Thursday, April 11, 2019

general relativity - What is the meaning of non-coordinate basis?


I mean how the co-frame field eI(x) differs from the coordinate vector basis for co-vector dxμ. How to interpret them? Does it means for coordinate vector we can find the integral curves?



Answer



Integral curves of non-coordinate (anholonomic) basis vectors also exist, they just don't form a coordinate system.


This might be a bit difficult to swallow, but the heart of the issue in a coordinate system, the coordinates are independent.


Here's a direct example:


Consider polar coordinates in R2. These are given by x=rcosφy=rsinφ.

The coordinate basis vectors are r=cosφx+sinφyφ=rsinφx+rcosφy.



These are orthogonal, but not orthonormal. We can also norm these vectors and get ˆer=r=cosφx+sinφyˆeφ=1rφ=sinφx+cosφy.

The first set is holonomic, the second isn't, you can calculate [ˆer,ˆeφ] to ascertain this.


To try to interpret what it means for the integral curves of the anholonomic set not forming coordinates, consider that for the holonomic polar coordinate vectors, the φ vector is longer, the further you are away from the origin. This is expected, φ is an angular coordinate, the same angular displacement corresponds to larger and larger actual displacements the further you are away from the origin.


Consider now the integral curves of the set ˆer,ˆeφ instead. It is visually clear that the "paths" corresponding to the integral curves are the same, BUT the parametrization for the φ-curves are different. The vector field ˆeφ has the same length everywhere, so all "ˆφ" curves have the same velocity.


Imagine you are at the point (r0,φ0). You move a parameter ˉφ along the integral curves of ˆeφ. Since the integral curves are path-length parametrized (the length of ˆeφ is 1 after all), you move a distance of ˉφ, and now you are at (r0,φ0+1r0ˉφ) (remember that I am measuring points in the original "holonomic" coordinates and that the real displacement corresponding to a coordinate displacement φ is ˉφ=r0φ, since we are at radius r0).


Now we move radially to 2r0, so our coordinates are (2r0,φ0+1r0ˉφ). After this, we move along the integral curves of ˆeφ a parameter value of ˉφ. This is once again, "actual displacement", and its value in φ-coordinates is 12r0ˉφ, since we are now at radius 2r0.


Our new position is (2r0,φ0+1r0ˉφ12r0ˉφ)=(2r0,φ0+12r0ˉφ). Now we move back radially from 2r0 to r0, and end up at (r0,φ0+12r0ˉφ).


What we notice is that we did not do a loop at all, we had a net displacement of 12r0ˉφ in the angular direction.


Now, if there actually did exist an (r,ˆφ) coordinate system attached to the basis (ˆer,ˆeφ), then in this coordinate system our path would have been (r0,ˆφ0)(r0,ˆφ0+ˉφ)(2r0,ˆφ0+ˉφ)(2r0,ˆφ0+ˉφˉφ)=(2r0,ˆφ0)(r0,ˆφ0),

so we would have made a "coordinate loop", yet we would have had a net displacement. The "anholonomic coordinates" are not unambigous, because doing a finite loop, we ended up in a different point, yet both points have the same coordinates.


Clearly a coordinate system could never work this way.


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