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A. Ridha
Researcher at University of Caen Lower Normandy
Publications - 12
Citations - 207
A. Ridha is an academic researcher from University of Caen Lower Normandy. The author has contributed to research in topics: Laminar flow & Boundary layer. The author has an hindex of 6, co-authored 12 publications receiving 196 citations. Previous affiliations of A. Ridha include Pierre-and-Marie-Curie University & University College London.
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Aiding flows non-unique similarity solutions of mixed-convection boundary-layer equations
TL;DR: In this article, the similarity equations for mixed-convection boundary-layer flow past a wedge having one of its surfaces parallel to the horizontal are derived for the latter surface.
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On the dual solutions associated with boundary-layer equations in a corner
TL;DR: In this paper, the dual solutions of two coupled third degree non-linear ordinary differential equations associated with the incompressible viscous laminar flow along a corner are considered and it is shown (through the numerical solution) that dual solutions occur in the interval βbβββ1.1211 for the Falkner-Skan parameter β with the bifurcation taking place at the regular turning point βb.
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Flow in Streamwise Corners of Arbitrary Angle
W. H. Barclay,A. Ridha +1 more
TL;DR: Rubin et al. as discussed by the authors presented a new formulation of the problem posed by the corner of arbitrary angle, and the result is a set of equations that, when specialized to meet the rectangular corner situation, coincide with those obtained by Rubin.
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Three-dimensional mixed convection laminar boundary-layer near a plane of symmetry
TL;DR: In this article, the mixed convection boundary-layer flow in the vicinity of the median plane of symmetry of a finite span wedge is considered and the similarity equations are derived for situations where one of the wedge surfaces is kept vertical.
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Flow along streamwise corners revisited
TL;DR: In this article, the authors investigated the three-dimensional laminar incompressible steady flow along a corner formed by joining two similar quarter-infinite unswept wedges along a side-edge.