400610689929zbMath1182.76962OpenAlexW2001071543WikidataQ57932864 ScholiaQ57932864MaRDI QIDQ5190543

Md. Mamun Molla, Md. Anwar Hossain

Publication date: 18 March 2010

Published in: Engineering Computations (Search for Journal in Brave)

Full work available at URL: https://doi.org/10.1108/02644400610689929

zbMATH Keywords

convectionchemical reactionsviscosity

Mathematics Subject Classification ID

Diffusion (76R50) Finite difference methods applied to problems in fluid mechanics (76M20) Free convection (76R10) Reaction effects in flows (76V05)

Related Items (3)

Modeling of free convection boundary layer flow on a solid sphere with Newtonian heating ⋮ Transient boundary layer flow of viscous compressible fluid past a heated sphere with the effect of Mach number ⋮ A fitted numerical method to investigate the effect of various parameters on an MHD flow over an inclined plate

Cites Work

• Flow and mass transfer on a stretching sheet with a magnetic field and chemically reactive species
• Transient free convection flow with temperature dependent viscosity in a fluid saturated porous medium
• Influence de gradients de propriétés physiques en convection forcee - application au cas du tube
• Analysis of mixed forced and free convection about a sphere
• Numerical study of the combined free-forced convective laminar boundary layer flow past a vertical isothermal flat plate with temperature-dependent viscosity
• Natural convection flow of a viscous fluid about a truncated cone with temperature-dependent viscosity
• Natural convection of fluid with variable viscosity from a heated vertical wavy surface
• Combined heat and mass transfer in natural convection flow from a vertical wavy surface
• The effect of temperature-dependent viscosity on free-forced convective laminar boundary layer flow past a vertical isothermal flat plate
• The nature of vertical natural convection flows resulting from the combined buoyancy effects of thermal and mass diffusion
• The effects of significant viscosity variation on convective heat transport in water-saturated porous media

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