Buch, Englisch, 220 Seiten, Format (B × H): 170 mm x 240 mm, Gewicht: 510 g
Advances in Nonlinear Heat Transfer in Fluids and Solids
Buch, Englisch, 220 Seiten, Format (B × H): 170 mm x 240 mm, Gewicht: 510 g
ISBN: 978-3-0357-1282-7
Verlag: Trans Tech Publications
Autoren/Hrsg.
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Weitere Infos & Material
Preface
Thermal Conductivity Impact on Thermal Stability of Reactive Materials
Performance Analysis of Magnetite Nano-Suspension Based Porous Slider Bearing with Varying Inclination and Slip Parameter
Impact of Chemical Reaction on Marangoni Boundary Layer Flow of a Casson Nano Liquid in the Presence of Uniform Heat Source Sink
Phenomenon of Radiation and Viscous Dissipation on Casson Nanoliquid Flow Past a Moving Melting Surface
Radiation Absorption and Viscous-Dissipation on MHD Flow of Casson Fluid over a Vertical Plate Filled with Porous Layers
Effects of Nonlinear Thermal Radiation and Thermo-Diffusion on MHD Carreau Fluid Flow Past a Stretching Surface with Slip
Non-Uniform Heat Source/Sink Effect on Liquid Film Flow of Jeffrey Nanofluid over a Stretching Sheet
Nonlinear Thermal Convection in Jeffrey Liquid Flow with Cross Diffusion Effects Past a Stretched Surface
Effects of Oil-Based Nanofluid on a Stretching Surface with Variable Suction and Thermal Conductivity
Radiative MHD Stagnation-Point Flow with Heat Transfer Past a Permeable Stretching/Shrinking Sheet in a Porous Medium
Analysis of Radiative Magneto-Nanofluid over an Accelerated Plate in a Rotating Medium with Hall Effects
Unsteady MHD Natural Convective Flow of a Rotating Fluid over an Infinite Vertical Plate due to Oscillatory Movement of the Free-Stream with Hall and Ion-Slip Currents
Thermal Radiation, Joule Heating and Hall Effects on Mixed Convective Navier Slip Flow in a Channel with Convective Heating
MHD Stagnation Point Flow over Exponentially Stretching Sheet with Exponentially Moving Free-Stream, Viscous Dissipation, Thermal Radiation and Non-Uniform Heat Source/Sink
An Integral Treatment for Dissipative Boundary Layer Flow along a Radiating Vertical Surface by Natural Convection in a Porous Medium