Polar Coordinates: A Nicer Way to Define?

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Discussion Overview

The discussion revolves around the definition and transformation of polar coordinates from rectangular coordinates, exploring the mathematical implications and potential issues with various definitions. Participants examine the validity of different mappings and the conditions under which they hold, as well as the implications for physical concepts involving angular coordinates.

Discussion Character

  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant defines polar coordinates using a transformation that involves the tangent function, but notes a failure at certain points where the tangent is undefined.
  • Another participant corrects the initial transformation, suggesting the use of the arctangent function instead of tangent for a more accurate definition.
  • A participant introduces the concept of diffeomorphisms, arguing that the transformation should be a smooth, invertible map, and points out that the proposed transformation is not a diffeomorphism.
  • There is a question raised about the necessity of the transformation being a diffeomorphism, with some participants expressing confusion over this requirement.
  • A later reply suggests a simpler definition of the mapping using cosine and sine functions, establishing a bijection almost everywhere between the coordinate systems.
  • Another participant questions the constraints on the angle theta in the context of potential energy equations, expressing confusion about the justification for treating theta as unrestricted in certain physical scenarios.

Areas of Agreement / Disagreement

Participants express differing views on the appropriate definitions and transformations for polar coordinates, with no consensus reached on the necessity of diffeomorphisms or the treatment of angular coordinates in physical equations.

Contextual Notes

Participants highlight limitations in the definitions provided, such as the failure of certain transformations at specific points and the need for careful consideration of the domains of the functions involved.

quasar987
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As I understand it, the polar coordinates of a point is defined by the rectangular coordinates of that point according to the transformation T from R² to R² defined by

[tex]T:(x,y)\mapsto (\sqrt{x^2+y^2},tan\left(\frac{y}{x}\right))[/tex]

But this definition fails for y=pi and x=2 because tan(pi/2) is not defined.

We could defined it this way for [itex](x,y)\in \mathbb{R}^2 \backslash \{(x,y) \ \vert \ y/x = (n+1/2)\pi, \ n\in \mathbb{Z}\}[/itex], and by

[tex]T:(x,y)\mapsto (\sqrt{x^2+y^2}, Arccos_n \left(\frac{x}{\sqrt{x^2+y^2}}\right))[/tex]

for [itex](x,y) \in \{(x,y) \ \vert \ y/x = (n+1/2)\pi, \ n\in \mathbb{Z}\}[/itex] and where Arccos_n is the inverse function of cos in the interval containing (n+1/2)pi.. i.e. [itex]Arccos_n(z): [-1,1]\rightarrow [n\pi, (n+1)\pi][/itex].

This is phenomenally ugly. Is there a nicer way to define the polar coordinates?
 
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quasar987 said:
[tex]T:(x,y)\mapsto (\sqrt{x^2+y^2},tan\left(\frac{y}{x}\right))[/tex]
That has never been correct, this is somewhat more correct:
[tex]T:(x,y)\mapsto (\sqrt{x^2+y^2},arctan\left(\frac{y}{x}\right))[/tex]
 
Oh damn!

But more like 'phew!' really. :smile:
 
These basis changes should be made through diffeomorphisms.Obviously

[tex]\hat{T}:(x,y)\mapsto \left(\sqrt{x^{2}+y^{2}},\arctan \frac{y}{x}\right)[/tex]

is not a diffeomorphism from [tex]\mathbb{R}^2}\rightarrow \mathbb{R}^{2}[/tex].

Daniel.
 
What does that mean Daniel?
 
Invertible [itex]C^{\infty}[/itex] maps from one space to another.

U'll have to exclude the Oy axis.

Daniel.
 
Last edited:
Well I don't see your point. Why must the transformation from rectangular to polar coord. be a diffeomorphism absolutely?!
 
Pick the point [itex](0,2)[/itex] in cartesian.Can your mapping send it to polar coords...?

Daniel.
 
No. So how do you suggest we avoid this problem?
 
  • #10
It's simplest to define the mapping by through:
[tex]x=r\cos\theta, y=r\sin\theta[/tex]

This sets up a bijection almost everywhere between (x,y) and [tex](r,\theta)[/tex].
(That is with (x,y) on the plane, r on the non-negative half-axis, and [tex]\theta[/tex] on the half-open interval [tex][0,2\pi)[/tex]
 
Last edited:
  • #11
If theta is traped in the interval [0, 2pi), then surely when we say that the potential energy of an object free to rotate around the z axis is

[tex]V(\theta) = -\int_{\theta _s}^{\theta}N\z(\theta)d\theta[/tex] (Symon pp.212)

the theta involved in this equation is not the theta of polar/cylindrical coordinates (i.e. constrained in [0, 2pi)), is it?

I had succeeded in proving this equation but it involved treating the polar angle has being free to take any value in [itex](-\infty, \infty)[/itex]. I was trying to justify that it was justified to do that. But now I'm a little confused. Is it justified?
 

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