The Schwarzschild Metric - A Simple Case

  • #151
I was assuming the given velocity was wrt coordinate time, but you say
<br /> \sqrt{2m/r} = \frac{dr}{d\tau}<br />
and I have no reason right now not to believe you.

So, you need to replace your integrand with the modified one...
I did that calculation some time ago and it does get very messy.
 
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  • #152
Mentz114 said:
I was assuming the given velocity was wrt coordinate time, but you say
<br /> \sqrt{2m/r} = \frac{dr}{d\tau}<br />
and I have no reason right now not to believe you.
Yes, more generally:

<br /> \sqrt{2m/r-2m/r_0} = \frac{dr}{d\tau}<br />I don't expect you to take anything on faith, I wrote the complete derivation https://www.physicsforums.com/blog.php?b=1957 . Please have a look at the file "RadialMotion1" and please check the results, all the necessary equations are derived from base principles, this is the proper and scientific thing to do and I am glad that we are interacting the way two scientists should interact .

I did that calculation some time ago and it does get very messy.

Such is life, we don't always get "nice" formulas. :-)
 
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  • #153


Mentz114 said:
I've finally come up with a proposal for the stretching factor in Gullstrand-Painleve coords.

A test body falls from r1 -> r2 ( being at r1 when t=0) in time T1, so
<br /> T_1 &amp;= \int_{r_1}^{r_2}\sqrt(r/2m) dr<br /> &amp;= \frac{1}{3}\sqrt{ \frac{2}{m} } \left( r_2^{3/2}- r_1^{3/2} \right)<br />
Another test body is on the same geodesic, but is at r1+L at time t=0. It will fall to point x in time T2
<br /> T_2 &amp;= \int_{r_1+L}^{x}\sqrt(r/2m) dr<br /> &amp;= \frac{1}{3}\sqrt{ \frac{2}{m} } \left( x^{3/2}- (L+r_1)^{3/2} \right)<br />
We can set T1-T2=0 and solve for x, which gives
<br /> x={\left( {\left( L+r_1\right) }^{\frac{3}{2}}+{r_2}^{\frac{3}{2}}-{r_1}^{\frac{3}{2}}\right) }^{\frac{2}{3}}<br />
and the new separation is given by r2-x.

This is essentially the equation given by passionflower in the closely related parallel thread "https://www.physicsforums.com/showpost.php?p=2904752&postcount=21"".

Passionflower said:
The free fall from infinity does not pose a problem in terms of discovering proper time if we switch things around and consider proper time in terms of 'proper time till ultimate doom', e.g. the arrival at the singularity. See the attached graph for a comparison between proper and coordinate time. As you can see coordinate time never gets beyond Rs while proper time gets all the way to the singularity.

Using (MTW 25.38):

<br /> -2/3\,{\it rs}\, \left( {\frac {r}{{\it rs}}} \right) ^{3/2}<br />

This is the proper time remaining until the clock falling from infinity before it arrives at the singularity. For the elapsed proper time as the clock falls from r1 to r2 if free-falling from initially at rest at infinity the equation is:

\Delta tau = \frac{2}{3}r_s \left( \left(\frac{r_1}{r_s}\right)^{3/2} - \left(\frac{r_2}{r_s}\right)^{3/2} \right)

It is clear from the above that your T1 and T2 are elapsed proper times and unfortunately I have to agree with Starthaus that setting T1-T2=0 does not give the proper distance and it is the coordinate time difference that has to be set to zero.
 
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  • #154


yuiop said:
This is essentially the equation given by passionflower in the closely related parallel thread "https://www.physicsforums.com/showpost.php?p=2904752&postcount=21"".



This is the proper time remaining until the clock falling from infinity before it arrives at the singularity. For the elapsed proper time as the clock falls from r1 to r2 if free-falling from initially at rest at infinity the equation is:

\Delta tau = \frac{2}{3}r_s \left( \left(\frac{r_1}{r_s}\right)^{3/2} - \left(\frac{r_2}{r_s}\right)^{3/2} \right)

It is clear from the above that your T1 and T2 are elapsed proper times and unfortunately I have to agree with Starthaus that setting T1-T2=0 does not give the proper distance and it is the coordinate time difference that has to be set to zero.

