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In the above paper the author treats the boundary layer flow along a verticalflat plate, immersed in a Darcy Brinkman Forchheimer porous medium. Theporosity and the permeability of the porous medium are variable across theboundary layer. In addition a magnetic field with constant strength is appliednormal to the plate. The fluid temperature at the plate is constant anddifferent from that of the ambient fluid. This temperature difference creates abuoyancy force and the flow is characterized as mixed convection. The partialdifferential equations of the boundary layer flow are transformed into ordinarydifferential equations and subsequently are solved with the Runge-KuttaFehlberg method. The results are presented in two tables and 11 figures.

Comment on Magnetohydrodynamic non-Darcy mixed convection heat transfer  from a vertical heated plate embedded in a porous medium with variable  porosity, by Dulal Pal