High School Can a Gravitational System be Treated as a Single Curved Spacetime?

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SUMMARY

The discussion centers on whether a gravitational system, such as the Earth and Moon, can be treated as a single curved spacetime. It is established that at a sufficient distance, the gravitational field of such a system can be approximated as that of a point mass located at the barycenter. However, for practical applications like rocket travel between the two bodies, this approximation fails. The conversation also touches on the challenges of applying these concepts to atomic systems, where the gravitational effects are negligible and difficult to measure accurately.

PREREQUISITES
  • General Relativity (GR) principles
  • Newtonian gravity fundamentals
  • Understanding of barycenter in gravitational systems
  • Basic knowledge of atomic structure and forces
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  • Study the implications of General Relativity on multi-body gravitational systems
  • Explore the concept of barycenter and its applications in celestial mechanics
  • Investigate the limitations of Newtonian gravity in small-scale systems
  • Learn about gravitational field measurements and their precision requirements
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Astrophysicists, physicists studying gravitational systems, and anyone interested in the applications of General Relativity in both large-scale and atomic contexts.

BeedS
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Hey, if I take two objects for Example the Earth and Moon and treat them as a gravitational bound “system”. The Earth and Moon have their own local curves in spacetime. Can I use/treat the whole “system” as a curve in spacetime? For example, a curve that includes all objects of the “system” mass/gravity merged/added and is strongest at the “systems” Barycenter.
 
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Depends what for. At a large enough distance the field will be pretty much identical to the field of a point mass at the barycentre, although that mass may or may not be well approximated by the sum of the independent masses (it would be ok for Earth and Moon). So in that case, yes you could. If you want to fly rockets from one object to the other, no, not even close.
 
Ibix said:
At a large enough distance the field will be pretty much identical to the field of a point mass at the barycentre
If I take objects for Example the particles of an atomic system and treat them as a gravitational bound “system”… ? ...is the atomic system far enough? :oops:

Ibix said:
If you want to fly rockets from one object to the other, no, not even close.
Yes, I was thinking for external objects located outside the system, interacting with the system.
 
BeedS said:
If I take objects for Example the particles of an atomic system and treat them as a gravitational bound “system”… ? ...
You mean the gravitational field of a single atom? It's too tiny for is to know if GR models it correctly. Assuming it does, though, you'd need such incredibly precise measurements to detect the field that it's impossible to say how close you could go and still treat it as a point source.

Note that an atom is not gravitationally bound. Atoms are held together by strong forces in the nucleus and electromagnetic forces between the nucleus and electrons.
BeedS said:
Yes, I was thinking for external objects located outside the system, interacting with the system.
Basically, any system will look like a point source when you're far enough from it. But what "far enough" means in practice depends on how precisely you're measuring. For a simple example, consider the case of the Sun, mass ##M_S## and distance ##R## away from you, and the Earth, mass ##M_E## and distance ##R+r## away from you. We'll have you, the Earth and the Sun in a straight line so we can be lazy about vectors and use Newtonian gravity, because that's valid way before pretending the Earth and Sun are a single point is valid.

The gravitational acceleration you feel is $$\begin{eqnarray*}
g&=&\frac{GM_S}R+\frac{GM_E}{R+r}\\
&=&\frac{GM_S}R+\frac{GM_E}{R}\frac{1}{1+r/R}\\
&=&\frac{GM_S}R+\frac{GM_E}{R}\left(1-\frac{r}{R}+\frac{r^2}{R^2}-\frac{r^3}{R^3}+\ldots\right)\\
&=&\frac{G(M_S+M_E)}R-\frac{GM_E}{R}\left(\frac{r}{R}-\frac{r^2}{R^2}+\frac{r^3}{R^3}-\ldots\right)
\end{eqnarray*}$$Whether you can detect the difference between that and ##G(M_S+M_E)/R^2## depends on whether the experiment you are doing is far enough away that your measurement error is bigger than that last term in the brackets - that is that your distance from the Sun, ##R##, is so much larger than the Earth-Sun distance, ##r##, that all those terms in the brackets are so nearly zero you don't care.
 
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Ibix said:
You mean the gravitational field of a single atom? It's too tiny for is to know if GR models it correctly
It's too tiny to tell if Newtonian gravity models it correctly too.
 
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In an inertial frame of reference (IFR), there are two fixed points, A and B, which share an entangled state $$ \frac{1}{\sqrt{2}}(|0>_A|1>_B+|1>_A|0>_B) $$ At point A, a measurement is made. The state then collapses to $$ |a>_A|b>_B, \{a,b\}=\{0,1\} $$ We assume that A has the state ##|a>_A## and B has ##|b>_B## simultaneously, i.e., when their synchronized clocks both read time T However, in other inertial frames, due to the relativity of simultaneity, the moment when B has ##|b>_B##...

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