Application of the laplace transform to the solution of the boundary layer equations. II Magneto-hydrodynamic blasius problem

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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 languageEnglish
Pages (from-to)888-891
Number of pages4
JournalJournal of the Physical Society of Japan
Volume25
Issue number3
DOIs
StatePublished - 1 Jan 1968
Externally publishedYes

ASJC Scopus subject areas

  • General Physics and Astronomy

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