What Is the Role of the r^2 Term in the Polar Arc Length Formula?

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Discussion Overview

The discussion revolves around the role of the r² term in the polar arc length formula, specifically in the context of understanding its geometric and analytical implications. Participants explore the meaning of this term in relation to the arc length calculation in polar coordinates, addressing both theoretical and practical aspects.

Discussion Character

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

Main Points Raised

  • One participant questions whether the r² term represents an initial or final distance from the origin or the change in r between two points.
  • Another participant describes the arc length in terms of a parametrized curve, indicating that the r² term relates to the distance from the origin and contributes to the overall arc length calculation.
  • A participant distinguishes between geometric and analytic reasons for the presence of the r² term, suggesting that the derivation is straightforward but the geometric interpretation is more complex.
  • One participant asserts that the r² term corresponds to the distance from the origin, emphasizing its significance in calculating arc length for small curves on a sphere.
  • Another participant challenges a proposed distance calculation between two polar points, stating that the differential relation is only valid for very close points and suggesting the need for trigonometric or Cartesian methods for larger distances.
  • A participant provides a visual explanation using the Pythagorean theorem, indicating how the arc length is derived from infinitesimal increments in polar coordinates.

Areas of Agreement / Disagreement

Participants express differing views on the interpretation of the r² term and its implications for arc length calculations. While some agree on its geometric significance, others highlight the limitations of the differential relation in broader contexts, indicating that the discussion remains unresolved.

Contextual Notes

Participants note that the differential relation is akin to a Taylor expansion, which may not hold for larger distances. The discussion also touches on the need for careful consideration of the angle's dependence on distance when interpreting the r² term.

planck42
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In the polar formula for arc length, [tex]ds^{2}=dr^{2}+r^{2}d{\theta}^{2}[/tex], what is the exact meaning of the [tex]r^2[/tex] term multiplying [tex]d{\theta}^2[/tex]? Is it an initial distance from the origin? A final distance from the origin? The change in r from point a to point b? This baffles me to no end and nothing explains it.
 
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God I hate this stuff. But after you use it, you kind of realize how much effort it saves.

This is the meaning of that rather "disembodied" statement.

Let's draw a curve through space. And now let's parametrize that curve with a parameter t. So along this path, [tex]r=\tilda r(t), \ \ \theta = \tilda \theta (t)[/tex].
Then the arclength satisfies the following 'differential' equation:

[tex](\frac{ds}{dt})^2 = (\frac{d\ r (t)}{dt})^2 + r^2 (\frac{d\ \theta (t)}{dt})^2[/tex]

I've included the (t) thing to make the method of calculation explicit. You literally differentiate the function r(t) wrt t. r=r(t) is a horrible abuse of notation that actually gets me confused from time to time but...it saves a lot of time too. Haha.
 
Do you mean a geometric reason, or an analytic reason?

To see how it got there, just consider the following:

[tex] dS = \sqrt{1 + (\frac{dy}{dx})^2}[/tex]

Let [tex]y = r \sin \theta[/tex] and [tex]x = r \cos \theta[/tex] and work it out and you'll get your r^2 factor on the [tex]d\theta[/tex]
 
I mean a geometric reason; the derivation is no problem.
 
It gives the arclength gained by increasing r by dr and theta by dtheta.

[tex] (\frac{ds}{dt})^2 = (\frac{d\ r (t)}{dt})^2 + r^2 (\frac{d\ \theta (t)}{dt})^2 [/tex]
So yes, the r^2 corresponds to how far you are from the origin.
Think about small curves on a sphere. If your r is large, then your ds is going to be larger, for a given dtheta.
 
Let's take an example: suppose I am moving from the polar point [tex](2, \frac{\pi}{4})[/tex] to [tex](3, \frac{\pi}{2})[/tex]. Would my distance traveled be [tex]1+\frac{{\pi}^{2}}{4}[/tex]?
 
No, the relation you stated in the beginning is a differential relation, meaning it is good only for really close points. (It's like a taylor expansion)

Otherwise you need to develope a formula using trigonometry or using the definition of distance via cartesian coordinates then substituting with polar coordinates.

Back to your original question: dtheta denotes a change in the angle. But as you may know, the angle between two rays doesn't depend on their length. So the information of the angle itself doesn't give you a measure of distance. At small distances from the origin, taking a small angle difference will give you a small distance (the arc of a small circle). At large distances, taking a small angle step will give you a larger distance.
Therefore the r dependence comes in.
 
http://img716.imageshack.us/img716/3151/arcy.jpg

Differentiable curves exhibit local linearity, so if we zoom up to infinitesimal scales the curve is approximately a straight line. We wish to find the infinitesimal increments of the arc length of the curve between polar coordinates [itex](r,\theta)[/itex] and [itex](r+dr, \theta + d\theta)[/itex].

By the Pythagorean theorem, [itex]ds^2 = dr^2 + (ab)^2[/itex], but the length of the line segment ab can be approximated by the length of the arc that passes through a and b of the circle centered at the origin of radius r. The length of this arc is given by [itex]r d\theta[/itex].
 
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