Force per unit area / Energy per unit volume / Quasi-static
adiabatic compression
In this section,
Feynman relates the pressure of a gas to force per unit area, energy per unit
volume, and quasi-static adiabatic compression. Most of these concepts trace back to Clausius’ (1857) paper, “On
the Nature of the Motion which we call Heat.” In that seminal work, Clausius
laid the foundation for the kinetic theory of gases, linking macroscopic
properties like pressure and temperature to the microscopic motion of molecules. However,
Feynman’s discussion goes beyond a basic explanation of gas pressure and
includes a derivation of the adiabatic law.
1. Force per unit area
“We
define the pressure, then, as equal to the force that we have to apply on a
piston, divided by the area of the piston: P = F/A……. So we see that the force,
which we already have said is the pressure times the area, is equal to the
momentum per second delivered to the piston by the colliding molecules (Feynman
et al., 1963, p. 39-3).”
The pressure of a
gas is a macroscopic property that arises from the collective motion of
microscopic particles. Its physical origin can be understood from three perspectives:
1. Macroscopic
definition: Pressure (P) is defined as the force (F) exerted
perpendicularly on a surface, divided by the area (A) of that surface: P
= F / A.
2. Microscopic
Origin: At the molecular level, gas particles move randomly at high speeds. When
they collide with the walls of a container, they transfer momentum to the
surface—producing a measurable force.
3. Statistical
Average: The net pressure arises from averaging the momentum changes of many
molecular collisions, as described by kinetic theory.
Feynman shows how
macroscopic quantities like force and pressure arise from the statistical
behavior of microscopic particles, bridging Newtonian mechanics with kinetic
theory of gases and linking individual molecular motion to thermodynamic
properties.
“… but
eventually, when equilibrium has set in, the net result is that the collisions
are effectively perfectly elastic. On the average, every particle that comes in
leaves with the same energy. So we shall imagine that the gas is in a steady
condition, and we lose no energy to the piston because the piston is standing
still (Feynman et al., 1963, p. 39-3).”
In his 1857 paper, Clausius writes: “In order
that Mariotte's and Gay-Lussac's laws, as well as others in connexion
with the same, may be strictly fulfilled, the gas must satisfy the following
conditions with respect to its molecular condition:
(1) The space
actually filled by the molecules of the gas must be infinitesimal in comparison
to the whole space occupied by the gas itself.
(2) The duration of
an impact, that is to say, the time required to produce the actually occurring
change in the motion of a molecule when it strikes another molecule or a fixed
surface, must be infinitesimal in comparison to the interval of time between
two successive collisions.
(3) The influence
of the molecular forces must be infinitesimal (p. 116).”
In essence,
Clausius stated three key simplifying assumptions to model ideal gases:
- Infinitesimal Molecular
Volume: The
volume occupied by gas molecules is negligible compared to the container’s
volume.
- Infinitesimal Collision
Duration: The
time a collision takes is negligible compared to the time between
collisions.
- Infinitesimal Molecular
Forces:
Intermolecular forces are negligible except during collisions.
While Clausius
restricted his model to these three assumptions, kinetic theory has
refined them to account for real-gas effects (e.g., van der Waals forces). However,
Clausius's framework remains a milestone in the development of statistical
mechanics.
The kinetic theory
of gases is built on a set of simplifying assumptions that ensure analytical
solvability while offering reasonable agreement with experimental observations
for gases:
1. Point Particles:
Gas molecules are idealized as point masses since their individual
volumes are negligible compared to the container size (L). Thus, the time between
collisions with the same wall can be simplified as Δt = 2L/vx, where vₓ is the average
velocity component in the x-direction.
2. No
Intermolecular Forces (Except During Collisions): Molecules are
assumed not to exert forces on each other except during brief, elastic collisions.
Between collisions, they move in straight lines at constant speeds.
3. Short Collision
Duration: Collisions are assumed to occur instantaneously, allowing the momentum
change to be treated as abrupt without the need of modeling the detailed
interaction over time.
4. Perfectly Elastic Collisions: All collisions—whether between
molecules or with the container walls—are assumed to be perfectly elastic. This
implies:
(a) Kinetic energy
is conserved, with no energy loss to heat or deformation.
(b) When a molecule
collides with a wall, its momentum changes from +p to –p, but
its speed remains unchanged.
5. Large Number of
Particles: The gas consists a large number of molecules (e.g., 1023 or more), allowing
statistical averaging. This enables definitions of macroscopic quantities such
as pressure and temperature.
