Thermal equilibrium / Isotropic
distribution / Absolute Temperature
This section
explores three interrelated concepts: thermal equilibrium, isotropic velocity distribution,
and absolute temperature. These ideas trace
back to James Clerk Maxwell’s 1860 seminal paper, Illustrations of the
Dynamical Theory of Gases. Part I: On the Motions and Collisions of Perfectly
Elastic Spheres. In essence, Feynman discusses the behavior of an ideal gas in
thermal equilibrium—a state in which molecular velocities are distributed uniformly in all
directions (isotropically), and the system maintains a constant, well-defined
temperature.
1. Thermal equilibrium
“What are the conditions
for equilibrium? We must realize that this is not the only condition over the
long run, but something else must happen more slowly as the true complete
equilibrium corresponding to equal temperatures sets in (Feynman et al.,
1963, p. 39-7).”
To avoid conceptual
ambiguity, Feynman could have more precisely referred to thermal, mechanical,
or thermodynamic equilibrium. Thermal equilibrium occurs
when a system attains a state in which temperature is uniform throughout the
system and no net heat transfer takes place. Mechanical equilibrium requires
the absence of net forces or pressure gradients. Thermodynamic equilibrium implies
that the system is in thermal, mechanical, and chemical equilibrium at the same
time. When Feynman remarks that “something else must happen more slowly,” he
seems to allude to these equilibrium conditions without naming them. While this
omission may make his explanation more intuitive, it is less precise from a
thermodynamic standpoint.
Temperature can be conceptualized
through three fundamental features:
1. Microscopic
Definition: Temperature is directly proportional to the average kinetic energy of
molecules in a system. This provides a molecular-level understanding that links thermodynamic
temperature to the motion of molecules.
2. Zeroth Law of
thermodynamics: If system A is in thermal equilibrium with system B, and system B is
in thermal equilibrium with system C, then systems A and C are also in
equilibrium. This establishes temperature as a transitive and measurable
property that can be used to compare the thermal conditions of different
systems.
3. Temporal
Stability: Once a system reaches thermal equilibrium, its temperature remains stable
over time, distinguishing it from transient conditions and making it a reliable
thermodynamic variable.
These three aspects—average
kinetic energy, transitive property, and temporal stability—provide an
operational basis for defining and measuring temperature.
2. Isotropic Distribution
“Now then, what is the
distribution resulting from this? From our previous argument we conclude this:
that at equilibrium, all directions for w are
equally likely, relative to the direction of the motion of the CM. There
will be no particular correlation, in the end, between the direction of the
motion of the relative velocity and that of the motion of the CM (Feynman et
al., 1963, p. 39-8).”
Maxwell’s
assumption of an isotropic velocity distribution implies that, in thermal
equilibrium, molecular motion has no preferred direction. However, in reality, gravity
causes gas molecules to follow parabolic trajectories between collisions
rather than idealized straight lines. Specifically, upward-moving molecules
lose kinetic energy as they ascend, whereas downward-moving molecules gain kinetic
energy as they descend, leading to a directional asymmetry in the velocity
distribution. Thus, Feynman’s explanation, which assumes molecular motion is
equally probable in all directions, applies to an idealized, force-free system.
This approximation is valid only locally, in small regions where
gravitational effects are negligible. Across larger vertical distances,
however, gravity becomes significant and breaks the isotropy of the velocity
distribution by imposing a preferred downward direction.
Note on
Distributions: In The Feynman Lectures on Physics (Section 40-1),
the Boltzmann distribution is derived to describe the spatial
distribution of molecules under the influence of gravity. This distribution
predicts an exponential decrease in particle number density with increasing
altitude. Crucially, this differs from the Maxwell-Boltzmann
distribution, which characterizes the probability distribution of molecular
speeds in a system at thermal equilibrium in the absence of external
forces.
Footnote: “This
argument, which was the one used by Maxwell, involves some subtleties.
Although the conclusion is correct, the result does not follow purely from
the considerations of symmetry that we used before, since, by going to a
reference frame moving through the gas, we may find a distorted velocity
distribution. We have not found a simple proof of this result (Feynman
et al., 1963, p. 39-8).”
In his 1860
derivation of the molecular speed distribution for an ideal gas, Maxwell
assumed that the velocity components are statistically independent and that all
directions of rebound are equally likely. These assumptions lead to some criticisms,
e.g., Richet (2001) argues that “the assumed isotropy of the gas does not
necessarily imply the statistical independence of the variables along different
directions of space” (p. 319). A more fundamental challenge arises from
relativistic physics: Walstad (2013) points out that in a relativistic gas,
kinetic energy cannot be decomposed into independent functions of the Cartesian
velocity components. As a result, the probability distribution for one
component of velocity depends inherently on the others. Interestingly, Walstad concludes
that Maxwell’s derivation lacks even pedagogical validity. However, Maxwell’s molecular
speed distribution is also recognized as the first statistical law proposed in
physics. Thus, we need not expect Maxwell’s derivation to be fully rigorous by
today’s standards—it was a pioneering insight rather than a formal proof.
Footnote: “Although
the conclusion is correct, the result does not follow purely from the
considerations of symmetry that we used before, since, by going to a reference
frame moving through the gas, we may find a distorted velocity distribution
(Feynman et al., 1963, p. 39-8).”