Thank you, in the meanwhile Mentz and I have solved the problem. Correctly.
 
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  • #155
Mentz114 said:
I was assuming the given velocity was wrt coordinate time, but you say
<br /> \sqrt{2m/r} = \frac{dr}{d\tau}<br />
and I have no reason right now not to believe you.I did that calculation some time ago and it does get very messy.

There are various ways to express the velocity of a particle initially at rest rest at R that falls to r.

The "proper velocity" (Coordinate distance divided by proper time of the falling object is:

\frac{dr}{dtau} = \sqrt{2m/r - 2m/R}

The local velocity according to a shell observer using his local rulers and clocks as the object passes is:

\frac{dr&#039;}{dt&#039;} = \frac{\sqrt{2m/r - 2m/R}}{\sqrt{1-2m/R}}

The Schwarzschild coordinate velocity in either case is:

\frac{dr}{dt} = (1-2m/r) \frac{\sqrt{2m/r - 2m/R}}{\sqrt{1-2m/R}}

All these have been given at some point in this thread, but I thought it might be useful to have them all in the same place and clearly defined.

There are obvious simplifications if R = infinity.
 
  • #156


starthaus said:
Thank you, in the meanwhile Mentz and I have solved the problem. Correctly.

To me, "a step in the right direction" and "A major problem with the approach" is a little short of solving the problem.

starthaus said:
This is a step in the right direction, the formalism is very nicely set and the math is very clear. I can see a major problem with the approach, T is proper time, so you do not want T_1=T_2. What you want is t_1=t_2, that is you want to mark the ends of the rod at the same time in the distant observer's frame, not in the rod frame. You can do that using Schwarzschild coordinates as well. When you do that, you get a very nasty transcendental equation, not due to the use of coordinates but due to the condition t_1=t_2. I solved this for the more general case of the rod falling from a finite height and I got a much nastier equation.

You have also come nowhere near solving the corresponding Schwarzschild coordinates of a rigid (constant proper length) falling object.
 
  • #157


yuiop said:
To me, "a step in the right direction" and "A major problem with the approach" is a little short of solving the problem.

You must have missed the fact that the "problem with the approach" has been fixed. All you are left to do is to introduce the correct integrand (as opposed to the incorrect one that you've been pushing throughout the thread) and evaluate the integral. Turn the crank kind of stuff, use your favorite canned software.
 
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  • #158
yuiop said:
There are various ways to express the velocity of a particle initially at rest rest at R that falls to r.

The "proper velocity" (Coordinate distance divided by proper time of the falling object is:

\frac{dr}{dtau} = \sqrt{2m/r - 2m/R}

The local velocity according to a shell observer using his local rulers and clocks as the object passes is:

\frac{dr&#039;}{dt&#039;} = \frac{\sqrt{2m/r - 2m/R}}{\sqrt{1-2m/R}}

The Schwarzschild coordinate velocity in either case is:

\frac{dr}{dt} = (1-2m/r) \frac{\sqrt{2m/r - 2m/R}}{\sqrt{1-2m/R}}

All these have been given at some point in this thread, but I thought it might be useful to have them all in the same place and clearly defined.

There are obvious simplifications if R = infinity.


They've been in https://www.physicsforums.com/blog.php?u=241315 (including their derivations from base principles) for months. You only needed to figure out what was the correct integrand to use (definitely not he one you've been pushing).
 
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  • #159
starthaus said:
I have repeatedly told both you and Passionflower that you are using the wrong approach since you are trying to force the stationary solution for the case of the moving rod.

