M
M. S. Alhothuali
Researcher at King Abdulaziz University
Publications - 12
Citations - 403
M. S. Alhothuali is an academic researcher from King Abdulaziz University. The author has contributed to research in topics: Partial differential equation & Nusselt number. The author has an hindex of 9, co-authored 12 publications receiving 338 citations.
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Mixed Convection Stagnation Point Flow of Casson Fluid with Convective Boundary Conditions
TL;DR: In this paper, the mixed convection stagnation-point flow of an incompressible non-Newtonian fluid over a stretching sheet under convective boundary conditions is investigated, and the resulting partial differential equations are converted into the ordinary differential equations by the suitable transformations.
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Three-dimensional flow of Oldroyd-B fluid over surface with convective boundary conditions
TL;DR: In this paper, a three-dimensional flow of an Oldroyd-B fluid over a stretching surface with convective boundary conditions was studied. The authors presented the problem formulation using the conservation laws of mass, momentum, and energy.
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Existence of solutions for integro-differential equations of fractional order with nonlocal three-point fractional boundary conditions
TL;DR: In this article, the existence of solutions for Riemann-Liouville type integro-differential equations of fractional order with nonlocal three-point fractional boundary conditions via Sadovskii's fixed point theorem for condensing maps was studied.
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Influence of induced magnetic field and heat transfer on peristaltic transport of a Carreau fluid
Tasawar Hayat,Tasawar Hayat,Najma Saleem,Saleem Asghar,Saleem Asghar,M. S. Alhothuali,Adnan Alhomaidan +6 more
TL;DR: In this paper, the effect of an induced magnetic field on peristaltic flow of an incompressible Carreau fluid in an asymmetric channel is analyzed and perturbation solution to equations under long wavelength approximation is derived in terms of small Weissenberg number.
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On a time fractional reaction diffusion equation
TL;DR: Under some conditions on the initial data, it is shown that solutions may experience blow-up in a finite time, however, for realistic initial conditions, solutions are global in time.