Abstract

This paper determines a class of exact solutions for plane steady motion of incompressible fluids of variable viscosity with body force term in the Navier-Stokes equations. The class consists of stream function  characterized by equation , in polar coordinates ,  where ,  and  are continuously differentiable functions, derivative of  is non-zero but double derivative of  is zero. We find exact solutions, for a suitable component of body force, considering two cases based on velocity profile. The first case fixes both the functions ,  and provides viscosity as function of temperature. Where as the second case fixes the function , leaves  arbitrary and provides viscosity and temperature for the arbitrary function . In both the cases, we can create infinite set of expressions for streamlines, viscosity function, generalized energy function and temperature distribution in the presence of body force. Â

Highlights

  • For the study of motion of a fluid element, we consider its momentum, the energy and conservation of mass equations

  • The complexity for exact solutions increases when we add more terms to the right-hand side of Navier-Stokes equations like body force, as it appears in geophysical fluid dynamics (GFD) due to the earth’s rotation and in magnetohydrodynamic (MHD) where the magnetic field induces currents in a moving fluid for creating force on the fluid [1,2,3]

  • For the exact solutions of these basic equations with and without body force, we find some appropriate dimension analysis method and coordinates transformation techniques in the available literature

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Summary

Introduction

For the study of motion of a fluid element, we consider its momentum, the energy and conservation of mass equations. We are using coordinate transformations technique on non-dimensional equations for determining the exact solutions in this communication. In order to determine the solution of the flow equations (15-16), we follow [4,5,6,7] and form a compatibility equation applying the natural integrability condition Lr = L r on the function L. We have given the resulting fundamental equations in Martin’s coordinates system ( , ) in [5,6,7] considering a common point P(x, y) on the curves = const. Once a solution of this equation (24) is determined, the energy function L and temperature distribution T are obtained from equations (15-16) and (17) respectively, the viscosity is obtained either from equation (19) or (20), the pressure p from equation (10) and velocity components u , v from (5).

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