Eliminating mass density $ \rho $ from equation of state

The equation of state (3) involves three physical quantities, namely $ \rho $, $ p$, and $ \mathbf{u}$. It turns out that the continuity equation can be used in the equation to eliminate $ \rho $. The equation of state

$\displaystyle \frac{d}{d t} (p \rho^{- \gamma}) = 0,$ (13)

can be written as

$\displaystyle \frac{d p}{d t} \rho^{- \gamma} - \gamma \rho^{- (\gamma + 1)} p \frac{d \rho}{d t} = 0,$ (14)

which simplifies to

$\displaystyle \frac{d p}{d t} = \gamma \frac{p}{\rho} \frac{d \rho}{d t}$ (15)

Expand the total derivative, giving

$\displaystyle \frac{\partial p}{\partial t} +\mathbf{u} \cdot \nabla p = \gamma...
...} \left( \frac{\partial \rho}{\partial t} +\mathbf{u} \cdot \nabla \rho \right)$ (16)

Using the mass continuity equation to eliminate $ \rho $ in the above equation gives

$\displaystyle \frac{\partial p}{\partial t} = - \gamma p \nabla \cdot \mathbf{u}-\mathbf{u} \cdot \nabla p.$ (17)

This equation governs the time evolution of the pressure. A way to memorize this equation is that, if $ \gamma = 1$, the equation will take the same form as a continuity equation, i.e.,

$\displaystyle \frac{\partial p}{\partial t} = - \nabla \cdot (p\mathbf{u}) .$ (18)

yj 2015-09-04