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1 Introduction. - MIT

1 Introduction. - MIT

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are called boundary layers. Within such layers the uid velocity changes rapidly from zero to its main-stream value, and this may imply a steep gradient of shearing stress; as a consequence, not all the viscous terms in the equation of motion will be negligible, even though the viscosity, which they contain as a factor, is itself very small.

  Early, Boundary, Boundary layer

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