Pressure and Newtonian potential energy

In summary, the recent discussions on pressure as a source of gravity and the related Tolman paradox have brought attention to the fact that even in Newtonian gravity, pressure is related to potential energy. Specifically, in an isolated static system of masses in free space, the total force across any plane must be zero for the system to be in equilibrium. This means that the integral of normal pressure over perpendicular planes is equal and opposite to the gravitational potential energy of the system. This result, while not currently known by a specific name, is easy to show and has significant implications. Furthermore, the Bianchi identities in general relativity prevent sudden changes in support or pressure, making it a more restrictive model than in Newtonian gravity. In short, the pressure
  • #1
Jonathan Scott
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Recent discussions on pressure as a source of gravity and the related Tolman paradox have reminded me that few people seem to be aware that even in Newtonian gravity the pressure is related to the potential energy, which I've mentioned a few times on these forums before.

This is easy to show, but a bit messy to describe. I'd like to know whether this is a known named result, and whether someone can give me a simpler way of describing it in Newtonian terms (preferably without requiring the use of GR-style tensor notation as in the Komar mass expression).

Specifically, if you have an isolated static system of masses in free space internally supported in equilibrium by any means (rods, strings, springs, balloons or whatever), then if you integrate the normal pressure component over planes perpendicular to three perpendicular axes through the whole system, the total of the three integrals is a positive quantity equal and opposite to the gravitational potential energy of the system.

To show this, you can divide up the system conceptually into point masses where each one is joined to all other point masses by lines representing their gravitational interaction. For the system to be static, the total force (including gravitational) across any plane must be zero. The gravitational force along the line between masses ##m_i## and ##m_j## is then ##-Gm_i m_j/r_{ij}^2##, so this is the contribution to the overall force across any plane cutting the line between those masses, which must be equal and opposite to the integral over that plane of the pressure. The force is the same at all points on the line between the masses. If the pressure is integrated along that line, that simply multiplies the result by ##r_{ij}## giving a contribution ##Gm_i m_j / r_{ij}## for that pair of masses, equal and opposite to the potential energy between those masses.

More generally, if the displacement vector ##(x,y,z)## between two masses is not perpendicular to the plane, the normal pressure is reduced by the cosine of the angle between the displacement line and the perpendicular to each plane, and so is the perpendicular component of the length of the line, so the contributions for three planes add up as ##x^2/r^2##, ##y^2/r^2## and ##z^2/r^2##, adding up to the same total as the original case. As these quantities add linearly for all contributing point masses, the total for the system is equal and opposite to the total potential energy of the system.

This means for example that if the system just consists of a perfect fluid held together by gravity, the gravitational potential energy is equal and opposite to the volume integral of three times the pressure.

Note that in the Newtonian case it is clear that although this pressure integral is equal and opposite to the potential energy for a static system, it cannot be identified with the potential energy, because for example if a support is removed and the system starts to collapse, the Newtonian potential energy is initially unaffected, but terms in the pressure integral can vanish immediately, at least to orders of magnitude smaller than their original values.

(For this reason, I feel that Tolman was on to something and there is something wrong either with the conventional interpretation that pressure is a source of gravity in GR or with the field equations themselves, but that's a different topic).
 
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  • #2
Jonathan Scott said:
I'd like to know whether this is a known named result

Not to my knowledge, but if it isn't it is somewhat surprising, since as you say it's easy to show, and it does seem to be something that's worth having a named result for. :wink:

Jonathan Scott said:
whether someone can give me a simpler way of describing it in Newtonian terms

Intuitively, I would say that, in hydrostatic equilibrium, the force due to pressure at any point must just balance the gravitational force. The gravitational force is the gradient of the potential, so integrating it over the volume of the object, heuristically, gives you the gravitational potential energy itself, and therefore you would expect that integral to be proportional to the volume integral of the pressure. The factor of 3 would come from the fact that there are 3 spatial dimensions.

