timmdeeg said:
Thanks a lot for this excellent overview.
I understand so far.
How would you describe these fictitious forces in relation to tidal forces, if there is any? Is there any difference between these two kinds of forces at all in case the rigid bar, which prevents the two particles from geodesic deviation, is very short?
In the case of Newtonian gravity, you have a universal notion of time shared by all observers, and you can regard tidal force at some time t as being the the spatial gradient of this fictitious force. It's easiest to illustrate the concept with only one spatial dimension, which we'll call x. Letting f be the fictitious force (due to gravity) and x be the position of the bar, you can write that the tidal force is ##\partial f/\partial x##. To perform the partial derivative, you need to specify what you're holding constant, in this case t - we've eliminated y and z from the problem.
So, if you imagine you describe 1-d Newtonian space-time by t,x if you hold t constant, you can find the fictitious force from the tidal force by taking ##\int (\partial f / \partial x) \, dx## up to some constant of integration. By setting the boundary condition that there is no fictitious force on an object that's far away from the source of gravity, you can set this integration constant as well, and find the fictitious forces from the tidal forces by taking an integral.
So - that describes the relation between the fictitious forces and the tidal forces in a 1-d Newtonian space-time. Which is what I think you were asking (except for the 1d part) I thought about discussing the 3d aspects, but I'll save that for another post, and only if you actually want to know about it and ask - it gets involved and possibly off-track.
When you attempt to duplicate this argument in a manner compatible with relativity, you run into the obstacle that there is no such thing as "universal time" t. However, two observers that are sufficiently close together and moving at low velocities relative to another do share a common notion of time. The upshot of this is that the notion of the tidal force survives in relativity, but the notion of integrating the tidal force into a fictitious force doesn't really work as well.
There's one other wrinkle. You ask if geodesic deviation is exactly the same as tidal force. At least one textbook, MTW's "Gravitation", would suggest they are the same, and under most circumstances it's an excellent approximation. However, at sufficiently high accelerations, you might have difficulties For instance, if you mount an accelerometer on the bow and stern of a rigid accelerating spaceship in the flat space-time of SR, the two accelerometers won't read the same value, because the clocks at the bow and stern will tick at different rates. If you define tidal force by the difference in proper accelerations divided by the separation of the bow and stern, then you would have a very tiny tidal force by this definition in this case, while the geodesic deviation is zero. Possibly the authors of MTW had some way around this difficulty, but they didn't specify it in enough detail to know what it might be. So some caution is warranted.
A more serious issue is that tidal force, measured with a bar and a pair off accelerometers, can be induced by rotation. So the identification between the two totally fails if the observer is rotating, and partially fails (though not very seriously) if the observer is accelerating.
I must have missed something. To me this conclusion is surprising, because natural motion means no forces. If there are "fictitious forces", thinking of the two particles separated by a rigid bar, then we have no natural motion. As I understood your approach, it leads from natural motion to fictitious forces. Why then should we forget about them?
One of the motivations of General relativity was to explain the identity of inertial mass with gravitational mass - something that was just a coincidence in Newtonian theory. The basic idea is that if we assume that inertia and gravity have the same origin, this unexplained equivalence becomes explained. The obvious way to unite the two is to describe gravity as an inertial force. But a better way to equate the two is to avoid using inertial forces for the reasons I discussed, and identify tidal gravity with geodesic deviation.
May I ask what your intuition tells you regarding the position of the "locus of no acceleration" on the rod?
In a nutshell, my first thought is that "the locus of no acceleration" isn't worded very well. What is the acceleration being measured relative to? So I would rephrase the question as "the locus of points with no relative acceleration to an observer in natural motion". My basic intuition is that under most static circumstances, the center of the bar wouldn't accelerate relative to an observer in natural motion. But the notion of a static bar is probably not quite right. If the bar is actually falling, it'll get closer to the object it's falling towards as time progresses. This means the stretching of the bar will change as it gets closer to the objet it's falling towards, meaning that the situation isn't exactly static. Being non-static, the bar will probably vibrate. If the bar is perfectly symmetrical, it should vibrate about its center. But if the bar isn't symmetrical - there point with no acceleration relative to a geodesic might vary periodically or semi-peridiocally with time due to the vibration.
Another thing that I worry about is gravitational radiation. If the bar isn't just composed of test particles, but has gravity of its own, the solution to Einstein's equations may result in gravitational radiation being emitted as the bar falls. The intuition is that the momentum carried away by the gravitational radiation will affect the motion of the bar, making it's center not follow a geodesic. But I haven't worked it out. Usually , though, this effect would be tiny.
If I see it correctly, the r-coordinate of the COM of the rod in radial free fall is not the arithmetic mean of the r-coordinates of top and the bottom. Thus the difference top between COM is smaller than the difference between COM and bottom. If so, shouldn't one expect larger "fictitious forces" in the lower part of the rod? Somewhere they change sign and cancel each other, but where?
That happens as well, but I think I've already discussed that. Basically my position is that's a second order effect, and when you take the limit of a short enough bar, you can make the importance of the effect as small as you like. Since my previous posts haven't seem to communicated this, I'd suggest trying it for yourself. Consider two 1 kg weights connected by a massless rigid, 10 meter bar, which is instantaneously at rest over the surface of an idealized Earth. Work out the total net force on the bar, the total mass of the bar (that's easy, it's 2kg), and the accleration (force/mass) of the assembly. Because the assembly is rigid, this gives you the acceleration of all points on the assembly. Compare this acceleraton to the acceleration of freely falling mass at the midpoint of the bar. Repeat for 1 meter bars, and .1 meter bars.
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You can use M=6*10^24 kg, r = 6.4*10^6 meters for the Earth - or whatever you like, actually. It's probably the most convenient if you keep the center of the bar at r=6.4*10^6 meters, so the ends of the bar would be at r+e, r-e, where e = 5 meters, .5 meters, and .05 meters.
Chose a suitable scale for acceleration where the ends of the bar for the 10 meter bar fall within the scale, and plot the free-fall accelerations of the end of the bar, the average acceleration of the entire bar (total force / total mass), and the acceleration of a freely falling mass at the midpoint (6*10^4) meters on this scale. See what happens as the length of the bar decreases from 10 meters to .1 meters.
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Actually, if you want something visible discrpeancies, it'd be more informative to try a 1000 km bar (e=500000) for the long bar, and a 200km bar for the "short" bar.