The shear viscosity of a system measures is resistance to flow. A simple flow field can be established in a system by placing it between two plates and then pulling the plates apart in opposite directions. Such a force is called a shear force, and the rate at which the plates are pulled apart is the shear rate. A set of microscopic equations of motion for generating shear flow is
where
is a parameter known as the shear rate.
These equations have the conserved quantity
The physical picture of this dynamical system corresponds to the presence of
a velocity flow field
shown in the figure.
The flow field points in the
direction and increases with
increasing y-value. Thus, layers of a fluid, for example, will slow
past each other, creating an anisotropy in the system. From the
conserved quantity, one can see that the momentum of a particle is
the value of
plus the contribution from the field evaluated
at the position of the particle
and
in equilibrium. Here, V is the volume of the
system. By analogy, one can write down an estimator for the
pressure tensor
:
and
where
is a unit vector in the
direction,
. This (nine-component) pressure tensor gives information about
spatial anisotropies in the system that give rise to off-diagonal pressure
tensor components. The isotropic pressure can be recovered from
which is just 1/3 of the trace of the pressure tensor. While most systems
have diagonal pressure tensors due to spatial isotropy, the application of
a shear force according to the above scheme gives rise to a nonzero value
for the xy component of the pressure tensor
. In fact,
is related to the velocity flow field by a relation of the
form
where the coefficient
is known as the shear viscosity and
is an example of a transport coefficient.
Solving for
we find
where
is the nonequilibrium average of
the pressure tensor estimator using the above dynamical equations of motion.
Let us apply the linear response formula to the calculation of the nonequilibrium average of the xy component of the pressure tensor. We make the following identifications:
Thus, the dissipative flux
becomes
According to the linear response formula,
so that the shear viscosity becomes
Recall that
means average of a canonical distribution
with
. It is straightforward to show that
for an equilibrium canonical distribution function. Finally, taking the
limit that
in the above expression gives the result
which is a relation between a transport coefficient, in this case, the shear viscosity coefficient, and the integral of an equilibrium time correlation function. Relations of this type are known as Green-Kubo relations. Thus, we have expressed a new kind of thermodynamic quantity to an equilibrium time correlation function, which, in this case, is an autocorrelation function of the xy component of the pressure tensor.