Jonathan Scott said:
I feel that Tolman was on to something and there is something wrong either with the conventional interpretation that pressure is a source of gravity in GR or with the field equations themselves

As you say, we've had this discussion before. :wink:

One thing I would mention is that the idea of "removing a support instantly" doesn't work as it stands in GR, because of the automatic conservation of the source--the Bianchi identities. There is nothing corresponding to those in Newtonian gravity, so, for example, in Newtonian gravity it's perfectly possible to construct a model where at time ##t = 0## a supporting strut suddenly just disappears, or the pressure inside an object in hydrostatic equilibrium suddenly just vanishes. In GR it's not possible to construct such a model, because it would violate the Bianchi identities, which means there is no solution of the Einstein Field Equation that describes such things.

I realize that "suddenly disappears" and "suddenly vanishes" are idealizations, and a more rigorous model would replace them with something more like "changes, not instantaneously, continuously, but really fast compared to all other timescales in the problem". But I still think that it's very important to pay attention to the constraints on the model from the Bianchi identities, since those constraints are quite a bit more restrictive than just "the change needs to be continuous".
 
  • #3
PeterDonis said:
Intuitively, I would say that, in hydrostatic equilibrium, the force due to pressure at any point must just balance the gravitational force. The gravitational force is the gradient of the potential, so integrating it over the volume of the object, heuristically, gives you the gravitational potential energy itself, and therefore you would expect that integral to be proportional to the volume integral of the pressure. The factor of 3 would come from the fact that there are 3 spatial dimensions.
Thanks for another way of looking at it.

I'm wondering whether there is a simple way to write down the integral which I've mostly described in words, without needing to express it as a sum of three separate integrals along arbitrary axes.

PeterDonis said:
One thing I would mention is that the idea of "removing a support instantly" doesn't work as it stands in GR, because of the automatic conservation of the source--the Bianchi identities. There is nothing corresponding to those in Newtonian gravity, so, for example, in Newtonian gravity it's perfectly possible to construct a model where at time t=0 a supporting strut suddenly just disappears, or the pressure inside an object in hydrostatic equilibrium suddenly just vanishes. In GR it's not possible to construct such a model, because it would violate the Bianchi identities, which means there is no solution of the Einstein Field Equation that describes such things.
In this case, there's no problem with "instantly" being a little slower. Removing a support doesn't mean removing matter or energy; it could just be taking a very thin rod which has a cut through it between frictionless faces and pushing the two parts a little so they slip past each other. Although this would temporarily cause a wave to propagate within the parts of the rode at up to the speed of sound in the material, the kinetic and potential energy in that wave would depend on the characteristics of the rod material and would typically be orders of magnitude too small for the pressure to continue to match the potential energy. Basically, there could be a little energy stored when the force in the rod causes it to be compressed elastically by a small distance, which can be arbitrarily small for a stiff rod, but since the pressure integral term is equal to exactly the same force multiplied by the full length of the rod, the energy from compression would be tiny in comparison.

(And as I've mentioned before in the GR-related threads, what is conserved is energy and momentum, not pressure or stress, so the conservation laws do not prevent a fairly abrupt change of pressure).
 
  • #4
Jonathan Scott said:
I'm wondering whether there is a simple way to write down the integral which I've mostly described in words, without needing to express it as a sum of three separate integrals along arbitrary axes.

For the spherically symmetric case, I think it can be written as an integral in one variable, since everything is a function of one variable (the radial coordinate).

Jonathan Scott said:
In this case, there's no problem with "instantly" being a little slower.

As I said, we've had this discussion before. :wink: I don't see the point of rehashing it here since we are just talking about heuristic, intuitive speculations; one would need to actually develop a specific mathematical model based on the EFE and see what it says.
 
  • #5
Jonathan Scott said:
as I've mentioned before in the GR-related threads, what is conserved is energy and momentum, not pressure or stress

No, what is conserved is the stress-energy tensor, in the sense that its covariant divergence is zero. That tensor includes pressure and stress as well as energy and momentum.
 
  • #6
PeterDonis said:
For the spherically symmetric case, I think it can be written as an integral in one variable, since everything is a function of one variable (the radial coordinate).
I'm still looking for a neat way to describe the integral in the general Newtonian case. I guess it will probably have to involve some sort of tensor notation, but just 3D tensors in flat space.

