Is the Boltzmann energy distribution an instance of energy diffusion?

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Discussion Overview

The discussion revolves around the relationship between the Boltzmann energy distribution and the concept of energy diffusion, particularly in the context of thermodynamic equilibrium and entropy. Participants explore the implications of these concepts in both theoretical and practical scenarios, including the notion of "heat death" in the universe.

Discussion Character

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

Main Points Raised

  • One participant suggests that both solute diffusion and energy diffusion are forms of diffusion, questioning why solute diffusion reaches a zero density gradient while energy diffusion maintains a non-zero energy gradient at maximum entropy.
  • Another participant seeks clarification on the meaning of the "gradient" mentioned, asking for references to support the claims made.
  • A claim is made that Boltzmann predicts a non-zero range of particle energies will persist indefinitely in a steady-state, raising the question of why particle energies do not converge to a uniform value.
  • Some participants argue that the distribution of energies is not position-dependent and thus results in a zero gradient, challenging the notion of a persistent energy gradient.
  • One participant references the diffusion equation to support the idea that a uniform distribution is reached when the time derivative of density is zero.
  • Another participant discusses the concept of "heat death," suggesting that if the universe resembles a Maxwell-Boltzmann box, thermal energy may never completely diffuse uniformly, implying that heat death may not be achievable.
  • A later reply emphasizes the importance of energy conservation and discusses how the Boltzmann distribution relates to diffusion over energy surfaces, introducing the idea of local thermodynamic equilibrium in macroscopic systems.

Areas of Agreement / Disagreement

Participants express differing views on the nature of energy diffusion and its relationship to the Boltzmann distribution. There is no consensus on whether energy diffusion can be equated with solute diffusion, and the discussion remains unresolved regarding the implications for the concept of heat death.

Contextual Notes

Participants highlight various assumptions and conditions, such as the dependence on definitions of equilibrium and the complexities of projecting distributions in higher dimensions. There are also references to local thermodynamic equilibrium and the conditions under which it may or may not hold.

SteveMaryland
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I (mechanical engineer) have researched this question but can't get to an answer.

The equilibrium condition for confined particle diffusion of a solute in a solvent is reached when the solute spatial density is uniform (= zero density gradient), and entropy is max.

But per Boltzmann, when confined particles reach equilibrium, a non-zero energy gradient) persists indefinitely, even as max entropy is reached.

My assumption here is that both are cases of diffusion - one of species, one of thermal energy.

If both processes are cases of diffusion, why, at max entropy, does solute diffusion reach a zero density gradient, but energy diffusion reaches a non-zero energy gradient?
 
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Hi,

SteveMaryland said:
But per Boltzmann, when confined particles reach equilibrium, a non-zero energy gradient) persists indefinitely, even as max entropy is reached.
Could you clarify this ? What gradient are you referring to ?
Any links or references ?

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Boltzmann predicts that a non-zero range (= distribution, = gradient) of particle energies will persist "forever" in the steady-state. Since this is an energy-diffusion process, why do the particle energies not "diffuse" to a single uniform value for all particles the same way a solute/solvent particle density gradient diffuses to zero in the steady-state?
 
SteveMaryland said:
non-zero range (= distribution, = gradient)
That is not correct. A non-zero gradient means that there is a change when you look at another position.

The distribution as found comes out as a result of averaging and is not position dependent: the outcome is the same in all places. Ergo a zero gradient.

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But isn't this a pretty simple outcome of the diffusion equation,
$$\partial_t \rho(t,\vec{x})=D \Delta \rho(t,\vec{x}).$$
Solving this for a finite volume with the appropriate boundary conditions, this gives ##\rho=\text{const}## for ##\partial_t \rho=0##.
 
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BvU said:
That is not correct. A non-zero gradient means that there is a change when you look at another position.

The distribution as found comes out as a result of averaging and is not position dependent: the outcome is the same in all places. Ergo a zero gradient.

##\ ##
What then is the "heat death" of the universe? My understanding of the "heat death" is that condition reached where all of the thermal energy in the universe has (spontaneously) diffused to the point where there are no more (= zero) thermal gradients anywhere - all thermal energy has diffused to the limit of uniform distribution, just like ink will (spontaneously) diffuse in a solution to the limit of completely uniform distribution.

To what extent does the universe resemble the Maxwell-Boltzmann box of particles?

If there IS a resemblance, then that means that thermal energy will never "completely" diffuse (like ink in water) but rather will "stop" at the M-B distribution - which in turn means there will always be vestigial thermal gradients in the universe and "heat death" will never be reached.
 
You have lost me completely. And it seems to me you still think that there is a gradient where there is none.

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Alright, I will restate the question without using the word gradient - it's the same question:

What then is the "heat death" of the universe? My understanding of the "heat death" is that condition reached where all of the thermal energy in the universe has (spontaneously) diffused to the limit of uniform distribution, just like ink will (spontaneously) diffuse in a solution to the limit of completely uniform distribution.

To what extent does the universe resemble the Maxwell-Boltzmann box of particles? If there IS a resemblance, then that means that thermal energy will never "completely" diffuse (like ink in water) but rather will "stop" at the M-B distribution - which in turn means there will always be vestigial thermal gradients differences in the universe and "heat death" will never be reached.
 
@SteveMaryland: forget about the heat death of the universe for the moment. Are you familiar with energy conservation? (That orbits of closed classical systems are confined to a constant energy "level set"?) From a purely classical perspective, the Boltzmann distribution emerges from a sort of "diffusion" over a space that very closely resembles the constant energy surface (modulo ##O(N^{\alpha})## additional conserved quantities, where ##\alpha < 1##), after projecting the resulting uniform distribution over that surface to a (much) lower-dimensional subspace. Consider the uniform distribution on a sphere: after projecting it onto a 2D cross section, is it uniform? No: instead, it looks something like ##\rho(r) \propto \frac{1}{\sqrt{1-r^2/R^2}}##. Something similar happens in higher (i.e. ##N\sim 10^{23}##) dimensions, modulo subtleties pertaining to how "well separated" the dimensions are from each other in the Hamiltonian (i.e. you can anticipate the Maxwell Boltzmann distribution for a dilute gas coupled to a thermal solid along a smooth boundary, but it's slightly more difficult to guess an a priori accurate, effective, statistical mechanical Hamiltonian for, say, the Na ions in salt, ignoring the Cl ions and valence electrons.)

There are many systems in nature that satisfy the conditions for thermodynamic equilibrium, at least to reasonable precision, and many systems that do not. Usually (but not always), a macroscopic system that isn't in equilibrium in its entirety can be thought of as consisting of small unit cells that are each in local equilibrium, and to some extent vice versa (you might find it interesting to come up with a few criteria that might determine 'local thermodynamic equilibrium'.) For example, in fluid mechanics and dynamical models of phase-transitions, it is often assumed that a local temperature is well defined for each infinitesimal control volume even though there might be significant heat gradients over large scales; because heat spreads diffusively over short distances, the equilibration time scale tends to decrease rapidly with length scale.
 

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