Painleve chart for FRW spacetime

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In summary, the conversation discusses a Painleve chart for FRW spacetime and how it can be used to visualize the worldlines of "comoving" observers. The conversation also delves into the underlying equations and principles of this chart, including the "gravitational redshift" experienced by observers and the existence of a horizon at r=3/2t. However, it is later clarified that the horizon is not a complete causal boundary, unlike a black hole's event horizon.
  • #1
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In a thread a while back, Mentz114 posted a Painleve chart for FRW spacetime; here's the link to the post:

https://www.physicsforums.com/showpost.php?p=2985307&postcount=60

He posted the metric in Cartesian coordinates, and I've derived a corresponding metric for polar coordinates. (I'm doing this so I can then see what the worldlines of "comoving" observers look like in this chart.) [Edit: originally I thought my answer looked different than what I expected based on Mentz114's post, but I made an error in deriving it; the error is now corrected below.]

Here's what I'm getting: I start with the FRW metric for k = 0 (i.e., flat spatial slices) and with a matter-dominated equation of state, so the scale factor is proportional to [itex]t^{\frac{2}{3}}[/itex]. (Mentz114 didn't say so, but it looks to me like that's the equation of state for the metric he wrote down.) I pick units so that the constant of proportionality for the scale factor is 1 (i.e., a(t) = 1 at t = 1), so

[tex]ds^{2} = - dt^{2} + t^{\frac{4}{3}} \left( dr'^{2} + r'^{2} d\Omega^{2} \right)[/tex]

We want a coordinate transformation that will make the purely spatial part of the metric static (i.e., independent of t). I try this:

[tex]r' = t^{- \frac{2}{3}} r[/tex]

(leaving all other coordinates the same), which gives

[tex]dr' = t^{- \frac{2}{3}} dr - \frac{2 r}{3} t^{- \frac{5}{3}} dt[/tex]

Substituting into the metric gives, after some algebra,

[tex]ds^{2} = - dt^{2} \left( 1 - \frac{4 r^{2}}{9 t^{2}} \right) - \frac{4 r}{3 t} dt dr + dr^{2} + r^{2} d\Omega^{2}[/tex]

If the above is correct, then the worldlines of comoving observers are easy. We haven't changed the t coordinate so for comoving observers we want [itex]ds^{2} = - dt^{2}[/itex]. That gives:

[tex]\frac{dr}{dt} = \frac{2 r}{3t}[/tex]

Does all this look correct?
 
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  • #2
It looks OK to me.

From the line element I get the metric as (just checking)

[tex]
\pmatrix{-1+\frac{4\,{r}^{2}}{9\,{t}^{2}} & -\frac{2\,r}{3\,t} & 0 & 0\cr -\frac{2\,r}{3\,t} & 1 & 0 & 0\cr 0 & 0 & {r}^{2} & 0\cr 0 & 0 & 0 & {r}^{2}\,{sin\left( \theta\right) }^{2}}
[/tex]

and this gives the right Einstein tensor.
 
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  • #3
Thanks! So it seems like the general principle of a Painleve-type chart is that the "Painleve observers" move at velocity [itex]\beta = \frac{dr}{dt}[/itex], and the line element looks like:

[tex]ds^{2} = - dt^{2} \left( 1 - \beta^{2} \right) - 2 \beta dt dr + dr^{2} + r^{2} d\Omega^{2}[/tex]

Also that the coordinate time in this chart *is* the proper time for Painleve observers, which in the FRW case are the "comoving" observers (I had speculated in the other thread that this was *not* the case, but it appears I was wrong).
 
  • #4
It's ingenious to derive it by requiring the S3 hyperslices. I tried doing it by calculating the acceleration vector for a general 4-velocity and setting it to zero and failed. This was some time ago and I don't remember why.

You're right about the general principle, which is to replace the spatial coord by one corrected with [itex]\beta \tau[/itex] so it becomes comoving and [itex]t=\tau[/itex].[I corrected the typo in my post , g00 had the wrong sign.]

It is possible to derive the metric by the geodesic route. Requiring that [itex]dt/d\tau=1[/itex] means that our observer has 4-velocity [itex]u^\mu=(1,\beta,0,0)[/itex] (mixing tensor and vector notation). Calculating the acceleration [itex]u_{\mu;\nu} u^\nu[/itex] gives a first-order simultaneous differential equation.
[tex]
\frac{d}{d\,t}\,\beta =-\beta\,\left( \frac{d}{d\,r}\,\beta\right) -\frac{2\,r}{9\,{t}^{2}}
[/tex]
The solution is your result for [itex]\beta[/itex]. But this much longer than your derivation.
 