I made it clear in post 82 of this thread and earlier in the related thread that that formula is for a stationary ruler. I was simply defending DrGreg when you said his equation for a static ruler distance in Schwarzschild coordinates is wrong and we have had to waste dozens of posts proving DrGreg equation was correct in the context it was given. Now that you have forced us to waste time proving that DrGreg's equation was correct (and both passionflower and myself expressly stated we did not want to waste time on it, you say oh yeah, that formula that you said was incorrect is actually correct but it not relevant.) Here is post 82:

yuiop said:
The integrated or ruler distance is given by:

<br /> \sqrt{r2*(r2-rS)} - \sqrt{r1*(r1-rS)}<br /> + rS*\left(LN\left(\sqrt{r2} + \sqrt{(r2-rS)}\right)- LN\left(\sqrt{r1} + \sqrt{(r1-rS)}\right)\right)<br />

...

Unfortunately, neither of the above equations tell us about the proper distance to the event horizon according to a moving observer and I am not sure if that can be defined. The last equation is the closest thing to a notion of proper distance to the event horizon but it applies to a stationary ruler.
I was aware and always have been that the above equation is for a stationary ruler in Schwarzschild coordinates.

There was nothing to check numerically since the Rindler formula was derived via Taylor expansion for r&gt;&gt;r_s. This is is quite clear from the Rindler book and from my explanation.

If you knew that the Rindler formula was an approxiamtion, then why on Earth did you change Rindler's "approximately equals" symbol to an "exactly equal" symbol and then proceed to integrate the approximate equation and declare you integration of the approximate equation to be correct and and Passionflower's integration of the exact equation incorrect? Your responses are barely those of a sane person sometimes. :rolleyes:
 
  • #160
yuiop said:
I was aware and always have been that the above equation is for a stationary ruler in Schwarzschild coordinates.

Yet, you kept pushing it as a solution for the problem. Why?
If you knew your solution was wrong all along why did you keep pushing it?
 
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  • #161
Thanks everyone, I understand the free falling frame much better now. Good job listing the various velocities, yuiop.

The Wiki page on G-P is rather good. It shows the essentials concisely, including the coordinate transformation which I couldn't find before and had to work out myself.

I'll leave you guys to argue about who said what, when and how often.
 
  • #162
starthaus said:
I don't think it is. Anyways, the error is easy to fix:

-start with coordinate speed for rod falling from r_0:

\frac{dr}{dt}=(1-r_s/r) \sqrt {1-\frac{1-r_s/r}{1-r_s/r_0}}

-make r_0-&gt;\infty, therefore:

\frac{dr}{dt}=(1-r_s/r) \sqrt {r_s/r}

So, you need to replace your integrand with the modified one:

\frac{dr}{1-r_s/r}*\sqrt{r/r_s}

After you do this, all you end up with is where the clocks are after they fallen for an equal coordinate time and this has already been done in this thread and is not the proper distance of the falling clocks (as far as I can tell). Anybody is welcome to try and convince me otherwise.
 
  • #163
yuiop said:
After you do this, all you end up with is where the clocks are after they fallen for an equal coordinate time and this has already been done in this thread

...incorrectly , by you. Several times.
and is not the proper distance[/color] of the falling clocks

What ever gives you the idea that the solution gives the proper distance[/color]? Do you even understand the basic formulas?
(as far as I can tell). Anybody is welcome to try and convince me otherwise.

Given that you've been pushing the wrong solution for 100+ posts, your opinion doesn't mean much.
 
  • #164
yuiop said:
After you do this, all you end up with is where the clocks are after they fallen for an equal coordinate time and this has already been done in this thread and is not the proper distance of the falling clocks (as far as I can tell). Anybody is welcome to try and convince me otherwise.
I was dealing with the question - given an initial coordinate separation, what will the separation be after a certain coordinate time has passed ?

And I think that's what I got, eventually.

[edit]yuiop - I think your opinions have merit.
 
  • #165
Mentz114 said:
Thanks everyone, I understand the free falling frame much better now. Good job listing the various velocities, yuiop.

The Wiki page on G-P is rather good. It shows the essentials concisely, including the coordinate transformation which I couldn't find before and had to work out myself.

Just had a quick look at GP coordinates on Wiki as you suggested. In radial motion terms only the GP metric is:

d tau^2 = (1-2m/r) dt_r^2 - 2\sqrt{(2m/r)} dt_r dr - dr^2

Now for dt_r = 0 the above metric appears to give d tau^2 = dr^2 (with c=1) so that in the free falling frame the proper distance derivative is the same as the Schwarzschild coordinate distance derivative. Maybe Passionflower was onto something :wink: The integrated distance between freefalling objects in GP coordinates is the same as the integrated distance between two stationary objects in Schwarzschild coordinates. Not quite sure what the significance of that is yet.
 
