Abstract

The objective of this article is to present the dynamics of an Upper Convected Maxwell (UCM) fluid flow with heat and mass transfer over a melting surface. The influence of melting heat transfer, thermal and solutal stratification are properly accounted for by modifying the classical boundary conditions of temperature and concentration respectively. It is assumed that the ratio of inertia forces to viscous forces is high enough for boundary layer approximation to be valid. The corresponding influence of exponential space dependent internal heat source on viscosity and thermal conductivity of UCM is properly considered. The dynamic viscosity and thermal conductivity of UCM are temperature dependent. Classical temperature dependent viscosity and thermal conductivity models were modified to suit the case of both melting heat transfer and thermal stratification. The governing non-linear partial differential equations describing the problem are reduced to a system of nonlinear ordinary differential equations using similarity transformations and completed the solution numerically using the Runge-Kutta method along with shooting technique. For accurate and correct analysis of the effect of variable viscosity on fluid flow in which (Tw or Tm) T∞ , the mathematical models of variable viscosity and thermal conductivity must be modified.

Highlights

  • Mass transfer can be described as the movement of mass through a fluid-fluid interface or a flu-How to cite this paper: Adegbie, K.S., Omowaye, A.J., Disu, A.B. and Animasaun, I.L. (2015) Heat and Mass Transfer of Upper Convected Maxwell Fluid Flow with Variable Thermo-Physical Properties over a Horizontal Melting Surface

  • The three kinds of fluxes in relation to mass transfer have been explained in Asano [1]; Mass flux can be expressed as the addition of diffusional flux and convective mass flux

  • The Upper Convected Maxwell model can be described as the generalization of the Maxwell material for the case of large deformation using the upperconvected time derivative which is the rate of change of some tensor properties of a small parcel of fluid that is written in the coordinate system stretching with the fluid

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Summary

Introduction

Mass transfer can be described as the movement of mass (material) through a fluid-fluid interface or a flu-How to cite this paper: Adegbie, K.S., Omowaye, A.J., Disu, A.B. and Animasaun, I.L. (2015) Heat and Mass Transfer of Upper Convected Maxwell Fluid Flow with Variable Thermo-Physical Properties over a Horizontal Melting Surface. The dynamics of material having the properties of elasticity and viscosity when undergoing deformation is a fundamental topic in fluid dynamics. This kind of material referred to as “Maxwell fluid” has attracted the attention of many researchers due to its wide industrial and technical applications. The Upper Convected Maxwell model can be described as the generalization of the Maxwell material for the case of large deformation using the upperconvected time derivative ( known as Oldyrold derivative) which is the rate of change of some tensor properties of a small parcel of fluid that is written in the coordinate system stretching with the fluid. It is worth noticing that mathematical model of Upper Convected Maxwell has been described (or defined) as a function of stress tensor, relaxation time, upper convected time derivative of stress tensor, fluid velocity, material viscosity at steady simple shear and tensor of the deformation rate

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