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GR Sessions 5: Gravitation

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GR Sessions 5: Gravitation

Wednesdays October 31, 2012

1. Rotation. Consider the ‘rotating metric’

ds2= − 1 − Ω2 x2+ y2 dt2+ 2Ω(y dx − x dy)dt + dx2+ dy2+ dz2 ,

which represents a coordinate system spinning about the z-axis with angular velocity Ω in the clockwise direction. Prove that this metric is flat by way of a coordinate transformation.

2. 2d gravity. Similar to the gauge invariance of electromagnetism Aµ → Aµ+∂µλ, General relativity has a similar symmetry of the equations of motion called diffeomorphism invariance:

gµν → gµν+ ∂µξν+ ∂νξµ , where ξµ is an arbitrary vector.

(a) Use this to argue that, in two spacetime dimensions, we can write gµν = eφηµν. (b) What does this imply about the Riemann tensor (see §3.9 of Carroll), and why?

(c) Use this to show that the Einstein tensor vanishes in two dimensions.

3. Carroll 4.1 The Lagrange density for electromagnetism in curved space is L =√

−g −14FµνFµν+ AµJµ , where Jµ is the conserved current

(a) Derive the energy momentum tensor by functional differentiation with respect to the metric.

You can assume that the AµJµ term does not contribute to the energy-momentum tensor.

(b) Consider adding a new term to the Lagrangian,

L0= β RµνgρσFµρFνσ .

How are Maxwell’s equations altered in the presence of this term? Einstein’s equation? Is the current still conserved?

4. Carroll 4.3 The four-dimensional δ-function on a manifold M is defined by Z

M

F (xµ) δ(4)(xσ− yσ)

√−g

√

−gd4x = F (yσ) ,

for an arbitrary function F (xµ). Meanwhile, the energy-momentum tensor for a pressureless perfect fluid (dust) is

Tµν = ρ UµUν ,

where ρ is the energy density and Uµ is the four-velocity. Consider such a fluid that consists of a single particle travelling on a world line xµ(τ , with τ the proper time. The energy momentum tensor for this fluid is then given by

Tµν = m Z

M

 δ(4)(xσ− yσ)

√−g

 dxµ

dxν dτ dτ ,

where m is the rest mass of the particle. Show that covariant conservation of the energy-momentum tensor, ∇µTµν = 0, implies that xµ(τ ) satisfies the geodesic equation.

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