After many years (from Newton's and Euler's time, to mid 19th century) of confusion and research, we arrievd at a set of postulates ( Stoke's Principle)
This is similar to an expansion of a function in polynomial
Here ,
,
and
From 2:(homogeneity)
From 5: (if at rest
is hydrostatic)
for a fluid at rest , then
for Newotonian fluids
Here are coefficients for viscous fluid model, in this case it has 81 terms. For example
Since
reduced to 36 terms
From 4: (Isotropic) For isotropic tensor of 4th order we may write
then
Here ,
and
are three scalar coefficients.
Since
,
, then
therfore, the stress tensor becomes
Here
is the rate of strain tensor. In components the stresses are
It should be remarked that the model coefficients are reduced from 81 to 2. They are the two viscosities
the first viscosity and
the second viscosity.
From 5:(Stoke's hypothesis)
pure dilatation. The average of normal stresses is
Stoke assumed that . Therefore
or
The derivation of Navier-Stokes' equations is now completed. In Cartesina tensor notation we have
where
is known as the stress deviator or
Now we can write the equations of motion as Continuity equation:
Momentum Equation:
It should be marked that is an unknown coefficient known as viscosity. It is determined from
experiment.