Application of the Laplace Transform to the Solution of the Boundary Layer Equations. II Magneto-Hydrodynamic Blasius Problem

抄録

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.