Calculating Historical Positions of the Asteroid Belt's Orbit

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Discussion Overview

The discussion centers on the possibility of calculating the historical positions of the asteroid belt, particularly in relation to its outward movement and the effects of various forces, including the radiometer effect. Participants explore the feasibility of determining the asteroid belt's location 1,000 or 100,000 years ago and whether it ever shared an orbit with Earth.

Discussion Character

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

Main Points Raised

  • Some participants propose that orbits of large objects in the asteroid belt change very slowly, suggesting that extrapolating current orbits back 1,000 years could provide a good approximation.
  • Others argue that while the radiometer effect may have some influence, its impact is negligible compared to gravitational forces, particularly for larger asteroids like Ceres.
  • A participant mentions the Kirkwood gaps and suggests that the outer edge of the asteroid belt may indicate changes in Jupiter's orbit over time.
  • There is a discussion about the difference between the radiometer effect and solar sail effects, with some noting that the radiometer effect is minimal in space.
  • One participant questions the assumptions regarding the stability of the asteroid belt's position over billions of years and raises the possibility of cataclysmic events affecting its formation.
  • Another participant states that while current changes can be calculated and extrapolated, the historical appearance of the solar system cannot be directly observed.
  • It is noted that the Yarkovsky effect complicates calculations for individual asteroids due to various factors that are not well understood.

Areas of Agreement / Disagreement

Participants express differing views on the significance of the radiometer effect and the stability of the asteroid belt's orbit over time. There is no consensus on whether the historical positions of the asteroid belt can be accurately calculated, and multiple competing perspectives remain regarding the factors influencing its movement.

Contextual Notes

Limitations include the uncertainty surrounding the effects of the radiometer and Yarkovsky effects, as well as the assumptions about the stability of orbits over billions of years. The discussion highlights the complexity of modeling historical positions due to various unknowns and the chaotic nature of celestial mechanics.

jackpelham
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Is it possible to calculate the historical whereabouts of the asteroid belt, as it seems to be moving ever outward due to the radiometer effect? Can it be calculated, for instance, where it was 1,000 years ago? 100,000 years ago? Etc.

In particular, I'm curious as to whether the science is solid enough to pin down at what time (if any) it would have shared the same orbit with the Earth.

Thanks!

Jack
 
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Orbits of large objects (like everything detectable in the asteroid belt) usually change very slowly. The only way to get a significant modification is a fly-by at another object of at least comparable size. Remember: The astroid belt exists for 5 billion years now.

Therefore, just extrapolating the current orbits back 1000 years should give a good approximation for most objects. For 100 000 years, I would expect that the orbits of most objects had a similar shape, but the phase (the current position in this orbit) might be different, as it is more sensitive to small deviations.

If an object crossed the orbit of Earth in the past, it is quite unlikely that it is part of the asteroid belt now. This would require some sort of capture process there.
 
MFB,
Thanks for the reply. Do you believe, then, that the radiometer effect is NOT constantly pushing the orbit of the asteroid belt outward?
 
Any drift in asteroid belt also has the Kirkwood gaps to contend with...
http://en.wikipedia.org/wiki/Kirkwood_gap

IIRC, the 'soft' outer edge of the asteroid belt has been offered as evidence that Jupiter has increased its orbital radius during the early aeons of solar system. YMMV.
 
jackpelham said:
Do you believe, then, that the radiometer effect is NOT constantly pushing the orbit of the asteroid belt outward?
I do not say that there is no effect. I say that the effect is negligible. We had some thread about solar sails here, and if I remember correctly they feel a force of some Newtons per square kilometer. The largest object, Ceres, would feel a force of some 10^6 N then. As comparison, the gravitational pull between Ceres and Earth is of the order of 10^12 N (current value), and the force between Ceres and Jupiter is even stronger.
In addition, a constant central force with 1/r^2 does not change orbits at all, as it can be added to gravity.
 
Thanks, MFB. Isn't there a difference, though, in the solar sail effect and the radiometer effect?
Jack
 
There is - solar sails work in a vacuum as the radiation pressure is present there, the "radiometer effect" (at least what I found as definition) does not work in a perfect vacuum and is really small in space.
 
So what's the consensus here regarding whether historical positions of the asteroid belt can be calculated? Does anyone in physics suggest that the orbital radius of the belt has indeed moved over time? If so, what are the calculations about where it might have been at various intervals in the past?
 
If the whole belt has moved in a significant way, this is something which happened on the time-scale of billions of years or during the formation of the planets (where things were a bit more unstable in general).
 
  • #10
mfb said:
If the whole belt has moved in a significant way, this is something which happened on the time-scale of billions of years or during the formation of the planets (where things were a bit more unstable in general).

Thanks, MFB, but how do we know this? Are the assumptions at work here well-founded ones?

How do we know, for instance, that the asteroids were not created/introduced by some cataclysmic event that is outside the ordinary pattern of things that we observe today? Why must it have dated back to "the formation of the planets"? Indeed, if the planets were at one time "forming", then why didn't the material constituting the asteroids get pulled into those formations?

Nothing personal here in peppering you with these questions; I just want to be sure I'm not assuming anything unwarranted by the evidence or by sound physics.

Thanks again.
Jack
 
  • #11
Well, we cannot observe how our system looked some billion years ago. But it is possible to calculate the current changes in it and extrapolate both in the future and the past.

After the planets and the asteroid belt formed, they collected most of the material in the inner system. Since then, there is not enough mass in the inner solar system to modify the planetary orbits in a significant way. Jupiter had nearly the same orbit 3 billion years ago, and the other planets had similar orbits, too (luckily Pluto does not count as planet any more).

You can always create a scenario which leads to the current orbits with completely different initial conditions. But the chance that a lot of objects in chaotic orbits survive for ~2 billion years and arrange in the nice way we observe today afterwards is negligible. Unless you introduce some aliens, moving objects around ;).
 
  • #12
jackpelham said:
Is it possible to calculate the historical whereabouts of the asteroid belt, as it seems to be moving ever outward due to the radiometer effect? Can it be calculated, for instance, where it was 1,000 years ago? 100,000 years ago? Etc.

In particular, I'm curious as to whether the science is solid enough to pin down at what time (if any) it would have shared the same orbit with the Earth.

Thanks!

Jack

This is impossible to compute. Yarkovsky effects are basically impossible to compute for a single body, because it depends on mass, albedo, rotation rate, sphericity of the object, etc. -- most of which are only tentatively known for asteroids. Also the effect is very weak with the more massive asteroids, and even for the smaller ones, other perturbations can easily be larger.
 

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