  • #166
yuiop said:
After you do this, all you end up with is where the clocks are after they fallen for an equal coordinate time and this has already been done in this thread and is not the proper distance of the falling clocks (as far as I can tell). Anybody is welcome to try and convince me otherwise.

starthaus said:
What ever gives you the idea that the solution gives the proper distance[/color]? Do you even understand the basic formulas?

When I say "is not the proper distance" I clearly do not mean that I have the idea that it is the proper distance. However one of the major things we have been trying to solve in this thread is the proper distance of the falling clocks. In the OP passionflower wanted to know the coordinate separation of two clocks that maintain constant proper distance apart as they fall. In order to do that you need to know how to define proper constant distance for the clocks. Since you claim to solved the questions posed in the OP this implies that you solved how to define proper distance in the reference frame of the falling clocks. Clearly you have not done that and your proposed solution does not solve that.

Given that you've been pushing the wrong solution for 100+ posts, your opinion doesn't mean much.
I gave a proposed solution early on in the thread that I also withdrew early on when I realized the problem was much more complicated than I originally assumed. Since then I have not proposed any definitive solutions to the problems in the OP. Although you have said the problem is intractable, the fact that think you have a solution only tells me you have not realized the full complexity of the problems posed in the OP. If you have a real solution, you can post a numerical solution to the problem posed in the OP and you can do this without fear of giving away any valuable secret information about the formulas used, as I know you think this it is detrimental to the educational process of readers if you are not not vague and evasive and provide concise accurate information.
 
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  • #167
starthaus said:
Yet, you kept pushing it as a solution for the problem. Why?
If you knew your solution was wrong all along why did you keep pushing it?

Show me one post where I claimed the the equation for the static ruler distance between two Schwarzschild coordinates is the proper length of a falling ruler?
 
  • #168
My error
<br /> \sqrt {r \left( r-1 \right) }+\ln \left( \sqrt {r}+\sqrt {r-1}<br /> \right) <br />

works just fine. And I think I see how to sketch out a solution that most of us will agree with.

(It appears that some other people wrote up similar ideas while I was writing this - and it appears that if yuiop agrees with me, strathaus will claim he's wrong, so I don't expect universal agreement ::smiley face::).

If we take r_s =1 or M = 1/2, and R = infinity, we can use the simpler equations MTW 25.38 to find the Schwarzschild t coordinate as a function of the r coordinate. It also gives us proper time, \tau, though we don't really need it.

<br /> \tau = -\frac{2}{3} \, r^{\frac{3}{2}}<br />

<br /> t = -\frac{2}{3} \, r^{\frac{3}{2}} - 2 \, r^{\frac{1}{2}} + ln\frac{r^{\frac{1}{2}}+1}{r^{\frac{1}{2}}-1}<br />

Now, all we need to do to make this a one-parameter group of curves is to use time-translation symmetry. We simply add some small number \epsilon to the schwarzschild time coordinate to represent the second particle, which works because of the time-translation symmetry of the metric, in fancier language \partial / \partial t is a "Killing vector". So we have

<br /> t\left(r, \epsilon\right) = -\frac{2}{3} \, r^{\frac{3}{2}} - 2 r^{\frac{1}{2}} + ln\frac{r^{\frac{1}{2}}+1}{r^{\frac{1}{2}}-1} + \epsilon<br />

Assume that the leading edge of the rod, with the parameter \epsilon =0, has some r-coordinate r_0 at some t-coordinate t_0.