PeterDonis said:
As I said, we've had this discussion before. :wink: I don't see the point of rehashing it here since we are just talking about heuristic, intuitive speculations; one would need to actually develop a specific mathematical model based on the EFE and see what it says.
For purposes of this thread, I was talking about the Newtonian case. It is very clear in the Newtonian case that the pressure integral is exactly equal to the potential energy when static, but nowhere near equal to the potential energy when released into a dynamic situation, for example by a rod being split as previously described, even though the Newtonian potential energy of the system is initially unchanged (although part of it will soon be converted to kinetic energy if a support has been removed).
 
  • #7
PeterDonis said:
No, what is conserved is the stress-energy tensor, in the sense that its covariant divergence is zero. That tensor includes pressure and stress as well as energy and momentum.
The stress-energy tensor represents the flow of the four components of energy-momentum density in the four directions of space-time, where for example the flow of x-momentum density in the x-direction is pressure. In flat space, each term of the ordinary divergence is effectively a continuity equation for one of those four components of the energy-momentum, giving global conservation of each component separately. As I understand it, the covariant divergence also takes into account the effect of curved space, so what is conserved is effectively the flow of energy-momentum density relative to a local free fall frame. So what is conserved is not the stress-energy tensor itself, but the energy and momentum whose flow is represented by the stress-energy tensor.

I thought this had been clarified before. I don't really want to discuss it again in this thread, which is supposed to be about the Newtonian pressure integral. It obviously still places constraints on what can happen with changing pressure, but pressure is definitely not "conserved".
 
  • #8
Jonathan Scott said:
I'm still looking for a neat way to describe the integral in the general Newtonian case.

For the general case, I don't think there's any way to avoid either tensors or something equally forbidding. :wink:

Jonathan Scott said:
The stress-energy tensor represents the flow of the four components of energy-momentum density in the four directions of space-time

Sure, but, as you note, if you insist on using this language, "energy-momentum density" includes pressure and stresses. So your statement that pressure is somehow "not included" is not correct.

Jonathan Scott said:
I thought this had been clarified before.

I thought so too, but the way you are stating it here does not correspond to what I thought had been clarified. See above.

In any case, I think it's highly preferable to express all this in math, not ordinary language, since, as we have just shown, ordinary language is vague.
 
  • #9
I think the pressure integral I've been describing can be simplified to simply taking the sum of the pressure in any three perpendicular directions at each point then taking the volume integral of that sum. That's like integrating the trace of the ordinary 3D stress tensor. Does that make it any more familiar to anyone?
 
  • #10
Jonathan Scott said:
I think the pressure integral I've been describing can be simplified to simply taking the sum of the pressure in any three perpendicular directions at each point then taking the volume integral of that sum. That's like integrating the trace of the ordinary 3D stress tensor. Does that make it any more familiar to anyone?

Not in the Newtonian case, but in the GR case this works out (once you include the correction factor for spacetime curvature and the 00 component of the stress-energy tensor) to be the Komar mass integral, for which it is well known that the contributions of pressure and gravitational potential energy exactly cancel (since the Komar mass only applies to stationary spacetimes, the concept of "gravitational potential energy" is well-defined). So I would say what you propose is certainly reasonable for the Newtonian case.
 
  • #11
Progress!

I've now realized that there's another simple quantity in Newtonian gravity which appears to create a total quantity equal and opposite to the potential energy, even in a dynamic situation, when added to the pressure term for an overall system. It's the integral of the dot product of the force density (mass density times acceleration) and the position. The position term is weird, in that it is relative to any arbitrary origin (as for example also applies to a center-of-mass calculation), but given that the overall force must be zero, it all balances out.

For example, consider a simple system of two small freely-moving particles with masses ##m_1## and ##m_2## separated by distance ##r##. Each of them will be accelerated towards the other with force ##Gm_1m_2/r^2## along the line between them. If we take the dot product of the force with the position of each one, since the forces have opposite sign we have effectively taken the dot product of the force with the vector between the two masses, which has magnitude ##r##, so the result is ##Gm_1m_2/r## which is equal and opposite to the potential energy between those masses.

These terms add linearly so they should also work for any combination of static and freely-moving masses. I'm not sure about the details in complex cases such as where internal pressure is accelerating one part of an object relative to another, but that would be just ordinary mechanics.

So this defines a quantity which is equal to the Newtonian potential energy both for static and dynamic situations, extending the pressure term of the Komar mass to dynamic situations.

