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In the above paper the authors treat the boundary layer flow along astationary, vertical, permeable, flat plate within a vertical free stream.Fluid is sucked or injected through the vertical plate. The fluid speciesconcentration at the plate is constant and different from that of the ambientfluid. It is also assumed that the plate is heated by convection from anotherfluid with constant temperature with a constant heat transfer coefficient. Thetemperature and species concentration difference between the plate and theambient fluid creates buoyancy forces and the flow is characterized as mixedconvection. The partial differential equations of the boundary layer flow (Eqs.1-4 in their paper) are transformed and subsequently are solved numericallyusing an implicit finite difference scheme in combination with aquasi-linearization technique. The quasi-linearization technique is aNewton-Raphson method. The results are presented in 12 figures.

Comment on Influence of convective boundary condition on double  diffusive mixed convection from a permeable vertical surface, by P.M. Patil,  E. Momoniat, S. Roy, International Journal of Heat and Mass Transfer, 70  (2014) 313-321