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@wikipedia


Mathematical form of Mass Conservation for continuum body:

Integral formDifferential form
(1) \frac{d}{dt} \iiint_\Omega \rho \, dV = \dot m = \frac{dm_\Omega}{dt}
(2) \frac{\partial \rho}{\partial t} + \nabla (\rho \, {\bf u}) = \frac{dm (t, {\bf r})}{dt}

where

t

time

{\bf r }

position vector

\rho(t, {\bf r})

continuum body spatial density distribution

{\bf u}(t, {\bf r)

continuum body spatial velocity distribution

\dot m = \frac{dm}{dt}

mass generation rate



For the stationary fluid flow:

(3) \frac{\partial \rho}{\partial t} = 0 \rightarrow \nabla (\rho \, {\bf u}) = 0


See also


Natural Science / Physics / Mechanics / Continuum mechanics 

[ Mass Conservation ]




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