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Residual power series method for solving nonlinear reaction-diffusion-convection problems
Author(s) -
M. S. Khader,
Mahmoud H. DarAssi
Publication year - 2020
Publication title -
boletim da sociedade paranaense de matemática
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.347
H-Index - 15
eISSN - 2175-1188
pISSN - 0037-8712
DOI - 10.5269/bspm.41741
Subject(s) - residual , series (stratigraphy) , homotopy analysis method , power series , nonlinear system , homotopy perturbation method , mathematics , diffusion , convection , homotopy , mathematical analysis , mechanics , physics , algorithm , thermodynamics , geology , paleontology , quantum mechanics , pure mathematics
where u = u(x, t) is an unknown function, and the arbitrary smooth functions a(u), b(u) and c(u) denote the diffusion term, the convection term and the reaction term respectively. The reaction diffusion convection equations are widely used in many areas in science such as biology modeling, physics, chemistry, astrophysics, medicine and engineering. For example, heat conduction [4], [5] and [20], haemodynamics [9], [23] and [22], dynamics of blood coagulation [6] and [25], cardiac arrhythmias [8] and [24] and atherosclerosis [16] and [15]. The following equation is a special case of the reaction diffusion convection equations, the Murray equation [18] and [19]

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