Paradox: Thermodynamic equilibrium does not exist in gravitational fields

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Discussion Overview

The discussion revolves around the paradox of thermodynamic equilibrium in a gas subjected to a homogeneous gravitational field. Participants explore the implications of an adiabatic temperature gradient, the conditions for thermodynamic equilibrium, and the nature of energy flows within the system. The conversation includes theoretical considerations and challenges related to equilibrium states in gravitational contexts.

Discussion Character

  • Debate/contested
  • Conceptual clarification
  • Exploratory
  • Technical explanation

Main Points Raised

  • One participant posits that in an isolated system, a gas in a gravitational field should reach a state of thermodynamic equilibrium, but the presence of an adiabatic temperature gradient suggests otherwise.
  • Another participant questions the assumption of an adiabatic process, suggesting that equilibrium implies constant temperature throughout the system.
  • Some participants argue that the temperature gradient observed in a gravitational field is a characteristic of hydrostatic equilibrium, where local thermodynamic equilibrium can still exist at different elevations.
  • A participant introduces the concept of gravitational potential energy converting to kinetic energy, which could lead to a temperature gradient, challenging the notion of uniform temperature in equilibrium.
  • There is a discussion about the lapse rate in the Earth's atmosphere, with some participants asserting that it is not in thermodynamic equilibrium, while others argue that the lapse rate does not exist in a true equilibrium state.
  • One participant suggests that any temperature profile could theoretically be in hydrostatic equilibrium, but some profiles may lead to instabilities.
  • Another participant asserts that disturbances in equilibrium will be damped out, although they acknowledge that certain configurations can lead to instability and convection.

Areas of Agreement / Disagreement

Participants express differing views on the nature of thermodynamic equilibrium in gravitational fields, with no consensus reached on whether a true state of equilibrium can exist given the presence of temperature gradients. The discussion remains unresolved, with multiple competing perspectives presented.

Contextual Notes

Participants highlight the complexity of defining thermodynamic equilibrium in the presence of gravitational fields, noting that assumptions about particle interactions and energy transfers may affect conclusions. The discussion also touches on the implications of statistical mechanics in understanding temperature profiles.

  • #121
Petr Matas said:
I didn't evaluate the modified formula, because it is too complicated.
Petr Matas said:
Obviously, your normalization constant mβ2π has to change accordingly – it is replaced with the denominator above.
I am afraid that these properties suggest your formula as well as mine does not coincide with the thermal equilibrium.

My argument to your point:
Petr Matas said:
Maybe I have found a mistake. If I read this expression correctly, you are integrating over the particles, which are currently at the floor. I agree, that every particle bounces off the floor regularly, but they do so with different time periods tP(v0) and with different vertical velocities v0 (i.e. the time spent at 0–1 μm above the floor depends on v0). Both of these affect the particle's contribution to the velocity distribution at the floor and I think that they have to be compensated for in your integral by giving weight
We do not have to think of bouncing time period here because time average in period has been already considered in getting f(r).
anuttarasammyak said:
time to reach maximum
T=v0g
<z>=1T∫0Tz(t)dt
=v023g
 
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  • #122
anuttarasammyak said:
We do not have to think of bouncing time period here because time average in period has been already considered in getting f(r).
I see, ## t_{\rm P}(v_0) = 2T ##, where ##T## is the time to reach maximum. It seems to me that you incorporated it correctly into your formula for average height of individual particle ## \langle z(v_0) \rangle = h f(r) ##. The problem is averaging this average not only over the particles currently at the floor, but over those in the entire volume:
$$
\langle z \rangle = \frac 1 N \int_N \langle z(v_0) \rangle \, dN,
$$ where ##N## is the number of particles in the volume.

The Boltzmann distribution for ##z = 0## is the distribution of ##v_0## for particles currently at the floor, not in the entire volume.
 
  • #123
Petr Matas said:
The problem is averaging this average not only over the particles currently at the floor, but over those in the entire volume:
Why do you think that I have focused on the particles currently at the floor ? I used v_0^2 is to express energy of a trajectory wherever on the trajectory the ball is.
 
  • #124
anuttarasammyak said:
Why do you think that I have focused on the particles currently at the floor ? I used v_0^2 is to express energy of a trajectory wherever on the trajectory the ball is.
I am aware that ##v_0^2## characterizes the entire trajectory. So you have a population of trajectories. Where does its distribution come from?
 
  • #125
Petr Matas said:
Where does its distribution come from?
It is coming from you. You stated that energy of bouncing-balls have same distribution spectrum as Maxwell's.
 
  • #126
anuttarasammyak said:
It is coming from you. You stated that energy of bouncing-balls have same distribution spectrum as Maxwell's.
Let me explain. Assuming that particles currently at the floor have thermal spectrum of velocities ##v_0## and that they move without collisions, I derived the spectrum of velocities ##v## at altitude ##z##. I found that the spectrum is the same as at the floor and that the density is lower. But the derived spectrum isn't the spectrum of velocities ##v_0## at the bottom of the trajectory, but of velocities ##v## at altitude ##z##. Velocity ##v_0## is greater than ##v##. At altitude ##z## (unlike at the floor), there are no particles with ##|v_0| < \sqrt{2gz}##. In other words, different altitudes have the same spectra of ##v##, but different spectra of ##v_0##.
 
