Abstract
The flow of an electrically conducting incompressible fluid due to buoyancy effects of thermal and mass diffusion past a finite vertical porous plate with constant suction was investigated in the presence of uniform transverse magnetic field. The problem has been solved for velocity, temperature and concentration profiles. The equations governing the flow are solved numerically using finite difference method for various values of Grashof parameter ranging from 0 to - 1. The results obtained are then presented using tables and graphs. It was noted that a decrease in Grashof parameter leads to an increase in primary, secondary, temperature and concentration profile.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callMore From: International Journal of Pure and Apllied Mathematics
Disclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
