Motivation for Theta = Pi/2 on Wald GR p138

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Discussion Overview

The discussion revolves around the justification for setting the angle ##\theta = \pi/2## in the context of geodesics in the Schwarzschild metric, as presented in Wald's General Relativity. Participants explore the implications of symmetry in the metric and its effects on geodesic motion, examining both theoretical and mathematical aspects of the argument.

Discussion Character

  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • Some participants express understanding of the simplification to equatorial geodesics in Newtonian mechanics and seek clarity on its application in general relativity.
  • One participant suggests that Wald's argument relies on the rhetorical question of directionality, implying that if initial conditions do not favor an increase or decrease in ##\theta##, the symmetry suggests a contradiction in any directional argument.
  • Another participant references Hartle's argument regarding planar motion starting from ##\phi = 0##, leading to the conclusion that the motion can be confined to the plane ##\theta = \frac{\pi}{2}##.
  • A different perspective introduces isotropic coordinates, arguing that the conservation of angular momentum in the Schwarzschild metric leads to trajectories lying in a plane, allowing the choice of ##\theta = \frac{\pi}{2}##.
  • Some participants reiterate confusion about Wald's argument, emphasizing the role of parity reflection symmetry and its implications for geodesic solutions, particularly at the fixed point of ##\theta = \frac{\pi}{2}##.
  • There is a discussion about the implications of symmetry leading to distinct solutions and how this relates to the behavior of geodesics in the equatorial plane.

Areas of Agreement / Disagreement

Participants express varying levels of understanding and interpretation of Wald's argument, indicating that there is no consensus on the clarity or validity of the reasoning provided. Multiple competing views on the justification for restricting to the equatorial plane remain present.

Contextual Notes

Participants note the dependence on the symmetry properties of the Schwarzschild metric and the implications of initial conditions on geodesic motion. The discussion highlights the complexity of the argument without resolving the underlying mathematical details or assumptions.

strangerep
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On p138 of Wald's General Relativity, 4th para, he says:

Wald said:
[...] First, we note that because of the parity reflection symmetry, ##\theta \to \pi - \theta##, of the Schwarzschild metric, if the initial position and tangent vector of a geodesic lie in the "equatorial plane" ##\theta = \pi/2##, then the entire geodesic must lie in this "plane." Since every geodesic can be brought to an initially (and hence everywhere) equatorial geodesic by a rotational isometry, this means that without loss of generality we may restrict attention to study of the equatorial geodesics, and we shall do so.
Firstly, I already understand (of course) that this sort of simplification is easy and immediate in Newtonian mechanics, since conservation of angular momentum always occurs in central force problems (the proof is just a few lines) and one can re-orient the coordinates so that motion occurs in the plane perpendicular to the angular momentum axis.

Secondly, in GR, if one actually computes the connection coefficients for Schwarzschild, to write down the geodesic equations explicitly, one then sees immediately that ##\theta=\pi/2## (say) is a convenient choice that one can make without loss of generality.

But I don't follow Wald's particular argument, i.e., that the symmetry ##\theta\to \pi-\theta## allows one to conclude that "if the initial position and tangent vector of a geodesic lie in the equatorial plane ##\theta=\pi/2##, then the entire geodesic must lie in this plane.''

What am I missing?
 
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Isn't he just using the "which way would it go" rhetorical question? If your particular initial conditions don't pick out a direction of increase/decrease for ##\theta## the symmetry of the metric implies any argument for "##\theta## will increase" must apply equally to "##\pi-\theta## will increase", so such an argument must be self-contradictory?
 
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I think Hartle argued this for initially ##\phi =0## to show the motion is planar. And then took the plane to be ##\theta = \frac \pi 2##.
 
I think the most simple argument is to use "isotropic coordinates" first. There the Schwarzschild line element reads
$$\mathrm{d} s^2 =\frac{[1-m/(2 R)]^2}{[1+m/(2R)]^2} c^2 \mathrm{d} t^2 - [1+m/(2R)]^4 \mathrm{d} \vec{x}^2,$$
where ##R=|\vec{x}|^2## and ##\vec{x}=(x^1,x^2,x^3)##.

The square-form Lagrangian for the geodesic reads
$$L=\frac{1}{2} \dot{s}^2,$$
where the dot denotes the derivative wrt. an arbitrary world-line parameter, ##\lambda##, which is automatically affine, because since ##L## doesn't depend explicitly on ##\lambda##, i.e., ##H=p_{\mu} q^{\mu}-L=L=\text{const}##, where ##p_{\mu} = \partial_{\dot{q}^{\mu}} L##, and for a massive particle we can set ##\lambda=\tau##, such that ##(\mathrm{d}_{\tau} s)^2=c^2##.

It's now also manifest that the solution is rotationally symmetric, i.e., the Lagrangian is invariant under rotations ##\vec{x}'=\hat{R} \vec{x}## with ##\hat{R} \in \mathrm{SO}(3)##. This implies that the angular momentum ##\vec{x} \times \vec{p}## is conserved as in Newtonian physics, and thus the trajectory is in a plane.

Since you know that the trajectory is in a plane, you can make the angular momentum pointing in ##x^3## direction, which means that ##\vartheta=\pi/2=\text{const}## for the usual spherical coordinates,
$$\vec{x}=R \begin{pmatrix} \cos \varphi \sin \vartheta \\ \sin \varphi \sin \vartheta \\ \cos \vartheta \end{pmatrix},$$
Since you get from the isotropic coordinates to the Schwarzschild coordinates by only transforming ##R## to ##r##, this also holds in Schwarzschild coordinates.
 
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strangerep said:
I don't follow Wald's particular argument, i.e., that the symmetry ##\theta\to \pi-\theta## allows one to conclude that "if the initial position and tangent vector of a geodesic lie in the equatorial plane ##\theta=\pi/2##, then the entire geodesic must lie in this plane.''

What am I missing?
The parity reflection symmetry in general means that we can take any solution to the geodesic equation and substitute ##\theta \to \pi - \theta## (and make all other changes that go along with this, such as changing derivatives with respect to ##\theta##) to get another solution. In general this will yield a pair of distinct solutions.

However, the particular value ##\theta = \pi / 2## is a fixed point of the parity reflection symmetry, which means that the symmetry takes any solution to the geodesic equation whose initial conditions are entirely in the plane ##\theta = \pi / 2## into itself. That can only be the case if the solution lies entirely in that plane.

Ibix said:
If your particular initial conditions don't pick out a direction of increase/decrease for ##\theta## the symmetry of the metric implies any argument for "##\theta## will increase" must apply equally to "##\pi-\theta## will increase", so such an argument must be self-contradictory?
If you add the qualifier that this argument only works for ##\theta = \pi / 2##, then I think it amounts to the same argument I gave above.
 
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PeterDonis said:
The parity reflection symmetry in general means that we can take any solution to the geodesic equation and substitute ##\theta \to \pi - \theta## (and make all other changes that go along with this, such as changing derivatives with respect to ##\theta##) to get another solution. In general this will yield a pair of distinct solutions.

However, the particular value ##\theta = \pi / 2## is a fixed point of the parity reflection symmetry, which means that the symmetry takes any solution to the geodesic equation whose initial conditions are entirely in the plane ##\theta = \pi / 2## into itself. That can only be the case if the solution lies entirely in that plane.
Thank you! (And thanks also to @Ibix , @vanhees71 and @PeroK.)

I must be getting older than I realize. :oldfrown:
 
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