The kinetic energy of a fluid occupying a region $\Omega \subset \mathbb{R}^3$ is given by
$$T = \frac{1}{2}\int_\Omega |v(x)|^2 dx.$$
I am looking for some physical intuition on where the above comes from given that the classical definition of kinetic energy is $T = \frac{1}{2}mv^2$. More specifically, I have two questions:
- What happened to the mass $m$?
- Why are we integrating?
My best guess is that the mass is taken to instead be a density, $\rho$, and we further assume that $\rho = 1$ (why is this justified?). In which case, for an infinitesimal amount of fluid, we find its average velocity $v(x)$ in that region and multiply the volume to get something like $T = \frac{1}{2}mv^2$. Repeating this over all infinitesimally small areas in $\Omega$ and summing them up amounts to taking the integral. If this is indeed correct, then my question reduces to why is taking $\rho = 1$ justified?