6. Random Motion: Molecules move
randomly, following the Maxwell-Boltzmann distribution. At any moment, molecules
are equally likely to move in any direction. The mean square velocity is
distributed evenly among the three spatial dimensions: ⟨v2⟩=⟨vx2⟩+⟨vy2⟩+⟨vz2⟩ where ⟨·⟩ denotes an ensemble averaging.
7. Negligible
Gravitational Effects: Gravitational forces are considered too weak to
significantly influence molecular motion. As a result, the velocity
distribution remains isotropic: ⟨vx2⟩ = ⟨vy2⟩ = ⟨vz2⟩ = ⟨v2⟩/3.
Some physicists
introduce additional simplifying assumptions, such as identical particle masses
(m), negligible relativistic effects (valid at low to moderate
temperatures), and the absence of quantum effects (valid at high temperatures
and low densities). These assumptions underpin the derivation of the ideal gas
law and help connect microscopic particle dynamics to macroscopic thermodynamic
observables. While real gases deviate from ideal behavior—especially at high
densities or low temperatures—the kinetic theory remains a foundational
framework for understanding gas behavior under most practical conditions.
2. Energy per unit volume
“For a monatomic gas we
will suppose that the total energy U is equal to a number of atoms
times the average kinetic energy of each, because we are disregarding any
possibility of excitation or motion inside the atoms themselves. Then, in these
circumstances, we would have PV= (2/3)U (Feynman et al., 1963, p. 39-5).”
Feynman showed that
the product PV of a monatomic ideal gas corresponds is directly
proportional to the internal energy U. This does not mean PV
represents the work done by compressing a gas to zero volume at constant
pressure—such a process would be physically unattainable. Rather, pressure and
volume are interdependent, governed by the ideal gas law, and cannot be varied
independently without altering other state variables. Notably, kinetic theory
offers a more fundamental view of pressure—not merely as force per unit area,
but as the rate of momentum transfer per unit area due to molecular collisions.
This perspective also allows pressure to be interpreted as an energy density
(energy per unit volume), revealing a deep connection between the mechanical
origin of pressure and its thermodynamic role.
Note: A single
particle cannot exert pressure in the thermodynamic sense—this pressure is a
statistical property that emerges only from the collective behavior of many
particles.
“It is only a matter of
rather tricky mathematics to notice, therefore, that they are each equal to
one-third of their sum, which is of course the square of the magnitude of the
velocity: ⟨vx2⟩=
(1/3)⟨vx2+ vy2+
vz2⟩=⟨v2⟩/3
(Feynman et al., 1963, p. 39-4).”
The
"trick" Feynman highlights goes beyond the familiar Pythagorean
theorem (or famous theorem of Greek*); it lies in bridging geometric symmetry with
statistical reasoning. First, the equation v2=vx2+vy2+vz2, which relies on the
three-dimensional Pythagorean theorem, applies to the velocity of a single atom
or molecule. Second, the expression <v2> = <vx2
+ vy2 + vz2> may resemble the
Pythagorean theorem, but its physical meaning is about statistical averaging
over a large number of atoms. Third, a key insight comes from exploiting
spherical symmetry. In an idealized isotropic system—where no direction is preferred
and external forces such as gravity are absent—the average kinetic energy is
evenly distributed across all spatial dimensions. This symmetry allows us to
reduce the complexity of three-directional motion to a simple relation: <vx2>
= <v2>/3. The one-third factor, a consequence
of isotropy, underpins the derivation of the equipartition theorem and
ultimately leads to the ideal gas law.
*In the audio recording [18:00], Feynman mentions the 'famous theorem of
the Greeks,' more commonly known today as the Pythagorean theorem—though in higher
dimensions, it is sometimes associated with de Gua’s theorem.
3. Quasi-static adiabatic compression
“A
compression in which there is no heat energy added or removed is called
an adiabatic compression, from the Greek a (not) + dia (through)
+ bainein (to go). (The word adiabatic is used in physics in
several ways, and it is sometimes hard to see what is common about them.)
(Feynman et al., 1963, p. 39-5).”
The term adiabatic
derives from the Greek a- (not) and diabatos (passable), meaning “not
passable”—in this context, referring to the absence of thermal energy transfer.
In thermodynamics, a process is considered adiabatic if there is no heat transfer
between a system and its surroundings, formally expressed as Q = 0 where
Q is the heat transfer. This condition can be achieved—or more
accurately, approximated—in two main ways:
1.
