In aerodynamics, the normal shock tables are a series of tabulated data listing the various properties before and after the occurrence of a normal shock wave. With a given upstream Mach number, the post-shock Mach number can be calculated along with the pressure, density, temperature, and stagnation pressure ratios. Such tables are useful since the equations used to calculate the properties after a normal shock are cumbersome. The tables below have been calculated using a heat capacity ratio, γ {\displaystyle \gamma } , equal to 1.4. The upstream Mach number, M 1 {\displaystyle M_{1}} , begins at 1 and ends at 5. Although the tables could be extended over any range of Mach numbers, stopping at Mach 5 is typical since assuming γ {\displaystyle \gamma } to be 1.4 over the entire Mach number range leads to errors over 10% beyond Mach 5.
Normal shock table equations Given an upstream Mach number, M 1 {\displaystyle M_{1}} , and the ratio of specific heats, γ {\displaystyle \gamma } , the post normal shock Mach number, M 2 {\displaystyle M_{2}} , can be calculated using the equation below.
M 2 = M 1 2 ( γ − 1 ) + 2 2 γ M 1 2 − ( γ − 1 ) {\displaystyle M_{2}={\sqrt {\frac {M_{1}^{2}\left(\gamma -1\right)+2}{2\gamma M_{1}^{2}-\left(\gamma -1\right)}}}}
The next equation shows the relationship between the post normal shock pressure, p 2 {\displaystyle p_{2}} , and the upstream ambient pressure, p 1 {\displaystyle p_{1}} .
p 2 p 1 = 2 γ M 1 2 γ + 1 − γ − 1 γ + 1 {\displaystyle {\frac {p_{2}}{p_{1}}}={\frac {2\gamma M_{1}^{2}}{\gamma +1}}-{\frac {\gamma -1}{\gamma +1}}}
The relationship between the post normal shock density, ρ 2 {\displaystyle \rho _{2}} , and the upstream ambient density, ρ 1 {\displaystyle \rho _{1}} is shown next in the tables.
ρ 2 ρ 1 = ( γ + 1 ) M 1 2 ( γ − 1 ) M 1 2 + 2 {\displaystyle {\frac {\rho _{2}}{\rho _{1}}}={\frac {\left(\gamma +1\right)M_{1}^{2}}{\left(\gamma -1\right)M_{1}^{2}+2}}}
Next, the equation below shows the relationship between the post normal shock temperature, T 2 {\displaystyle T_{2}} , and the upstream ambient temperature, T 1 {\displaystyle T_{1}} .
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