Proving Geodesics in Hyperbolic Geometry

In summary: Yep, you are correct. So what about the other terms?Yep, you are correct. So what about the other terms?0 = -r\cos \theta \sin \theta - \frac{2}{r \sin \theta} \cdot r \cos \theta \sin \theta \cdot r \cos \theta \sin \theta + \frac{1}{r\sin \theta} \cdot r^2 \cos^2 \theta + x_0^2 \sin^2 \theta 0 = -r\cos \theta \sin \theta - 2r \cos^2 \theta \sin^2 \theta + r \cos^2 \theta + x_0
  • #1
ChrisJ
70
3
Given ##ds^2 = y^{-2}(dx^2 + dy^2)##, I am trying to prove that a demicircle centred on the x-axis, written parametrically as ##x=r\cos\theta + x_0 ## and ##y= r \sin \theta ## are geodesics. Where ##r## is constant and ##\theta \in (0,\pi)##

I have already found the general form of the geodesic equation for this metric by finding the christoffell symbols,

[tex]
0 = \frac{d^2x}{ds^2} - \frac{2}{y}\frac{dx}{ds}\frac{dy}{ds} \\
0 = \frac{d^2y}{ds^2} - \frac{1}{y} \left( \frac{dy}{ds} \right)^2 + \frac{1}{y}\left( \frac{dx}{ds} \right)^2
[/tex]Then I was not exactly sure where to go from here, but just started spitballing,

[tex]
dx = -r \sin \theta d\theta\\
dy = r \cos \theta d\theta\\
ds^2 = \left( \frac{1}{r^2 \sin^2 \theta } \right) \left( -r^2 \sin^2 \theta d\theta^2 + r^2 \cos^2 \theta d \theta^2 \right) \\
ds^2 = (\cot^2 \theta- 1 ) d\theta^2 \\
ds = \sqrt{\cot^2 \theta-1} d\theta
[/tex]

Am I even on the right track here? Any help/advice is much appreciated.
 
Physics news on Phys.org
  • #2
Take good care of sign of ##dy^2##. The fifth line is [tex]ds^2=cosec^2\theta d\theta
^2[/tex]
 
  • #3
sweet springs said:
Take good care of sign of ##dy^2##. The fifth line is [tex]ds^2=cosec^2\theta d\theta
^2[/tex]

Sorry, I cannot see that?

What I did was this,
[tex]
ds^2 = \left( \frac{1}{r^2 \sin^2 \theta } \right) \left( -r^2 \sin^2 \theta d\theta^2 + r^2 \cos^2 \theta d \theta^2 \right) \\
ds^2 = \frac{-r^2 \sin^2 \theta d\theta^2}{r^2 \sin^2 \theta} + \frac{r^2 \cos^2 \theta d \theta^2}{r^2 \sin^2 \theta} \\
ds^2 = -1 d\theta^2 + \cot^2 d \theta^2 \\
ds^2 = (\cot^2 \theta - 1) d \theta^2
[/tex]
 
  • #4
What is your idea behind computing ##ds## in terms of ##d\theta##? How is it going to help you find out whether or not your curves are geodesics? (I am not saying it doesn't, just asking for your rationale.)

I also agree with @sweet springs , you need to be more careful with your signs. Note that ##(-1)^2 = 1## and not ##-1##.
 
  • #5
Orodruin said:
What is your idea behind computing ##ds## in terms of ##d\theta##? How is it going to help you find out whether or not your curves are geodesics? (I am not saying it doesn't, just asking for your rationale.)

I also agree with @sweet springs , you need to be more careful with your signs. Note that ##(-1)^2 = 1## and not ##-1##.

The idea was to find ##ds^2=##...##d\theta^2## to then find the non-vansihing christoffel symbols of metric in terms of ##\theta## to plug into new geodesic equation.