Then we need to find the radial coordinate r_1 of the trailing rod at the same time coordinate t_0 by solving

<br /> t\left(r_1, \epsilon) = t_0 = t\left(r_0, 0\right)<br />

i.e.
<br /> -\frac{2}{3} \, r_{1}^{\frac{3}{2}} - 2 r_{1}^{\frac{1}{2}} + ln\frac{r_{1}^{\frac{1}{2}}+1}{r_{1}^{\frac{1}{2}}-1} + \epsilon = -\frac{2}{3} \, r_{0}^{\frac{3}{2}} - 2 r_{0}^{\frac{1}{2}} + ln\frac{r_{0}^{\frac{1}{2}}+1}{r_{0}^{\frac{1}{2}}-1} <br />

Then we use
<br /> \sqrt {r_{1} \left( r_{1}-1 \right) }+\ln \left( \sqrt {r_{1}}+\sqrt {r_{1}-1} \right) - \sqrt {r_{0} \left( r_{0}-1 \right) } - \ln \left( \sqrt {r_{0}}+\sqrt {r_{0}-1}<br /> \right) <br />

to integrate between r_0 and r_1 to get the length as seen by a static observer for the falling rod. To get the proper length, we multiply by gamma, based on the radial velocity which we know is 1 / \sqrt{r}.
 
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  • #169
pervect said:
If we take r_s =1 or M = 1/2, and R = infinity, we can use the simpler equations MTW 25.38 to find the Schwarzschild t coordinate as a function of the r coordinate. It also gives us proper time, \tau, though we don't really need it.

<br /> \tau = -\frac{2}{3} \, r^{\frac{3}{2}}<br />

<br /> t = -\frac{2}{3} \, r^{\frac{3}{2}} - 2 \, r^{\frac{1}{2}} + ln\frac{r^{\frac{1}{2}}+1}{r^{\frac{1}{2}}-1}<br />

I got a similar result for t by starting with the coordinate velocity dr/dt = (1-2m/r)*sqrt(2m/r) of a falling object that was initially stationary at infinity and then using 2m=1 and integrating dt = sqrt(r)/(1-1/r) dr, except my signs were reversed, but I won't worry about that too much right now. A small simplification of the equation for t can be brought about by noting that:

ln\frac{r^{\frac{1}{2}}+1}{r^{\frac{1}{2}}-1} = 2 \, arcoth(r)<br />

valid for r>1 which is OK if we stay outside the event horizon.

...

Then we use
<br /> \sqrt {r_{1} \left( r_{1}-1 \right) }+\ln \left( \sqrt {r_{1}}+\sqrt {r_{1}-1} \right) - \sqrt {r_{0} \left( r_{0}-1 \right) } - \ln \left( \sqrt {r_{0}}+\sqrt {r_{0}-1}<br /> \right) <br />

to integrate between r_0 and r_1 to get the length as seen by a static observer for the falling rod. To get the proper length, we multiply by gamma, based on the radial velocity which we know is 1 / \sqrt{r}.

So far I have only skimmed your solution, but broadly it seems a reasonable approach. One small observation is that the last part where you suggest multiplying by gamma based on radial velocity, there seems to be the minor problem that for an extended string of particles, the velocities will be different (I think) depending on where the particles are located. Are you proposing a sort of average velocity or having an arrangement where the particles fall at the same velocity or simply relying on the spatial separation being small enough that differences in individual falling velocities is insignificant?

[EDIT] After a quick re-read I now think you mean the last one because you have specified a small separation. [/EDIT]

Forgive me if I have missed anything significant. This is just a first pass on your proposed solution.
 
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  • #170
yuiop said:
So far I have only skimmed your solution, but broadly it seems a reasonable approach. One small observation is that the last part where you suggest multiplying by gamma based on radial velocity, there seems to be the minor problem that for an extended string of particles, the velocities will be different (I think) depending on where the particles are located.

Correct. If you have a long enough rod, rather than integrate

<br /> \int_{r1}^{r2} \frac{dr}{\sqrt{1-1/r}}<br />

and then multiply the result by gamma, which varies, you want to integrate instead

<br /> \int_{r1}^{r2} \gamma\left( r \right) dr = \int_{r1}^{r2} \frac{dr}{1-1/r}<br />

since in this case \gamma = 1/sqrt(1-v^2) = 1/sqrt(1-1/r)

You can view this as breaking up the long rod into a bunch of short ones, with the evenly spaced "tic marks" of \epsilon marking the divisions, and summing up the distances between the segments of the rod

You might want to do this all the time anyway - it's an easier integral :-)

Note that this means there is no single"frame" for the falling rod. We break the long rod up into a series of short ones, small enough where we can use the flat-space approximation of a "frame" for each segment.