This suggests that if pressure acts as a source of gravity in GR, then this new dynamic term must also do so, otherwise internal pressure fluctuations within a system could cause fluctuations in the distant field, which (as Tolman pointed out) seems highly implausible. Perhaps it's already there in the GR maths, although I don't have the skills and patience to investigate that.
 
  • #12
Note that the integral of the cross product of a force density and a position vector is already a well-known physical quantity: torque. In the case of a complete system conservation of angular momentum means this is zero. So one could actually take the algebraic product of the force density and position vector (including both the dot and cross product terms) and it would still give the dynamic part of the potential energy expression.
 
  • #13
Jonathan Scott said:
if pressure acts as a source of gravity in GR
There is no "if" involved. The source of gravity in GR is the stress energy tensor, and pressure is part of that.
 
  • #14
Jonathan Scott said:
This suggests that if pressure acts as a source of gravity in GR, then this new dynamic term must also do so

I don't see how such a term appears in the stress-energy tensor.

Jonathan Scott said:
otherwise internal pressure fluctuations within a system could cause fluctuations in the distant field, which (as Tolman pointed out) seems highly implausible

Is there an online reference that gives Tolman's argument? I'm wondering if a key premise of the argument is that the fluctuations have to be purely "internal", i.e., there is some boundary condition imposed at the surface of the object (for example, holding the object's radius, surface area, etc. constant). In the presence of such a boundary condition, yes, I can see how we would not expect internal fluctuations to affect the external field; but I also think such a boundary condition is highly implausible except as an extreme idealization.
 
  • #15
The new term in the Newtonian equivalent involves the energy density, the acceleration and spatial coordinates, all of which are in some way involved in the stress-energy tensor and its time and space derivatives. The new term only applies in non-static cases and it would need to cause the equivalent effect of a transient additional source for the period in which the system was changing.

I don't remember where I originally saw this one of Tolman's paradoxes (there are several) first mentioned, but I see it is also mentioned in the paper "Pressure as a source of gravity" by J Ehlers: https://arxiv.org/pdf/gr-qc/0510041.pdf

Here's a brief excerpt:
The following scenario is known as Tolman’s Paradox: A static spherical box has been filled with a gravitating substance of a given mass. If this substance undergoes an internal transformation (e.g. matter and anti-matter turning into radiation) raising the pressure, the active mass in the box would change because of the 3p-term since the energy is conserved. However, such an internal transformation should not affect the mass measured outside the box, say by an orbiting particle obeying Kepler’s third law. In a spherically symmetric field the particle should be oblivious to all spherically symmetric changes inside its orbit, a consequence of the vacuum equations known as Birkhoff’s Theorem [6].

This particular paper does not address the case in which I'm interested, as it only addresses the static or slowly-changing case and shows that as in the Newtonian equivalent any increase in pressure in one place is matched by a cancelling increase in tension elsewhere, which I do not find surprising.

The surprising case is where the pressure changes abruptly and material is being accelerated as a result, for example if a supporting shell breaks and material falls. It is only when a new static situation is reached with no net acceleration that the original pressure is restored.

In a static situation the pressure within a single object acts as a source equal and opposite to the potential energy (as in the Komar mass). That pressure can temporarily decrease or increase while material is being accelerated internally. However, Birkhoff's theorem says that the external field is unaffected by internal changes (provided they are close enough to spherically symmetrical). This is what I understand to be the Tolman paradox in its original form. As far as I can see, this means that during the transient period when the pressure is unbalanced, there must be some other physical term which effectively compensates for the difference in pressure to maintain a constant source strength.

For the Newtonian case, my new term added to the pressure term gives a quantity equal and opposite to the potential energy even in a general dynamic case involving a mixture of free-falling and static objects. If a support breaks or similar the total remains unaffected, with the acceleration term taking over from the pressure term. Obviously the potential energy can change gradually as the configuration changes, but there is no instantaneous change even during the process of a support breaking or similar. A similar term in GR could therefore fix this Tolman paradox completely.
 
  • #16
Jonathan Scott said:
The new term in the Newtonian equivalent involves the energy density, the acceleration and spatial coordinates, all of which are in some way involved in the stress-energy tensor and its time and space derivatives.

