Curvilinear coordinates from orbits

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Discussion Overview

The discussion revolves around the construction of curvilinear coordinates from the orbits of points under the actions of rotation and scaling transformations in the plane. Participants explore the implications of these transformations and the conditions necessary for constructing such a coordinate system.

Discussion Character

  • Exploratory
  • Technical explanation
  • Conceptual clarification
  • Debate/contested

Main Points Raised

  • One participant describes a problem involving transformations R_\alpha (rotation) and S_\lambda (scaling) and seeks a method to construct curvilinear coordinates based on the parameters of these transformations.
  • Another participant notes that the rotation group is diffeomorphic to the circle S^1 and the scaling group to the real line, suggesting a diffeomorphic map that relates these transformations to polar coordinates in R², but questions the relevance of log-polar coordinates.
  • A third participant acknowledges the clarity of the previous explanation and expresses interest in the procedure for constructing curvilinear coordinates when using different, less familiar groups of transformations.
  • One participant cautions that the generalization of the diffeomorphic map may not hold for arbitrary groups, providing examples where the differential fails to be surjective, emphasizing the importance of transverse orbits for the original example to work.

Areas of Agreement / Disagreement

Participants express varying degrees of understanding and curiosity about the construction of curvilinear coordinates, with some agreement on the limitations of generalizing the method to other groups. However, there is no consensus on a definitive procedure for arbitrary transformations.

Contextual Notes

Participants highlight that the success of constructing curvilinear coordinates depends on the nature of the orbits under the group actions, particularly their transversality, which is not guaranteed for all groups.

mnb96
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Hello,

I have the following problem where I have two groups of transformations R_\alpha (rotation) and S_\lambda (scaling) acting on the plane, so that the orbits of any arbitrary point x=(x0,y0) under the actions of S_\lambda and R_\alpha are known (in the former case they are straight lines from the origin; in the latter case they are concentric circles with center in 0).

From this information, how can I "build" a system of curvilinear coordinates, where the coordinates are exactly the parameters (α,λ) of the transformations?

PS: I know that the answer leads to the log-polar coordinates, but I need a procedure to arrive at it.
 
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The rotation group is diffeomorphic to the circle S^1, while the scaling group is diffeomorphic to the real line. It is clear that if you take the standard coordinates θ on S^1 and r on R^1, then the map

(-pi,pi) x (0,infty)-->R x S --->R^2
(θ,r)------------->(Rθ,Sr)--->(Rθ\bulletSr\bullet(1,0)

is a diffeomorphism onto R²\{the x<=0 ray} commonly referred to as "the polar coordinates on R^2"! ("\bullet" stands for the group action)

But there is no Log anywhere in this construction so perhaps this is not what you are after?
 
Hi quasar987,

thanks! your explanation was pretty clear. I simply didn't think of making such observations in terms of diffeomorphisms. And by the way you are right, the log-polar is not important in this case. I was just a bit confused.

One more thing I would be very interested to know. If I replace the rotation and scaling groups with two different and not well-known groups of transformations, can we do the same? What is the procedure to find a system of curvilinear coordinates in the plane, when we know the orbits of the points under the action of the two groups?
 
Well, in general, no, the analogue of the map we created for general group is not going to be a diffeomorphism. For instance, if instead of S^1 and R^1, you take two R^1's (both acting in the same way on R²), then we see fairly easily that the differential will be at every point non surjective. Similarly if we take two S^1's. The key for the above example to work was that the orbits are transverse.
 

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