How do we apply the Friedman solution to a fluid with constant pressure and energy density?

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The discussion focuses on applying the Friedman solution to a fluid with constant pressure and energy density, starting from the Robertson-Walker metric. Participants explore how to derive the scale factor a(t) by inserting the stress-energy tensor of a perfect fluid into the Einstein field equations. The conversation highlights the significance of the curvature constant k, which can take values of -1, 0, or +1, indicating different geometric properties of the universe. Additionally, it emphasizes the relationship between the fluid's rest frame and the components of the stress-energy tensor, ultimately leading to a diagonal form that represents energy density and pressure. The participants conclude that the process is manageable but requires careful consideration of the underlying mathematics.
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Looking at the Friedman solution for a fluid with a given pressure and energy density, we have:

H^2 = \left(\frac{\dot{a}}{a}\right)^2 = \frac{8 \pi G}{3}\rho + \frac{\Lambda}{3} - \frac{k}{a^2}

Would someone mind walking me through how we arrive at a?

Rev Prez
 
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From the assumption that the universe is isotropic we are lead immediately to the Robertson-Walker metric:

ds^2 = c^2dt^2 + a(t) [ dr^2 + S_k(r) d\Omega^2 ]

K is a constant either -1, 0, +1.

If k = +1 , the function S(r) = sin(r).

If k = -1, S(r) = sinh(r).

k = 0 implies S(r) = r.

By the way, omega is shorthand for some angular metric components, look it up under "hypersphere" at www.mathworld.com

Anyway, from this metric, along with the stress-energy tensor for a perfect fluid:

T_{\alpha\beta} = P g_{\alpha\beta} - (P - \rho)U_\alpha U_\beta

(P is pressure, u is four velocity, rho is density, and g is the metric tensor)


We insert both of these guys into the einstein field equations (remember the einstein tensor G is just a bunch of derivatives of the RW metric):

G_{\alpha\beta} = \frac{8 \pi G}{c^2} T_{\alpha\beta}

Then solve for a(t) to get the freidmann equation. It is all very do-able, but it takes at least half an hour.
 
Crosson said:
From the assumption that the universe is isotropic we are lead immediately to the Robertson-Walker metric:

ds^2 = c^2dt^2 + a(t) [ dr^2 + S_k(r) d\Omega^2 ]

K is a constant either -1, 0, +1.

If k = +1 , the function S(r) = sin(r).

If k = -1, S(r) = sinh(r).

k = 0 implies S(r) = r.

By the way, omega is shorthand for some angular metric components, look it up under "hypersphere" at www.mathworld.com

Okay.

1. d\Omega = d\theta^2 + \sin^2(\theta)d\phi.

2. Shouldn't S_k(r) take on the same units as dr (as d\Omega is dimensionless)? In which case, as is indicated http://en.wikipedia.org/wiki/Friedmann-Lema%EEtre-Robertson-Walker, we should multiply by the mag of the curvature radius. I'm not being facetious, but its easy to get lost when you're not quite clear on the unit constant convention used.

3. The codomain of k is restricted to -1, 0, 1, or is this just a convenient choice since we're more or less concerned with whether the large scale structure is closed, flat or hyperbolic?

Anyway, from this metric, along with the stress-energy tensor for a perfect fluid:

T_{\alpha\beta} = P g_{\alpha\beta} - (P - \rho)U_\alpha U_\beta

(P is pressure, u is four velocity, rho is density, and g is the metric tensor)

Now this is where I should've started asking questions. What process do you go through starting with "homogenous, isotropic universe" to get a tensor description of it? I understand intuitively what it means, but I would love to know how you reason out a perfect fluid's formal representation.

I can guess that:
1. Because FLRW is for an isotropic, homogenous universe, P and \rho are assumed constant...

...and...

2. for an observer at rest with the fluid, the equation reduces to T_{\alpha\beta} = P g_{\alpha\beta}

But where do you get (P - \rho)?

We insert both of these guys into the einstein field equations (remember the einstein tensor G is just a bunch of derivatives of the RW metric):

G_{\alpha\beta} = \frac{8 \pi G}{c^2} T_{\alpha\beta}

Then solve for a(t) to get the freidmann equation. It is all very do-able, but it takes at least half an hour.

Thanks for your help. I'll digest this and get back to the thread if I have more questions.

Rev Prez
 
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It is much easier to look at the stress energy tensor for a perfect fluid in matric form than as:

T_{\alpha\beta} = P g_{\alpha\beta} - (P - \rho)U_\alpha U_\beta

But I don't know how to Latex format a matrix. I will describe the components in the rest frame of the fluid:

T_{00} = \rho c^2

T_{11} = P_x

T_{22} = P_y

T_{33} = P_z

And the rest (off diagonal) are zero. Remember that U is the four velocity, and in the rest frame of the fluid this is equal to c in the time direction. Also, remember pressure is stress.

3. The codomain of k is restricted to -1, 0, 1, or is this just a convenient choice since we're more or less concerned with whether the large scale structure is closed, flat or hyperbolic?

Yes, an isotropic (simply connected) shape can only have one of three curvatures.
 
Crosson said:
Remember that U is the four velocity, and in the rest frame of the fluid this is equal to c in the time direction. Also, remember pressure is stress.

Okay, I got it. So check me here. In the fluid's rest frame, which a choice of units c = 1, the equation gives us just the energy density, correct?

Rev Prez
 
Last edited:
Okay, I got it. So check me here. In the fluid's rest frame, which a choice of units c = 1, the equation gives us just the energy density, correct?

What are you using for g ? In the rest frame of the particle the metric tensor (g) is simply the flat metric of minkowski spacetime (16 components, all of them zero except g00 = -1 and g11=g22=g33=1).

U is a vector which is all zero accept for the zeroth component (time) which is c = 1.

Using these and the abstract equation, you should be able to construct the components of the stress-energy tensor of a perfect fluid (in its rest frame). (the diagonal terms I described.)
 
Crosson said:
What are you using for g ?

Just g00 = -1, everything else set to zero.

U is a vector which is all zero accept for the zeroth component (time) which is c = 1.

Since

g_{\alpha\beta} = -U_{\alpha}U_{\beta

in the rest frame,

T_{\alpha\beta} = Pg_{\alpha\beta} - (P - \rho)U_{\alpha}U_{\beta}

reduces to

T_{\alpha\beta} = \rho(U_{\alpha}U_{\beta})

where all that remains is the energy density component in the time direction.

Right?

Rev Prez
 
I think I got it.

You will end up with diag(\rho, p, p, p) for constant pressure and energy density and with c = 1. The U_{\alpha}U_{\beta} term will give us the energy density in the time dimension and the metric term will give us the pressure in space.

Rev Prez
 

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