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  • #127
Petr Matas said:
. Assuming that particles currently at the floor have thermal spectrum of velocities v0 and that they move without collisions, I derived the spectrum of velocities v at altitude z.
anuttarasammyak said:
Recalling that for each trajectory
v0^2=v^2+2gz
this integral is exressed as
Is the spectrum
Ce^{-(\frac{1}{2}mv^2+mgz)\beta}=Ce^{-\frac{1}{2}mv_0^2\beta}
specified by total energy of the trajectory ##v_0^2## ?
 
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  • #128
anuttarasammyak said:
Is the spectrum
Ce^{-(\frac{1}{2}mv^2+mgz)\beta}=Ce^{-\frac{1}{2}mv_0^2\beta}
specified by total energy v_0^2 ?
Yes, but the phase space has two dimensions (##z## and ##v##), so we must integrate over both,
$$
\begin{align}
\langle z \rangle &= C \int_0^h dz \int_{-\infty}^{+\infty} dv \, e^{-\frac{1}{2}mv_0^2\beta} \, z \nonumber \\
&= C \int_0^h dz \int_{-\infty}^{+\infty} dv \, e^{-\frac{1}{2}mv_0^2\beta} \, \langle z(v_0) \rangle, \nonumber
\end{align}
$$ or compensate for it with the weight.
 
  • #129
physicsprint said:
Yup, that's peace for ya. Relativity
I dropped the relativity altogether after finding that it does not resolve the paradox.
 
  • #130
Petr Matas said:
Yes, but the phase space has two dimensions (z and v), so we must integrate over both,
<br /> \begin{align}<br /> <br /> \langle z \rangle &amp;= C \int_0^h dz \int_{-\infty}^{+\infty} dv \, e^{-\frac{1}{2}mv_0^2\beta} \, z \nonumber \\<br /> <br /> &amp;= C \int_0^h dz \int_{-\infty}^{+\infty} dv \, e^{-\frac{1}{2}mv_0^2\beta} \, \langle z(v_0) \rangle, \nonumber<br /> <br /> \end{align}
=C \int_0^h dz \ e^{-mgz\beta} \int_{-\infty}^{+\infty} dv \ e^{-\frac{1}{2}mv^2\beta} &lt;\mathbb{z}(\sqrt{v^2+2gz})&gt;
which is equivalent to my
anuttarasammyak said:
this integral is exressed as
\sqrt{\frac{m\beta}{2\pi}}\int_{-\infty}^{+\infty}dv\int_0^h dz \ f(\frac{2gh}{v^2+2gz})e^{-(\frac{1}{2}mv^2+mgz)\beta}
where integration wrt z and integration wrt v are not separatively done.
Now we get the same result which is different from thermal equilibrium.
 
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  • #131
anuttarasammyak said:
=C \int_0^h dz \ e^{-mgz\beta} \int_{-\infty}^{+\infty} dv \ e^{-\frac{1}{2}mv^2\beta} &lt;z(\sqrt{v^2+2gz})&gt;
which is equivalent to my

Now we get the same result which is different from thermal equilibrium.
Now that the problem is solved with statistical mechanics, one could check if we can exhaust the methods and see if one gets the same solutions with Langevin equations of with Fokker-Planck equation.
 
  • #132
The problem is also how you define temperature. In thermodynamics, systems in thermal equilibrium are defined to have the same temperature. However, this is not the temperature you measure, say, with a mercury thermometer which is the "local temperature". Hence you cannot run a carnot engine between two states at different heights, if they are in thermal equilibrium, although they have different local temperatures.
 
  • #133
DrDu said:
The problem is also how you define temperature. In thermodynamics, systems in thermal equilibrium are defined to have the same temperature. However, this is not the temperature you measure, say, with a mercury thermometer which is the "local temperature". Hence you cannot run a carnot engine between two states at different heights, if they are in thermal equilibrium, although they have different local temperatures.
Maxwell refferred in post #26 says that temperature is same at high and low positions. What you mention is the progress after him ?
I find the relation in (27.2) of Landau-Rifshitz Statistial Mechanics
T\sqrt{g_{00}}=const.
So in thermal equillibrium
T_{@high}&lt;T_{@low}
 
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  • #134
I would call ##T\sqrt{g_{00}}## the thermodynamical temperature and ##T## the local temperature. thermodynamical temperature is a consequence of the zeroth law of thermodynamics (transitivity of thermal equilibrium). There is no reason to think that it does not hold in gravitational systems. The situation is comparable to the concept of mass, given your interest, in special relativity there is rest mass, longitudinal mass and transversal mass. All three concepts coincide in the non-relativistic Galilean limit. So in gravitational fields, it might be useful to introduce several temperature concepts. This is ok, so long as you make clear which one you are using.
 
  • #135
DrDu said:
I would call ##T\sqrt{g_{00}}## the thermodynamical temperature and ##T## the local temperature. thermodynamical temperature is a consequence of the zeroth law of thermodynamics (transitivity of thermal equilibrium). There is no reason to think that it does not hold in gravitational systems.
It resembles with
\omega\sqrt{g_{00}}=const.
along world line of a photon which means red shift of going up light. They have the same reason.
Photon gas in vertical cylinder at equilibrium show blueish at bottom end and reddish at top end.
 

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