Energy density is part of the SET, yes. Acceleration would be a first derivative of a momentum density; momentum density is in the SET. But only the SET itself is a source of gravity; its derivatives are not.

Jonathan Scott said:
The surprising case is where the pressure changes abruptly and material is being accelerated as a result, for example if a supporting shell breaks and material falls.

We've had discussions on this before. :wink: The corresponding change in the SET is in momentum terms, not acceleration, since there are no acceleration terms in the SET. The momentum terms are "where the pressure goes" to keep the overall source behavior the same as seen externally.

Note that the statement that ##\rho + 3p## is the "source" of gravity, as made for example in the paper you quoted from, is only true in static situations. In dynamic situations momentum is also a source of gravity, since it appears in the SET (also viscous stresses).
 
  • #17
When a collapse occurs (such as a support failing) there is a sudden change in pressure but there is no instantaneous change in momentum nor in position. There is however an instantaneous change in acceleration, and I've spotted that in the Newtonian case this can explain where the potential energy equivalent "goes".

An accelerated object is known to induce gravitational acceleration via the linear frame-dragging effect but the source acceleration doesn't feature directly in the SET.
 
  • #18
Jonathan Scott said:
When a collapse occurs (such as a support failing) there is a sudden change in pressure but there is no instantaneous change in momentum nor in position.

We had this discussion before. :wink: See post #2 in this thread.

Basically, your argument is intuitive hand-waving, but my argument is a solid mathematical theorem: the SET is locally conserved (its covariant divergence is zero). That theorem means that it is impossible for stress-energy to just "disappear". But your intuitive hand-waving basically says that stress-energy can "disappear"--you're claiming that there is an imbalance between the change in one component and the change in other components. So your intuitive hand-waving argument must be wrong since it contradicts a mathematical theorem.

I cannot give you a detailed explanation of why your intuitive argument is wrong. But the above should explain why I think it's wrong even though I can't do that. And it should also clarify your burden of proof: you need a lot more than just intuitive hand-waving. You need to show how either the mathematical theorem is wrong (which seems to me to be a non-starter), or how your intuitive hand-waving doesn't actually contradict it even though it appears that it must.
 
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  • #19
PeterDonis said:
The momentum terms are "where the pressure goes" to keep the overall source behavior the same as seen externally.

Actually, since the local conservation law involves covariant derivatives, this isn't completely true in a dynamic situation, since in a dynamic situation the gravitational potential energy is also changing (strictly speaking, it isn't well-defined, but I think that can be finessed). Also the energy density is changing. So heuristically, I think the balance in rates of change (to satisfy local conservation) would look something like energy density change + pressure change + momentum density change + potential density change = 0.

For example, in a case of spherically symmetric collapse of an object like a star due to a loss of internal pressure, this heuristic balance would look something like: energy density increasing, pressure decreasing, momentum density increasing, potential density decreasing, overall balance zero.
 
  • #20
Jonathan Scott said:
there is a sudden change in pressure but there is no instantaneous change in momentum
This is not really correct. In relativistic terms the change in pressure is not sudden, and it goes exactly at pace with the not sudden change in momentum.
 
  • #21
There are formalisms (ADM mass and Bondi mass) that give a sensible value for 'mass' in asymptotically flat space-times. These sorts of mass handle the problem of a pressure vessel that's rigged to self-destruct and turn into an expanding ball of gas without any glitches. So we do have concepts of mass that can handle this sort of transition, they are just not the ones that one might be used to.

Using these approaches, the mass is derived from the behavior of the metric at infinity. As a consequence, one loses the idea of the mass as some sort of integral of the stress-energy tensor, and replaces it with something that's derived from the space-time curvature.

So how the pressure changes doesn't matter so much. That's part of the stress-energy tensor, but we compute the mass not from the stress-energy tensor, but the space-time curvature.

Worrying about how and when the pressure changes isn't going to lead to anything useful in the non-stationary case. Perhaps someday someone will come up with a new approach - it's unlikely, considering how long the problem has been around, but possible. What works in this case is a different approach. It's worth learning this approach if one has the background, and it's not too productive to imagine that the useful approach that works in some important special case can be generalized to work when the conditions needed to make it work are not met.