This is what I have done so far now, leaving where last post left off and fixing mistake

[tex]
ds^2 = \left( \frac{1}{r^2 \sin^2 \theta } \right) \left( r^2 \sin^2 \theta d\theta^2 + r^2 \cos^2 \theta d \theta^2 \right) \\
ds^2 = d\theta^2 + \cot^2 d \theta^2 \\
ds= \sqrt{(\cot^2 \theta + 1)} d \theta \\
ds = \csc \theta d\theta \\
ds^2 = \csc^2 d\theta^2

[/tex]

Then I can write a new tensor metric as such

[tex]

g_{\alpha\beta} = \begin{pmatrix} 0 & 0 \\ 0 & \csc^2 \theta \end{pmatrix} \\
g^{\alpha\beta} = \begin{pmatrix} 0 & 0 \\ 0 & \sin^2 \theta \end{pmatrix} \\
\\
\Gamma^{\theta}_{\theta\theta} = \frac{1}{2} \sin^2 \theta \left( - \frac{\partial}{\partial \theta} \csc^2 \theta \right) \\
\Gamma^{\theta}_{\theta\theta} = \sin^2 \theta \cot^2 \theta \csc^2 \theta = \cot^2 \theta \\
[/tex]

Then new geodesic equation becomes, noting that since ##ds=\csc \theta d\theta## that ##d\theta = \sin \theta ds##...
[tex]
0= \frac{d^2\theta}{ds^2} - \Gamma^{\theta}_{\theta\theta} \left( \frac{d\theta}{ds} \right)^2 \\
0=\frac{d}{ds}\left( \sin \theta \right) - \left( \cot^2 \theta \right) \left( \sin^2 \theta \right) \\
0=\cos \theta \sin \theta - \cos^2 \theta
[/tex]

Which does not equal zero. Any help is really appreciated. Thanks.
 
Last edited:
  • #6
ChrisJ said:
The idea was to find ds2=ds2=ds^2=...dθ2dθ2d\theta^2 to then find the non-vansihing christoffel symbols of metric in terms of θθ\theta to plug into new geodesic equation.
This will not work. All you are doing is getting an induced metric on the circle. Your manifold has two coordinates and the metric is non-degenerate.

You need to find the Christoffel symbols in your original coordinate system (or another coordinate system on your original manifold) and show that the curve is a geodesic. Note that a curve can be a non-affinely parametrised geodesic, which means that it will not satisfy the geodesic equation directly, but can be made to do so by a reparametrisation.
 
  • #7
Orodruin said:
This will not work. All you are doing is getting an induced metric on the circle. Your manifold has two coordinates and the metric is non-degenerate.

You need to find the Christoffel symbols in your original coordinate system (or another coordinate system on your original manifold) and show that the curve is a geodesic. Note that a curve can be a non-affinely parametrised geodesic, which means that it will not satisfy the geodesic equation directly, but can be made to do so by a reparametrisation.

Oh, bugger. Ok thanks.

Well the geodesic equation, given the chrsitoffel symbols to the original coordinate system is as follows
[tex]
0 = \frac{d^2x}{ds^2} - \frac{2}{y}\frac{dx}{ds}\frac{dy}{ds} \\
0 = \frac{d^2y}{ds^2} - \frac{1}{y} \left( \frac{dy}{ds} \right)^2 + \frac{1}{y}\left( \frac{dx}{ds} \right)^2
[/tex]

are you saying that I need to work the following out?
[tex]
0 = \frac{d}{ds} \left( \frac{d}{ds} \left( r \cos \theta + x_0 \right) \right) - \frac{2}{r \sin \theta} \left( \frac{d}{ds} (r \cos \theta + x_0) \right) \left( \frac{d}{ds}r\sin \theta \right) \\
0 = \frac{d}{ds}\left(\frac{d}{ds} r \sin \theta \right) - \frac{1}{r\sin \theta} \left( \frac{d}{ds} r\sin \theta \right)^2 + \frac{1}{r \sin \theta} \left(\frac{d}{ds} (r \cos \theta + x_0) \right)^2
[/tex]
 
  • #8
ChrisJ said:
are you saying that I need to work the following out?
Yes. This should not be too difficult seeing that there is only one variable (the curve parameter ##\theta##). Do not forget that ##\theta## is not necessarily an affine parameter.
 
