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A Mathematical Study of Natural Convection Flow Through a Channel With Non-Singular Kernels: an Application To Transport Phenomena

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2020

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Elsevier

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Abstract

In this manuscript, we have obtained closed form solution using Laplace transform, inversion algorithm and convolution theorem. The study of mass transfer flow of an incompressible fluid is carried out near vertical channel. Recently, new classes of differential operators have been introduced and recognized to be efficient in capturing processes following the decay law and the crossover behaviors. For the study of heat and mass transfer, we applied the newly differential operators say Atangana-Baleanu oABCTHORN and Caputo-Fabrizio oCFTHORN to model such flow. This model for temperature, concentration and velocity gradient is presented in dimensionless form. The obtained solutions have been plotted for various values physical parameters like alpha, D-f, G(m); G(r); S-c and P-r on temperature and velocity profile. Our results suggest that for the variation of time the velocity behavior for CF and ABC are reversible. Finally, an incremental value of prandtl number is observed for decrease in the velocity field which reflects the control of thickness of momentum and enlargement of thermal conductivity. Further, dynamical analysis of fluid with memory effect are efficient for ABC as compared to CF. (C) 2020 The Authors. Published by Elsevier B.V. on behalf of Faculty of Engineering, Alexandria University. This is an open access article under the CC BY license (http://creativecommons.org/licenses/by/ 4.0/).

Description

Saeed, Dr. Syed Tauseef/0000-0002-0971-8364; Saeed, Syed Tauseef/0009-0001-4221-052X

Keywords

Modern Fractional Operator, Inversion Algorithm, Dufour Effect, Mass Transfer, Convolution, Convection Flow

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Citation

Saeed, S.T...et al. (2020). "A Mathematical Study of Natural Convection Flow Through A Channel With Non-Singular Kernels: An Application to Transport Phenomena", Alexandria Engineering Journal.

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32

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59

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4

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2269

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2281
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CrossRef : 34

Scopus : 39

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39

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37

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