The quasi-static case is an interesting one, but I've never seen anything written about it. I think what one can say is that if all the pressures are sufficiently close to equilibrium pressures, the errors one makes by assuming the system is static will be small and one can imagine that one might get the right answer even though the system is not quite static. However, this is a bit of an intuitive leap - it's probably true, but I haven't seen any formal discussion or proof of it, and there might be some hidden problem with the idea.
 
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  • #22
Pressure isn't conserved!

Consider a flat-space SET in cartesian coordinates. The divergence then has four terms, consisting of continuity equations for energy, x-momentum, y-momentum and z-momentum, each of which has a zero sum expressing conservation of that overall quantity.

If we consider a point in a rigid system which is at rest and has pressure in the x-direction (that is, across the yz-plane) then only the energy density and x-pressure terms are non-zero. The divergence tells us that the partial rate of change of x-momentum with time plus the partial rate of change of x-pressure with x is zero. (This means for example that if the pressure on one side of a tiny cell is higher than on the other, then the contents of that cell will be accelerated away from the higher pressure side, preserving momentum). It says NOTHING about the partial rate of change of x-pressure with time, so if it changed abruptly over a whole system this would not affect the divergence. (Neither would any sudden change to the other stress terms).

More realistically, if the pressure dropped to zero at a point in a rigid structure, then there would briefly be a pressure gradient which would propagate as a wave through the material. This gradient would be matched locally by a change in the rate of change of momentum (not a change in momentum itself) which would only last for a very brief time and cause a small amount of motion (depending on how elastic the material was) after which there would be a tension wave which would cancel out most of the change. (An elastic material might then oscillate about the original position). The net effect of this is that on the time scale of the larger system, the pressure has simply dropped to zero nearly simultaneously, on a time scale which does not allow any significant motion to develop.

As I explained in another post long ago, any energy involved in this tiny motion due to the sudden drop of pressure can easily be shown to be negligible compared with the gravitational potential energy term, as that would require the force involved in the pressure to act without decreasing through the entire distance between the gravitational source objects.
 
  • #23
Birkhoff's theorem says that the external field of a spherically symmetrical object is unaffected by spherically symmetrical internal changes. GR says that the pressure is a source term. However, the total pressure can vary at times when there is net acceleration occurring over macroscopic regions within the object.

That's the paradox, and as far as I can see the only possible resolution is that when the total pressure fluctuates, something else effectively compensates for the fluctuation, acting as a transient correction (positive or negative) to the source strength and maintaining the same overall external field.

I have now identified a simple quantity in Newtonian physics which exactly matches this "something else". If an equivalent quantity has the same effect in GR, then this would solve the paradox, which as far as I'm concerned would be a great relief.
 
  • #24
Jonathan Scott said:
Pressure isn't conserved!
Of course it isn’t. But it is part of the SET which has no divergence.

In analogy with charge, charge is conserved and the conservation of charge is given by the zero divergence of the density of charge-current. Similarly, energy-momentum is conserved and the conservation of energy-momentum is given by the zero divergence of the density of energy-momentum-stress. Pressure is a momentum “current density”. Neither current density nor pressure are conserved, they are part of the conservation laws for charge and energy-momentum respectively.

Jonathan Scott said:
if the pressure dropped to zero at a point in a rigid structure, then there would briefly be a pressure gradient which would propagate as a wave through the material.
This is the thing I was referring to above, that happens slowly on relativistic scales. It propagates at the speed of sound, which is far lower than c.

Jonathan Scott said:
the pressure has simply dropped to zero nearly simultaneously, on a time scale which does not allow any significant motion to develop.
I disagree completely. The time scale is exactly as long as is needed for exactly the right amount of momentum to develop. Work it out mathematically and you will see that it is guaranteed.

Jonathan Scott said:
GR says that the pressure is a source term. However, the total pressure can vary at times when there is net acceleration occurring over macroscopic regions within the object.

That's the paradox
So what? Current density is a source term for EM and it can vary too. What has one thing to do with the other? It is no paradox, it is simply a confusion on your part that you mistakenly believe that sources should have a property that they don’t.

