Abstract
1. In this paper I have followed the method given in my paper “On the Dynamical Theory of Gases” (Phil. Trans., 1867, p. 49). I have shown that when inequalities of temperature exist in a gas, the pressure it a given point is not the same in all directions, and that the difference between the maximum and the minimum pressure at a point may be of considerable magnitude when the density of the gas is small enough, and when the inequalities of temperature are produced by small; solid bodies at a higher or lower temperature than the vessel containing the gas. 2. The nature of this stress may be thus defined: let the distance from the given point, measured in a given direction, be denoted by
h
, and the absolute temperature by
θ
; then the space-variation of the temperature for a point moving along this line will be denoted by
dθ
/
dh
, and the space-variation of this quantity along the same line by
d
2
θ
/
dh
2
. There is in general a particular direction of the line
h
, for which
d
2
θ
/
dh
2
is a maximum, another for which it is a minimum, and a third for which it is a maximum-minimum. These three directions are at right angles to each other, and are the axes of principal stress at the given point; and the part of the stress arising from inequalities of temperature is in each of these principal axes a pressure equal to— 3
μ
2
/
ρθ
d
2
θ
/
dh
2
, where
μ
is the coefficient of viscosity,
ρ
the density, and
θ
the absolute temperature.
Subject
General Earth and Planetary Sciences,General Environmental Science
Cited by
315 articles.
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