Perfect insulation – The system
is thermally isolated, preventing any heat flow.
2.
Rapid process – The process occurs so quickly
that there is insufficient time for significant heat transfer (e.g., a sudden
gas expansion).
In general,
adiabatic conditions are idealized approximations—used to simplify the analysis
of systems in which heat transfer is minimal or intentionally ignored. In
reality, perfectly adiabatic processes are physically unattainable; even under
highly controlled conditions, some degree of thermal interaction inevitably
occurs. As such, the term adiabatic can be somewhat misleading when
applied to complex real-world systems—such as quantum systems—where complete
isolation from thermal exchange is practically impossible.
“That
is, for an adiabatic compression all the work done goes into changing
the internal energy. That is the key—that there are no other losses of
energy—for then we have PdV=−dU (Feynman et al., 1963, p. 39-5).”
Specifically, it is
a quasi-static adiabatic compression, which has the following key features:
1. Quasi-static
(Reversible): The process is carried out infinitely slowly, allowing the system to remain
in thermal equilibrium at every stage. This ensures the process is reversible
and that pressure P and volume V are well-defined throughout, allowing work to
be calculated as ∫P dV.
2. Adiabatic
condition (no heat transfer): The system is perfectly insulated,
so no heat transfer with the surroundings. This implies ΔQ=0, and all energy
transfer occurs only through mechanical work.
3. Compression (external
work): Work is done on the gas by compressing it, which increases its
internal energy. Since ΔQ = 0, the first law of thermodynamics reduces to dU = −PdV,
where the change in internal energy dU results entirely from volume change
under pressure.
This idealized
model is fundamental in thermodynamics, providing insight into processes such
as the temperature rise of a gas during compression and forming the theoretical
basis for thermodynamic cycles, including those in heat engines.
Everyday Connection
“In
banging against the eardrums they make an irregular tattoo—boom, boom,
boom—which we do not hear because the atoms are so small, and the sensitivity
of the ear is not quite enough to notice it. The result of this perpetual
bombardment is to push the drum away, but of course there is an equal perpetual
bombardment of atoms on the other side of the eardrum, so the net force on it
is zero…... We sometimes feel this uncomfortable effect when we go up too fast
in an elevator or an airplane…... (Feynman et al., 1963, p. 39-3).”
Another notable
example is swimming-induced vertigo, often caused by air pressure imbalances in
the ear—a condition known as alternobaric vertigo (swimming-induced vertigo).
This type of vertigo can occur in several scenarios:
Shallow-water
diving: Even small changes in depth (1–2 meters) can cause discomfort due to
unequal pressure in the ears.
Uneven pressure
equalization: Clearing pressure in one ear but not the other, sometimes due to nasal
congestion or poor technique.
Tight swim goggles: Excessive external
pressure on the outer ear may worsen air pressure imbalances.
While swimming may
improve posture (e.g., reverse hunchback), relieve neck discomfort or reduce back
pain, addressing one issue can sometimes introduce another.
Review Questions:
1. What is the
minimum number of assumptions needed for the kinetic theory of (ideal) gases?
2. How does the
mechanical definition of pressure as force per unit area (F/A) relate to
its thermodynamic interpretation as energy per unit volume (U/V)?
3. Can a Zen master
releasing intestinal gas be considered an example of an adiabatic process? What
conditions (e.g., rapid expansion, thermal isolation) would be necessary for it
to approximate an adiabatic process?
The moral of the lesson (in Feynman’s spirit): While one might theoretically liken flatulence to a quasi-static process, biological reality imposes strict constraints—no human can regulate the release slowly enough to maintain thermal equilibrium. In practice, achieving 'no heat transfer' requires either near-perfect insulation or a process so rapid that heat exchange is negligible—such as an adiabatic compression.
Note: The term
'adiabatic' was first introduced by William John Macquorn Rankine in his 1866
publication as shown below.
![]() |
(Rankine, 1866) |
References:
Clausius, R.
(1857). Ueber die Art der Bewegung, welche wir Wärme nennen [On the nature
of the motion which we call heat]. Annalen der Physik und Chemie, 176(3),
353–380.
Feynman,
R. P., Leighton, R. B., & Sands, M. (1963). The Feynman lectures on
physics, Vol. I: Mainly mechanics, radiation, and heat. Addison-Wesley.
Rankine,
W. J. M. (1866). On the theory of explosive gas engines. Proceedings
of the Institution of Civil Engineers, 25, 509–539.
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