Jonathan Scott said:
as far as I can see the only possible resolution
As far as I can see “it ain’t broke” and I am firmly of the “if it ain’t broke don’t fix it” persuasion. Hence my lack of enthusiasm or relief about this.
 
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  • #25
Dale said:
I disagree completely. The time scale is exactly as long as is needed for exactly the right amount of motion to develop. Work it out mathematically and you will see that it is guaranteed.
Sorry, but that's definitely wrong. This is simple classical mechanics.

I've already shown mathematically that the conservation laws do not prevent an abrupt change in pressure, for example if a support breaks or slips past an opposing one. Regardless of what happens in detail, any relative transient motion within each part on either side of the break at the time of release is only related to the mechanical energy stored as a result of the original pressure, which depending on the rigidity of the structure can be arbitrarily small, and the effect within each part is that the pressure drops abruptly. This may be slow on relativistic scales, but it is very fast compared with the overall motion of the parts.

The only significant change in the parts on either side of the break are they they suddenly start to accelerate towards each other with the total initial force on each half being the same as the force that was originally applying at the point of pressure. Neither their velocities nor their positions change immediately, but their accelerations change instantly.
 
  • #26
Jonathan Scott said:
I've already shown mathematically that the conservation laws do not prevent an abrupt change in pressure, for example if a support breaks or slips past an opposing one.
I disagree with calling it “abrupt” on relativistic scales. But again, so what? In EM the conservation laws do not prevent a change in current. But current is nonetheless clearly a source in EM. You erroneously think that source terms should be conserved. Fixing that error is the resolution here.
 
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  • #27
Dale said:
I disagree with calling it “abrupt” on relativistic scales. But again, so what? In EM the conservation laws do not prevent a change in current. But current is nonetheless clearly a source in EM. You erroneously think that source terms should be conserved. Fixing that error is the resolution here.
I have not called it "abrupt" on relativistic scales. It is abrupt compared with the overall motion. If I have a brick balanced on a brittle stick and the stick snaps, the brick will not have gained much velocity or moved very far by the time the pressure in the stick has reached zero.

I have not made my own assumption that source terms should be conserved. I have rather pointed out that Birkhoff's theorem says that the effective source strength is unaffected by internal changes. Total energy and momentum cannot be affected by internal changes, but total pressure can be temporarily affected, so there must be some compensating effect which preserves the constant external field.
 
  • #28
Jonathan Scott said:
If I have a brick balanced on a brittle stick and the stick snaps, the brick will not have gained much velocity or moved very far by the time the pressure in the stick has reached zero.
You say "will not have gained much velocity", but at each moment in time it will have gained exactly enough momentum that the SET will be divergenceless. It doesn't matter if, in your estimation, that is "much" or "little". It is the right amount for the physics to work out without paradox.

Jonathan Scott said:
I have rather pointed out that Birkhoff's theorem says that the effective source strength is unaffected by internal changes.
For spherical symmetry, yes, but not in general.

Jonathan Scott said:
Total energy and momentum cannot be affected by internal changes, but total pressure can be temporarily affected, so there must be some compensating effect which preserves the constant external field.
Total pressure doesn't even make sense. It is an intensive property, not an extensive property. You don't sum it up to get a total pressure.

At each location pressure contributes to the SET, and so does momentum density and energy density and stress. That is the source of gravity in GR, period. The EFE is absolutely clear about that: no ambiguity whatsoever.

Under the special case of spherical symmetry any internal changes in pressure are automatically compensated by internal changes in some other part of the SET (no divergence) such that the external field remains the same as per Birkhoff. That neither changes the fact that pressure is a source of gravity in GR nor does it introduce any true paradox nor is it even a general result that applies for non-spherical geometries.
 
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  • #29
Dale said:
You say "not have gained much velocity", but at each moment in time it will have gained exactly enough momentum that the SET will be divergenceless. It doesn't matter if, in your estimation, that is "much" or "little". It is the right amount for the physics to work out without paradox.
No, a change in pressure is matched by a change in the unbalanced force density, which determines the rate of change of momentum (and hence acceleration), not momentum or velocity or position. Pressure and unbalanced force density (and hence acceleration) can both change essentially instantaneously in a totally related way. This does not affect the divergence, provided that on average the spatial gradient of the pressure is unchanged, as the divergence only involves the gradient of the pressure, not the absolute value nor the rate of change with respect to time.