The distorted
velocity distributions in different reference frames can be understood through
a relativistic analogy. Just as electric field lines change direction under a
Lorentz transformation (See figure below), molecular velocity distributions
appear anisotropic when viewed from a moving reference frame—though the
transformation rules governing each are fundamentally different. This asymmetry is a kinematic
effect—it reflects the motion of the observer rather than the intrinsic property
of the gas. In the lab frame (where thermal equilibrium is defined), Maxwell’s assumption
of isotropy remains valid. However, while the average molecular momentum remains approximately zero in
directions perpendicular to the observer’s motion, a non-zero net momentum
emerges in the direction opposite to that motion. This illustrates how velocity
distributions are frame-dependent, and how apparent anisotropies can emerge
solely from changes in the observer’s reference frame.
3. Absolute Temperature
“We may arbitrarily define the
scale of temperature so that the mean energy is linearly proportional to the
temperature. The best way to do it would be to call the mean energy itself ‘the
temperature’…… we use a constant conversion factor between the energy of a
molecule and a degree of absolute temperature called a degree Kelvin
(Feynman et al, 1963, p. 39-10).”
The Absolute
Nature—and Arbitrary Aspects—of Temperature
Physicists often emphasize
that absolute temperature is not an arbitrarily construct, but is grounded in fundamental
physical principles. There are at least three possible arguments: (1) Universal
minimum: The Kelvin scale’s zero point (absolute zero) represents a
theoretical limit where all thermal motion ceases, in accordance with the classical
laws. (2) Fundamental constant: Unlike empirical scales (e.g., Celsius
or Fahrenheit), the Kelvin is defined via the Boltzmann constant (k), linking
temperature directly to energy and separating it from material-dependent
references like the boiling point of water. (3) Universal standard: Absolute
temperature is linearly proportional to the average kinetic energy of the
particles, making it a universal standard and objective measure applicable from real
gases to cosmological observations. Thus, the Kelvin scale is often called
the absolute (not arbitrary) temperature scale, a framework based on
physical principles.
Arbitrary
Conventions Remain
Despite its
foundation in physical principles, the so-called absolute temperature is
not entirely free from human-defined conventions. Firstly, the size of the Kelvin
unit was historically chosen to match the Celsius degree for practical
continuity. Secondly, the Kelvin scale is defined via the Boltzmann constant (k), which
connects temperature to energy through the expression kT. However, energy
is measured in joules—a unit based on human-defined standards (e.g., the
kilogram and second). Thirdly, the choice to define temperature as linearly
proportional to average kinetic energy is a convention, agreed upon for
consistency across physical theories. In summary, although the Kelvin scale
is grounded in physical principles, its construction still depends on
human-defined conventions—such as unit choices, scaling, and dimensional system.
This interplay between the objective foundation of temperature and its
conventional elements reflects a deeper philosophical question, which is
closely associated with conventionalism in the philosophy of science.
Review questions:
1. Should the term
“thermal equilibrium” be used in introductory discussions?
2. How would you
explain the directions of molecules after collisions in different frames?
3. To what extent
is the Kelvin scale (or absolute temperature) arbitrarily defined?
The Moral of the
lesson:
Scientific
conventions—such as systems of measurement—are built on collective agreement
rather than absolute truths. Similarly, societal norms like laws, ethics, and
customs are developed by consensual agreement instead of universal morality.
This highlights the importance of dialogue, cooperation, and shared
understanding in building a functional and adaptable society.
Fun Facts:
Why did SARS virus struggle
to spread in tropical regions? Research suggests that temperature and humidity
accelerate the breakdown of the virus (Biryukov et al, 2020; Chan
et al, 2011). In contrast, cooler and drier conditions—such as Hong Kong’s
springtime or air-conditioned environments—allow the virus to survive longer,
increasing transmission risk. This may help explain why countries like
Indonesia, Malaysia, and Singapore experienced fewer major outbreaks: their
warm, humid climates acted as a natural barrier. On the other hand, sunlight
may also help, but its antiviral power comes not from warmth, but from
ultraviolet (UV) radiation.
References:
Biryukov, J.,
Boydston, J. A., Dunning, R. A., Yeager, J. J., Wood, S., Reese, A. L., ...
& Altamura, L. A. (2020). Increasing temperature and relative humidity
accelerates inactivation of SARS-CoV-2 on surfaces. MSphere, 5(4),
10-1128.
Chan, K. H.,
Peiris, J. M., Lam, S. Y., Poon, L. L. M., Yuen, K. Y., & Seto, W. H.
(2011). The effects of temperature and relative humidity on the viability of
the SARS coronavirus. Advances in virology, 2011(1),
734690.
Feynman,
R. P., Leighton, R. B., & Sands, M. (1963). The Feynman Lectures on
Physics, Vol I: Mainly
mechanics, radiation, and heat. Reading, MA: Addison-Wesley.
Maxwell, J.C.
(1860). Illustrations of the dynamical theory of gases. Part I. On the
motions and collisions of perfectly elastic spheres. The London, Edinburgh,
and Dublin Philosophical Magazine and Journal of Science, 4th Series,
vol.19, pp.19–32.
Richet, P. (2001). The
Physical Basis of Thermodynamics: With Applications to Chemistry. New York:
Kluwer Academic/Plenum.
Resnick, R.
(1991). Introduction to special relativity. John Wiley & Sons.
Walstad, A. (2013).
On deriving the Maxwellian velocity distribution. American Journal of
Physics, 81(7), 555-557.