guitarphysics
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Hi all, this might be a silly question, but I was curious. In Carroll's book, the author says that, in a manifold M, for any vector k in the tangent space T_p at a point p\in M, we can find a path x^{\mu}(\lambda) that passes through p which corresponds to the geodesic for that vector (k being the tangent vector to the path). Two conditions for this path are:
\lambda(p)=0 \\ \frac{dx^{\mu}}{d\lambda}(\lambda=0)=k^{\mu} <br />
(And, of course, it must satisfy the geodesic equation.)
From this, we can then construct a map, call it \exp_p: T_p\to M such that \exp_p(k)=x(\lambda=1)
Where x(\lambda=1) is the point in M belonging to the parametrized path introduced earlier (the geodesic for k) evaluated at \lambda=1. Now, my question is: why are we evaluating at \lambda=1? Not only does this seem arbitrary- it also seems completely independent of all aspects of the manifold. What I mean by this is that we could pick any parameter, big or small, for our geodesic (since we're working with an affine parameter, I think). Given this, it seems like we lose our ability to say that \exp_p maps to the neighborhood of p; it could map to faraway places in the manifold, given the right parameter. So given this,
1) Why was this chosen? Arbitrary convention?
2) Is what I pointed out above problematic, or is it a non-issue? (Regarding the fact that we can map to faraway places.)
3) Could something be chosen instead of \lambda=1, that sort of characterizes a "small scale" in the manifold? This is related to something I'm not very sure about- is there a way to establish the "physical size" of a manifold? Throwing rigor out the window, what I mean is this: maybe we could say that a manifold has "size" S_M, and then redefine the map so that \exp_p(k)=x(\lambda=s), where s<<S_M. For an example of what I mean by this "size", maybe we could say S_M=2\pi R for S^2? (The problem is I doubt this could be done in general :c ).
Many thanks in advance!
\lambda(p)=0 \\ \frac{dx^{\mu}}{d\lambda}(\lambda=0)=k^{\mu} <br />
(And, of course, it must satisfy the geodesic equation.)
From this, we can then construct a map, call it \exp_p: T_p\to M such that \exp_p(k)=x(\lambda=1)
Where x(\lambda=1) is the point in M belonging to the parametrized path introduced earlier (the geodesic for k) evaluated at \lambda=1. Now, my question is: why are we evaluating at \lambda=1? Not only does this seem arbitrary- it also seems completely independent of all aspects of the manifold. What I mean by this is that we could pick any parameter, big or small, for our geodesic (since we're working with an affine parameter, I think). Given this, it seems like we lose our ability to say that \exp_p maps to the neighborhood of p; it could map to faraway places in the manifold, given the right parameter. So given this,
1) Why was this chosen? Arbitrary convention?
2) Is what I pointed out above problematic, or is it a non-issue? (Regarding the fact that we can map to faraway places.)
3) Could something be chosen instead of \lambda=1, that sort of characterizes a "small scale" in the manifold? This is related to something I'm not very sure about- is there a way to establish the "physical size" of a manifold? Throwing rigor out the window, what I mean is this: maybe we could say that a manifold has "size" S_M, and then redefine the map so that \exp_p(k)=x(\lambda=s), where s<<S_M. For an example of what I mean by this "size", maybe we could say S_M=2\pi R for S^2? (The problem is I doubt this could be done in general :c ).
Many thanks in advance!