The issue of how a drop in pressure actually propagates within the separate part for a realistic material is independent of that acceleration change, and depends on the material and the construction. The propagation speed is likely to be related to the speed of sound in the material, and although the pressure may oscillate about the new (zero) value briefly, the time scale is likely to be tiny compared with the motion of what was originally supported by the pressure.
 
  • #30
Dale said:
For spherical symmetry, yes, but not in general.
That's why I'm using the spherical case to illustrate the paradox. To illustrate changes of pressure, I'm using more everyday examples as ways of achieving this with spherical symmetry are somewhat contrived.
 
  • #31
Dale said:
Total pressure doesn't even make sense. It is an intensive property, not an extensive property. You don't sum it up to get a total pressure.
I simply mean the total integral of the pressure over the system in the way being previously discussed (as in the Komar mass expression and the volume integral of 3p in the Newtonian case for isotropic pressure). I used "total" just to make it clear the pressure was temporarily changing, not just moving, but I guess I could have left some more words into be more accurate.
 
  • #32
Jonathan Scott said:
If I have a brick balanced on a brittle stick and the stick snaps, the brick will not have gained much velocity or moved very far by the time the pressure in the stick has reached zero.

But the contribution of the pressure in the stick to the source of gravity is also very small, so you don't actually know that the change in pressure (and the similar small change in energy density) is not balanced by the change in momentum density. You're just waving your hands and claiming it without actually doing the math. And, as I said before, your intuitive handwaving doesn't carry any weight if it tells you something that contradicts an exact mathematical theorem.

Jonathan Scott said:
a change in pressure is matched by a change in the unbalanced force density

No, it isn't. A change in pressure is balanced by a change in momentum (and energy) density. See below.

Jonathan Scott said:
This does not affect the divergence, provided that on average the spatial gradient of the pressure is unchanged, as the divergence only involves the gradient of the pressure, not the absolute value nor the rate of change with respect to time.

The divergence (more precisely the space components of the divergence) also include the spatial gradient of momentum density, which will be nonzero if the material is not at rest. So the pressure gradient cannot remain unchanged in this case.

The force density is the rate of change of momentum density with respect to time, so it enters into the divergence in the equation containing the time rate of change of energy density; it doesn't enter into the divergence equation where pressure appears at all, as you say. (And the rate of change of force density doesn't appear anywhere in this; the force density itself is a rate of change of an SET component.)
 
  • #33
Dale said:
Under the special case of spherical symmetry any internal changes in pressure are automatically compensated by internal changes in some other part of the SET (no divergence) such that the external field remains the same as per Birkhoff.
You're missing the point (and Tolman's point too). The divergence is not affected by pressure changes. As for my simple classical examples, a sudden pressure change can occur without any change to total energy or momentum. This will soon cause transfers of energy and momentum, but at the time it occurs the only thing which changes abruptly is that some material is being accelerated, and it takes time for any change in momentum and position to take effect. If the change is purely internal, then that acceleration will eventually be stopped and the system will get back into equilibrium with the same total integral of pressure as before.
 
  • #34
Jonathan Scott said:
I simply mean the total integral of the pressure over the system in the way being previously discussed (as in the Komar mass expression and the volume integral of 3p in the Newtonian case for isotropic pressure).

And since we know the covariant divergence of the SET is zero, we can also show that the Komar mass of the system remains unchanged as long as we can find a "world-tube" containing the system such that no stress-energy crosses the tube in either direction.
 
  • #35
PeterDonis said:
The divergence (more precisely the space components of the divergence) also include the spatial gradient of momentum density, which will be nonzero if the material is not at rest. So the pressure gradient cannot remain unchanged in this case.
If a support breaks, causing the pressure to drop, it IS still at rest initially.

At the microscopic level, I agree that what actually happens in a real material is that this takes a finite time to settle, but as I've said before, the amount of energy stored in a rigid stick or similar for a given compression force is related to the compression distance but the value of the integral of the pressure is equal to the same force times the length of the whole stick, so there is no way to transfer energy or momentum equivalent to the overall pressure integral.
 

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