Abstract
The results of an earlier paper on the behavior of the boundary layer at an axisymmetric stagnation with hydrogen injection into a hot external airstream are extended to span the entire range from essentially frozen to essentially equilibrium flow. This extension is made possible by the employment of finite difference methods; the accurate treatment of the boundary conditions at “infinity,” the differencing technique employed and the formulation resulting in block tri-diagonal matrices are slight variants in the present work.

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