  • #9
Orodruin said:
Yes. This should not be too difficult seeing that there is only one variable (the curve parameter ##\theta##). Do not forget that ##\theta## is not necessarily an affine parameter.

ok its been a while since I've done implicit differentiation, but am I correct in thinking that, for example ##\frac{d}{ds} r \sin \theta = r \cos \theta \frac{d\theta}{ds} = r \cos \theta \sin \theta ##

Since in my wrong method above I found that ##\frac{d\theta}{ds}= \sin \theta ##
 
  • #10
ChrisJ said:
ok its been a while since I've done implicit differentiation, but am I correct in thinking that, for example ##\frac{d}{ds} r \sin \theta = r \cos \theta \frac{d\theta}{ds} = r \cos \theta \sin \theta ##

Since in my wrong method above I found that ##\frac{d\theta}{ds}= \sin \theta ##
Yes, this would amount to implicitly reparametrising the curve with the path length ##s##.
 
  • #11
Orodruin said:
Yes, this would amount to implicitly reparametrising the curve with the path length ##s##.

Ok, I think I am having a bit of trouble here, does not seem to equal zero the way I'm doing it.

I found all the derivatives I need separately to make it clearer, then plug in at the end.
[tex]
\frac{d}{ds} r \sin \theta = r \cos \theta \frac{d\theta}{ds} = r \cos \theta \sin \theta \\
\frac{d}{ds}(r \cos \theta + x_0) =- r \sin \theta \frac{d\theta}{ds} = -r \sin^2 \theta \\
\frac{d}{ds} \left( \frac{d}{ds} \left( r \cos \theta + x_0 \right) \right) = \frac{d}{ds} \left( r \sin^2 \theta \right) = (-r \cos \theta \sin \theta + r \sin\theta \cos \theta) \frac{d\theta}{ds} = 0 \\
\frac{d}{ds}\left(\frac{d}{ds} r \sin \theta \right) = \frac{d}{ds}(r \cos \theta \sin \theta) = (r \sin^2 \theta - r \sin^2 \theta) \frac{d\theta}{ds} =0
[/tex]

So both of the second derivative in the geodesic equations equal zero, and just need to focus on the single derivatives. So,
[tex]
0 = \frac{d}{ds} \left( \frac{d}{ds} \left( r \cos \theta + x_0 \right) \right) - \frac{2}{r \sin \theta} \left( \frac{d}{ds} (r \cos \theta + x_0) \right) \left( \frac{d}{ds}r\sin \theta \right) \\
0 = -\frac{2}{r\sin \theta} \left( -r \sin^2 \theta \right) \left( r \cos \theta \sin \theta \right) \\
0 = 2r \sin^2 \theta \cos \theta
[/tex]

and the other one..
[tex]
0 = \frac{d}{ds}\left(\frac{d}{ds} r \sin \theta \right) - \frac{1}{r\sin \theta} \left( \frac{d}{ds} r\sin \theta \right)^2 + \frac{1}{r \sin \theta} \left(\frac{d}{ds} (r \cos \theta + x_0) \right)^2 \\
0 =- \frac{1}{r \sin\theta} \left( r \cos \theta \sin \theta \right)^2 + \frac{1}{r \sin\theta} ( -r \sin^2 \theta )^2 \\
0 = -r \cos^2 \theta \sin \theta + r \sin^3 \theta
[/tex]
 