Are you proposing a sort of average velocity or having an arrangement where the particles fall at the same velocity or simply relying on the spatial separation being small enough that differences in individual falling velocities is insignificant?

My original post was for a short enough rod where the velocity change was small enough, the above revision is needed to handle a longer one.
 
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  • #171
yuiop said:
When I say "is not the proper distance" I clearly do not mean that I have the idea that it is the proper distance.

LOL, you clearly don't understand what the formulas mean.

However one of the major things we have been trying to solve in this thread is the proper distance of the falling clocks[/color].

Again? Same mistake? And you still claim that you understand the problem?
Since then I have not proposed any definitive solutions to the problems in the OP.
Then why do you push the incorrect stationary solution in each one of your posts?
 
  • #172
yuiop said:
Show me one post where I claimed the the equation for the static ruler distance between two Schwarzschild coordinates is the proper length of a falling ruler?

Each post you pushed the integrand \frac{dr}{\sqrt{1-r_s/r}} or its integral <br /> \sqrt{r*(r-r_s)} + r_s*LN\left(\sqrt{r} + \sqrt{(r-r_s)}\right)<br />. Meaning all your posts where you made an attempt at solving the problem.
 
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  • #173


Mentz114 said:
I've finally come up with a proposal for the stretching factor in Gullstrand-Painleve coords.

A test body falls from r1 -> r2 ( being at r1 when t=0) in time T1, so
<br /> T_1 &amp;= \int_{r_1}^{r_2}\sqrt(r/2m) dr<br /> &amp;= \frac{1}{3}\sqrt{ \frac{2}{m} } \left( r_2^{3/2}- r_1^{3/2} \right)<br />
Another test body is on the same geodesic, but is at r1+L at time t=0. It will fall to point x in time T2
<br /> T_2 &amp;= \int_{r_1+L}^{x}\sqrt(r/2m) dr<br /> &amp;= \frac{1}{3}\sqrt{ \frac{2}{m} } \left( x^{3/2}- (L+r_1)^{3/2} \right)<br />
We can set T1-T2=0 and solve for x, which gives
<br /> x={\left( {\left( L+r_1\right) }^{\frac{3}{2}}+{r_2}^{\frac{3}{2}}-{r_1}^{\frac{3}{2}}\right) }^{\frac{2}{3}}<br />
and the new separation is given by r2-x.

The algebra and calculus was done with Maxima. This is the only sensible looking result I've managed so far so it would be gratifying if it was right.

[edit] changed second integral

Replace the incorrect integrand with the correct one:

\frac{dr}{1-r_s/r}*\sqrt{r/r_s}

and you get the correct solution, expressed in coordinate time, as it should be.
 
  • #174
Now

While finding a closed for solution for r_1 as a function of r_0, \epsilon from the following is probably impossible

<br /> -\frac{2}{3} \, r_{1}^{\frac{3}{2}} - 2 r_{1}^{\frac{1}{2}} + ln\frac{r_{1}^{\frac{1}{2}}+1}{r_{1}^{\frac{1}{2}}-1} + \epsilon = -\frac{2}{3} \, r_{0}^{\frac{3}{2}} - 2 r_{0}^{\frac{1}{2}} + ln\frac{r_{0}^{\frac{1}{2}}+1}{r_{0}^{\frac{1}{2}}-1} <br />we can do the usual and consider a sufficiently short rod. Let \Delta_r = r_{1} - r_{0}. Then for a short enough rod:

<br /> \Delta_{r} = -\frac{\epsilon}{dt/dr} = \frac {\epsilon\, \left( r-1 \right) }{{r}^{3/2}}<br />

Now \Delta_{r} is a coordinate difference and not really a length of any sort. The length relative to a static observer will be \Delta_{r} / sqrt(1-1/r), and the proper length will be \Delta_{r} / (1-1/r) - for reasons I mention in the last post, basically gamma = 1/sqrt(1-v^2) and v=1/sqrt(r), where v is the local velocity seen by a static observer.

