Abstract
The boundary layer equations for the magneto-hydrodynamic version of the Blasius problem are reduced to the system of simultaneous non-linear ordinary differential equations. These equations are solved by the Laplace transform method. The obtained solution, which has a finite radius of convergence is extended by using the steepest descent technique.
Original language | English |
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Pages (from-to) | 888-891 |
Number of pages | 4 |
Journal | Journal of the Physical Society of Japan |
Volume | 25 |
Issue number | 3 |
DOIs | |
State | Published - 1 Jan 1968 |
Externally published | Yes |
ASJC Scopus subject areas
- General Physics and Astronomy