4
1. Introduction
The pressure, , defined as the average force per unit area acting on a surface of area ,
is one of the primary state variables, together with the temperature, , and composition, that
determine the thermodynamic properties of a homogeneous system of molecules at equilibrium.
In such a system the average force and the pressure are the same in all directions, is a scalar, and
is well-defined even at the micro-scale. Statistical mechanics informs us that , where
superscript indicates the contribution due to the kinetic energy of the molecules, and indicates
the configurational contribution, i.e. that from the intermolecular forces and any external field. For
condensed phases the configurational contribution to is usually dominant, especially at low
temperatures. For a perfect gas at equilibrium in the absence of an external field, or a real
equilibrium gas at low enough density that the influence of intermolecular forces can be neglected,
the configurational contribution is negligible, and , where is the number
density at position and is the Boltzmann constant. For such a gas this relation holds even
when the gas is non-uniform in density or composition, as long as the concept of a local average
density, , is valid.
For more general situations, for example an inhomogeneous dense fluid, a nanoscale fluid
or solid, or a non-equilibrium system, the pressure is a second-order tensor, depending on the
direction of both the force and of the surface it acts on. In general, has 9 components , where
is the force per unit area in the -direction acting on a surface element normal to the -
direction. These components depend on position, , and for non-equilibrium systems they will also
depend on time, . Off-diagonal components are the shear pressures (shear stress) and the diagonal
components are the direct pressures. In some specific types of systems, the number of non-
vanishing components of may be less than 9. For an inhomogeneous fluid that is at equilibrium
and not under strain, for example, the off-diagonal components vanish and there are only 3 non-
vanishing components. Also, the condition of mechanical (hydrostatic) equilibrium (the average
rate of change of linear momentum vanishes) often provides relations between the remaining non-
vanishing components.
A difficulty in many applications is that the local (microscopic) pressure tensor at some
point is not uniquely defined in non-equilibrium systems or in equilibrium ones that are
inhomogeneous. Although the kinetic contribution, , is well-defined, as noted above, the
configurational part, is not, because the intermolecular forces themselves are non-local. Thus,
while the force between molecules and , located at positions and , is well defined in general,
there is no well-defined way to assign a contribution to the force acting on a surface element at
some position . This arbitrariness in the force acting across the surface element seems to have
first been stated explicitly by Irving and Kirkwood in 1950.1 There they stated the matter
succinctly:
“…all definitions (of the configurational pressure tensor) must have this in common – that the
stress between a pair of molecules be concentrated near the line of centers. When averaging over
a domain large compared with the range of intermolecular force, these differences are washed
out, and the ambiguity remaining in the macroscopic stress tensor is of negligible order.”
This point was discussed in a footnote to an appendix to Irving & Kirkwood’s paper, and so was
not noticed widely at the time. It was of little consequence to these authors, who were primarily