1958
DOI: 10.21236/ad0202403
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Normal Shock (Rankine-Hugoniot) Relations for Various Altitudes for Sea Level to 300,00 Feet

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“…The lower shaded zone in Fig. 1 was obtained from normal shock calculations for air in thermodynamic equilibrium 8 and a viscosity which varied as T s 112 . Since radiative effects on the shock structure were also neglected, the extent of this zone is highly qualitative.…”
Section: Flow Regimesmentioning
confidence: 99%
“…The lower shaded zone in Fig. 1 was obtained from normal shock calculations for air in thermodynamic equilibrium 8 and a viscosity which varied as T s 112 . Since radiative effects on the shock structure were also neglected, the extent of this zone is highly qualitative.…”
Section: Flow Regimesmentioning
confidence: 99%