Natural convection flow from a vertical permeable flat plate with variable surface temperature and species concentration

DOI10.1108/02644400010352261zbMath0982.76082OpenAlexW2043939991MaRDI QIDQ2701896

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Publication date: 8 April 2002

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

Full work available at URL: https://doi.org/10.1108/02644400010352261

zbMATH Keywords

asymptotic methodparametric investigationperturbation methodfree convectionbuoyancy forceboundary layer equationsspecies concentrationlocal non-similarity methodKeller-box methodvariable surface temperaturelarge transpiration parametersmall transpiration parametervertical permeable flat plate

Mathematics Subject Classification ID

Finite difference methods applied to problems in fluid mechanics (76M20) Asymptotic methods, singular perturbations applied to problems in fluid mechanics (76M45) Free convection (76R10)

Related Items (7)

Numerical investigation of natural convection viscoelastic Jeffrey's nanofluid flow from a vertical permeable flat plate with heat generation, thermal radiation, and chemical reaction ⋮ Effect of fluctuating surface heat and mass flux on natural convection flow along a vertical flat plate ⋮ Thermal radiation effects on heat and mass transfer over an unsteady stretching surface ⋮ Hydromagnetic flow of viscous incompressible fluid past a wedge with permeable surface ⋮ Thermal radiation and buoyancy effects on heat and mass transfer over a semi-infinite stretching surface with suction and blowing ⋮ Efficient Multi-Domain Bivariate Spectral Collocation Solution for MHD Laminar Natural Convection Flow from a Vertical Permeable Flat Plate with Uniform Surface Temperature and Thermal Radiation ⋮ On the multidomain bivariate spectral local linearisation method for solving systems of nonsimilar boundary layer partial differential equations

Cites Work

• Unnamed Item
• The effects of blowing and suction on free convection boundary layers
• Scaling of boundary-layer flows driven by double-diffusive convection
• Combined heat and mass transfer in natural convection flow from a vertical wavy surface
• The nature of vertical natural convection flows resulting from the combined buoyancy effects of thermal and mass diffusion
• Free convection with blowing and suction
• Laminar boundary-layer flow near separation with and without suction

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