Solving for the proper length, one gets \epsilon / \sqrt{r}.
 
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  • #175
pervect said:
Assume that the leading edge of the rod, with the parameter \epsilon =0, has some r-coordinate r_0 at some t-coordinate t_0.

Then we need to find the radial coordinate r_1 of the trailing rod at the same time coordinate t_0 by solving

<br /> t\left(r_1, \epsilon) = t_0 = t\left(r_0, 0\right)<br />

i.e.
<br /> -\frac{2}{3} \, r_{1}^{\frac{3}{2}} - 2 r_{1}^{\frac{1}{2}} + ln\frac{r_{1}^{\frac{1}{2}}+1}{r_{1}^{\frac{1}{2}}-1} + \epsilon = -\frac{2}{3} \, r_{0}^{\frac{3}{2}} - 2 r_{0}^{\frac{1}{2}} + ln\frac{r_{0}^{\frac{1}{2}}+1}{r_{0}^{\frac{1}{2}}-1} <br />
I am running some numbers to verify I understand it.

If we take the front clock at R=40 we have 180.9850160 time units left.
Now let's take an epsilon of 13 time units, this will give us a back coordinate value of R=41.98100155. Thus the coordinate distance between the front and the back is 1.98100155 which gives a proper distance (for a static observer) of 2.005621996. The two are not identical due to the curvature of spacetime.

I calculated r for t=-60-0 for the front and t=-73-13 for the back and plotted the results. I also calculated the coordinate and proper distance (for a static observer).

Now I do see a stretch both in coordinate and proper time. Is this the tidal stress? One problem with this approach is that we cannot run this past the event horizon, the major spaghettification happens closer to r=0, rather than changing coordinate charts is there any way we can use proper time for this?

pervect said:
<br /> \int_{r1}^{r2} \gamma\left( r \right) dr = \int_{r1}^{r2} \frac{dr}{1-1/r}<br />

since in this case \gamma = 1/sqrt(1-v^2) = 1/sqrt(1-1/r)
I thought the proper distance for a free falling observer is simply dr because the integral becomes the integral for a static observer times 1/gamma and these two factors exactly cancel in this case. (See the page from Raine's and Thomas' book on Black Holes I quoted: https://www.physicsforums.com/attachment.php?attachmentid=28805&d=1286253576)

<br /> \int_{r1}^{r2} {1 \over \gamma(r)} \frac{dr}{\sqrt{1-1/r}} = dr<br />
 

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  • #176
pervect said:
Correct. If you have a long enough rod, rather than integrate

<br /> \int_{r1}^{r2} \frac{dr}{\sqrt{1-1/r}}<br />

There is no justification for such an integral for the problem in the OP.
and then multiply the result by gamma,

Why would you do such a meaningless thing?
which varies, you want to integrate instead

<br /> \int_{r1}^{r2} \gamma\left( r \right) dr = \int_{r1}^{r2} \frac{dr}{1-1/r}<br />

since in this case \gamma = 1/sqrt(1-v^2) = 1/sqrt(1-1/r)

I hope you realize that the multiplication of the integral and the multiplication of the integrand followed by integration produce different results, so the two computations produce different results notwithstanding that both calculations are equally meaningless.
Is this some sort of test to see how many things we can detect in a post?
 
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  • #177
Passionflower said:
I am running some numbers to verify I understand it.

If we take the front clock at R=40 we have 180.9850160 time units left.
Now let's take an epsilon of 13 time units, this will give us a back coordinate value of R=41.98100155. Thus the coordinate distance between the front and the back is 1.98100155 which gives a proper distance (for a static observer) of 2.005621996. The two are not identical due to the curvature of spacetime.

I calculated r for t=-60-0 for the front and t=-73-13 for the back and plotted the results. I also calculated the coordinate and proper distance (for a static observer).
I wonder if you would like to run some numbers using the same parameters I used in post 64 quoted below:
yuiop said:
As I said before, it is probably easier to relax the fall from infinity requirement (although we might try that later) and assume a drop from initially at rest from a finite height.