Last edited:
  • #12
ChrisJ said:
0=dds(sinθ)−(cot2θ)(sin2θ)
0=cosθsinθ−cosθ​
I do not follow physical meaning but there is a mistake in your calculation. From the top one
[tex]cos\theta(\frac{d\theta}{ds}-cos\theta)=0[/tex]
[tex]ds=\frac{d\theta}{cos\theta}[/tex]
[tex]s=\frac{1}{2}log|\frac{1+sin\theta}{1-sin\theta}|+C[/tex]
 
  • #13
sweet springs said:
I do not follow physical meaning but there is a mistake in your calculation. From the top one
[tex]ds=\frac{d\theta}{cos\theta}[/tex]

Where did you get that from? From post 5, it can be seen that

[tex]ds^2 = \csc^2 \theta d\theta^2 \\
ds = \csc \theta d \theta \\
ds = \frac{d\theta}{\sin \theta}
[/tex]
 
  • #14
I've got it from your
[tex]0=\frac{d}{ds}(sin\theta)-cot^2\theta sin^2\theta[/tex]
Could you elaborate which equation is a right one?
 
  • #15
sweet springs said:
I've got it from your
[tex]0=\frac{d}{ds}(sin\theta)-cot^2\theta sin^2\theta[/tex]
Could you elaborate which equation is a right one?

Oh right ok, there might be an error there somewhere but that is a wrong method anyway. As per post 6 onwards tried to go about the problem from a different angle as per Orodruin's suggestion. However, I am pretty certain that ##\frac{d\theta}{ds} = \sin \theta ##, which that bit is still needed in new method.
 
  • #16
If you are certain about that formula why do not you integtrate immediately to get
[tex]s=\frac{1}{2}log|\frac{1-cos\theta}{1+cos\theta}|+C[/tex]?
 

Related to Proving Geodesics in Hyperbolic Geometry

1. What is a geodesic in hyperbolic geometry?

A geodesic in hyperbolic geometry is the shortest path between two points on a hyperbolic surface, similar to a straight line in Euclidean geometry. However, in hyperbolic geometry, the geodesic is not necessarily a straight line and can appear to be curved.

2. How do you prove that a curve is a geodesic in hyperbolic geometry?

To prove that a curve is a geodesic in hyperbolic geometry, you can use the hyperbolic law of cosines. This law states that for a triangle in hyperbolic space, the sum of the angles is less than 180 degrees. If the curve follows this law, it can be considered a geodesic.

3. What are some real-world applications of proving geodesics in hyperbolic geometry?

Proving geodesics in hyperbolic geometry has various applications in fields such as physics, engineering, and computer science. It is used in designing optimal paths for transportation systems, optimizing communication networks, and understanding the behavior of light in non-Euclidean spaces.

4. What are some differences between geodesics in hyperbolic geometry and geodesics in Euclidean geometry?

In Euclidean geometry, geodesics are straight lines, while in hyperbolic geometry, they can appear to be curved. Also, the sum of angles in a triangle is 180 degrees in Euclidean geometry, while it is less than 180 degrees in hyperbolic geometry.

5. Are there any challenges in proving geodesics in hyperbolic geometry?

Yes, there are challenges in proving geodesics in hyperbolic geometry due to the non-Euclidean nature of the space. It requires different mathematical techniques and assumptions compared to proving geodesics in Euclidean geometry. Additionally, visualizing and understanding hyperbolic space can be difficult, making it a challenging task to prove geodesics.

Similar threads

  • Special and General Relativity
2
Replies
44
Views
1K
  • Special and General Relativity
Replies
8
Views
1K
  • Special and General Relativity
Replies
11
Views
250
  • Special and General Relativity
Replies
9
Views
1K
  • Special and General Relativity
Replies
14
Views
810
  • Special and General Relativity
Replies
10
Views
1K
  • Special and General Relativity
Replies
2
Views
739
  • Special and General Relativity
Replies
4
Views
1K
Replies
12
Views
1K
  • Special and General Relativity
Replies
18
Views
2K
Back
Top