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  • #5
Mentz114 said:
It's ingenious to derive it by requiring the S3 hyperslices.

Do you mean the FRW spacetime with k = 1 (i.e., closed universe, assuming zero cosmological constant)? For that case the "comoving" spatial hyperslices are not flat. Does that spacetime admit any slicing with flat spatial slices?
 
  • #6
PeterDonis said:
Do you mean the FRW spacetime with k = 1 (i.e., closed universe, assuming zero cosmological constant)? For that case the "comoving" spatial hyperslices are not flat. Does that spacetime admit any slicing with flat spatial slices?

I'm sorry my remark "It's ingenious to derive it by requiring the S3 hyperslices" is not relevant and has sowed confusion.

It's interesting that in the comoving coords you derived the 'gravitational' redshift is the familiar [itex]1/\sqrt{1-\beta^2}[/itex].
 
  • #7
Mentz114 said:
It's interesting that in the comoving coords you derived the 'gravitational' redshift is the familiar [itex]1/\sqrt{1-\beta^2}[/itex].

Yes, it looks like that is a general feature of Painleve charts since g_tt always assumes the same form in terms of beta. Another way of expressing this would be that "static" observers in this chart (i.e, observers who hold station at a constant r, theta, phi) will have to accelerate to hold station, with an acceleration that increases with r, and the "gravitational redshift" they experience can be thought of as due to their acceleration relative to the observer at r = 0.

Also, the "static" observers will see the "comoving" observers falling past them with a speed beta. Since beta goes to 1 when r = 3/2 t, there is a "horizon" there, and beyond that horizon there are no static observers, i.e., no observers holding station at constant r, theta, phi (because they would have to move faster than light), and no observers beyond the horizon can send signals back to the region "above" it. All very interesting parallels to a black hole spacetime.
 
  • #8
PeterDonis said:
no observers beyond the horizon can send signals back to the region "above" it.

On thinking this over, I realized it's not correct. I should have realized that it can't be, because there are "comoving" observers who emerge from "behind" the horizon! This follows easily from the formulas I derived: the horizon is the line r = 3/2 t, but "comoving" worldlines have the equations

[tex]r = r_{0} t^{\frac{2}{3}}[/tex]

where r_0 is the radius of that particular worldline at t = 1. (You can see from my derivation that r_0 is also the "r" coordinate of that particular "comoving" observer in the standard FRW chart.) For any value of r_0, there is some value of t at which the corresponding comoving worldline intersects the horizon; before that time t, that comoving observer is behind the horizon, but after it, he has emerged from it.

So the horizon is not a complete causal boundary in the spacetime the way a black hole horizon is.
 

Related to Painleve chart for FRW spacetime

What is a Painleve chart for FRW spacetime?

A Painleve chart for FRW spacetime is a coordinate system used to describe the evolution of the universe in the framework of the Friedmann-Robertson-Walker (FRW) metric. It is a transformation of coordinates that simplifies the mathematical equations describing the expansion of the universe in the FRW model.

Why is a Painleve chart useful in studying FRW spacetime?

A Painleve chart is useful because it allows us to simplify the complex equations of the FRW model and make it easier to analyze and understand the behavior of the universe. It also helps us to identify important features of the universe, such as the expansion rate and curvature, which can have significant implications for our understanding of the cosmos.

How is a Painleve chart constructed?

A Painleve chart is constructed by performing a coordinate transformation on the standard FRW coordinates, which are comoving coordinates that move with the expansion of the universe. This transformation is chosen to eliminate singularities in the equations and make them easier to solve. The resulting coordinates are called Painleve coordinates.

What are the limitations of using a Painleve chart for FRW spacetime?

One limitation of using a Painleve chart is that it only works for certain types of FRW metrics, namely those with a flat spatial curvature. It also does not account for the effects of dark energy or dark matter, which are important components of the universe but are not included in the standard FRW model.

How does a Painleve chart help us understand the evolution of the universe?

A Painleve chart helps us understand the evolution of the universe by providing a simplified mathematical framework for studying the FRW model. It allows us to identify important features and behaviors of the universe, such as the expansion rate and curvature, and make predictions about its future evolution. It also helps us to compare our observations of the universe to theoretical models and test our understanding of its origins and development.

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