After a coordinate time of 5 the leading clock will have fallen to 9.99437 and in the same coordinate time the trailing clock will have fallen to 10.953 and the coordinate gap will have increased from 1 to 1.009 if both particles were initially at rest and released at the same coordinate time from heights 10 Rs and 11 Rs.

It is a bit more interesting if you let the particles fall further.

If we start with the same release heights and let the leading particle fall to height 2 Rs then the coordinate fall time is 2.64 and trailing clock is at 4.64 Rs.

I am using the equations given in post 48 to obtain these results, but I have to numerically solve them as the mathematical software I use is unable to find a symbolic solution for r when t is know.

Here is a list of results for various initial and final heights for the trailing clock, all with the leading clock starting one coordinate unit lower and end point determined by the leading clock arriving at 2 Rs.

11 : 4.64
101 : 9.81
1001 : 21.86
10001 : 48.42
100001 : 105.987
1000001 : 230.22
10000001 : 498.02
100000001 : 1075.06
1000000001 : 2318.31

Very approximately, each tenfold increase in the initial drop height results in a two fold increase in the coordinate separation at the end point.

No, it is not that simple. All we have done is determined the coordinate separation of the unconnected free falling particles. We have still not determined the proper separation of the freely falling particles in the rest frame of the particles and I not even sure at this point if it is possible to define what that is. It is as you probably already aware, very difficult to operationally define the proper length of the falling particles for non infinitesimal separations. It does however give an indication of the tidal stretching in coordinate terms.

The attached diagram is a graph in Schwarzschild coordinates of the objects falling from 10 Rs and 11 Rs.

and see how the results compare. The method I used was essentially based on using equal coordinate falling times so the results should be similar to yours and Pervect's.

Now I do see a stretch both in coordinate and proper time. Is this the tidal stress? One problem with this approach is that we cannot run this past the event horizon, the major spaghettification happens closer to r=0, rather than changing coordinate charts is there any way we can use proper time for this?

For equal proper time you could try the method outlined by Mentz in post 147 or even use the equation you gave earlier for "time till doom"

tau = -(2/3)\sqrt{r^3/rs}

which is basically the same thing. As you know, you can use those equations from infinity all the way to through the event horizon to the singularity.
 
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  • #178
It would be interesting to compare with whatever comes out as "distance" via this method to something more standard, like Fermi or Riemann normal coordinates (MTW, pg 285, 332).

I probably haven't stressed enough the fact that there are many "distances" in GR - depending for the most part on the definition of simultaneity, which is a coordinate dependent concept.

Unfortunately, the equations (as usual) are rather intractable, but there's enough for numerical analysis.

Normal" coordinates, whether they be Fermi-normal or Riemann-normal coordinates, measure distance along a space-like geodesic passing through some specified point. Fermi normal coordinates would probably be the best choice for this situation since we have a worldline. So in the region of applicability, for Fermi normal coordinates we use the time along the worldline for the time coordinate, and the distance along the space-like geodesic as the space coordinate.

We can paramaterize a space-like geodesic as a curve t(s), r(s), where s is an affine parameter.

If we require this space-like geodesic to pass through some point (r0,t0), and to be orthogonal to the worldline of an object "falling from infinity" at that point, I get the following equations which determine the geodesic r(s), t(s).

I've assumed that r_s = 1.

<br /> \frac{dr}{ds} = -\sqrt{1 + \frac{1}{r0} - \frac{1}{r}}<br />

<br /> \frac{dt}{ds} = \frac{r}{\sqrt{r0} \, \left( r -1 \right) }<br />

though I don't think we need dt/ds, actually.

and of course at t=t0, r= r0 - it's simplest to take t0 = 0.

Finding the value of s at which r=1 should be the "distance to the event horizon in Fermi normal coordinates", s is an "affine paramaterization" along the geodesic which measures total length.

This is a solution for ingoing geodesics because dr/ds is negative - for outgoing geodesics, just change the sign - making s negative should also work.
 
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