Polar integration - Length and Area of curve

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Discussion Overview

The discussion revolves around the derivation of the area and length of polar curves in mathematics, specifically addressing the differences in approaches to calculating these two quantities. Participants explore the mathematical foundations and reasoning behind the formulas used for area and length in polar coordinates.

Discussion Character

  • Technical explanation
  • Debate/contested
  • Mathematical reasoning

Main Points Raised

  • One participant presents the formula for the area of a polar curve as A=(1/2)∫ r² d(theta) and questions why a similar approach does not yield the correct length of the curve.
  • Another participant asserts that the length of a curve is not generally the rate of change of the area, providing a counterexample involving a square.
  • A participant seeks clarification on where their derivation of the length of the curve is incorrect.
  • It is noted that the derivation violates the Pythagorean theorem, leading to a discussion about the differential length element ds.
  • One participant argues that they are treating each length element as part of a circle, similar to the area derivation.
  • Another participant counters that this approach cannot be applied to curves in the same way as areas, emphasizing the differences in how deviations are treated in each case.
  • A detailed explanation is provided regarding the parametrization of the curve and the correct expression for the arc length, reinforcing that the initial assumption about ds was incorrect.
  • The area formula is discussed in terms of the radius vector and the area swept out, with a mathematical derivation presented to support the area calculation.

Areas of Agreement / Disagreement

Participants do not reach a consensus on the derivation of the length of the curve, with multiple competing views on the validity of the approaches presented. The discussion remains unresolved regarding the specific errors in the initial reasoning.

Contextual Notes

Participants highlight limitations in the assumptions made about the relationship between area and length in polar coordinates, particularly regarding the treatment of differential elements and the applicability of certain mathematical principles.

rahuljayanthb
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The area of a polar curve is given by A=(1/2)∫ r2 d (theta).
this can be interpreted as δA= ∏r2δ(theta)/2∏ (treating the area element as the area of a sector of a circle with angle δ(theta).)
taking limit of δ(theta)→0,
dA= [STRIKE]∏[/STRIKE]r2 d(theta)/2[STRIKE]∏[/STRIKE]=1/2 (r2d(theta) )
there fore A=1/2∫r2 d(theta).

By the same logic, shouldn't length of a polar curve be L=∫[STRIKE]2∏[/STRIKE]r d(theta)/[STRIKE]2∏[/STRIKE]=∫r d(theta)?

the actual equation for curve length is L=∫√(r2+r'2)d(theta).

why is this approach giving me an incorrect equation in the second case but a correct one in the first?

ps. the equation for length of a curve can also be derived by partially differentiating the equation for area by r: ∂A/∂r=L. This is again consistent with looking at length of a curve as the rate of change of area.
 
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The length of a curve is not, in general, the rate of change of the area.

As a simple example, the circumference of a square is 4l, whereas the area is l^2
 
but where is the derivation of the length of curve wrong?
 
It violates the Pythagorean theorem, for example.

You have, differentially, that the curve length ds equals:
ds=\sqrt{(dr)^{2}+(rd\theta)^{2}}
 
but i am treating every length element of the curve as a part of a circle of appropriate radius. so i am treating the curve as a conglomerate of numerous circular elements just in the area derivation.
 
well, but that is precisely what you cannot do.

For areas, deviations from area of the circular section are negligible relative to the area for the circular section, while a similar negligibility is not present for the CURVE.

Basically, the reason why this works for areas is that an area of "tiny*tiny" can be neglated relative to "tiny", while for curves "tiny" can't be neglected relative to.."tiny"
 
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Ok, what you consider here is a curve parametrized with the polar angle \theta of polar coordinates in a plane. Your position vector reads
\vec{r}=\vec{r}(\theta)=r(\theta) \hat{r}(\theta).
The arc element is
\mathrm{d} s=|\mathrm{d} \vec{r}|=\mathrm{d} \theta|r' \hat{r}+r \partial_{\theta} \hat{r}|=\mathrm{d} \theta \sqrt{r^2 +(r')^2},
which indeed shows that your assumption about \mathrm{d} s is wrong and the "actual equation" is right.

The area is another thing. Your formula gives the area swept out by the above radius vector. This area is thus parametrized by
\vec{r}(\lambda,\theta)=\lambda r(\theta) \hat{r}(\theta)
with \lambda \in [0,1]. The area element is
\mathrm{d} F=\mathrm{d} \lambda \mathrm{d} \theta |\partial_\lambda \vec{r} \times \partial_{\theta} \vec{r}|=\mathrm{d} \lambda \mathrm{d} \theta |\vec{r}(\theta) \times \partial_{\theta} \vec{r}|=\mathrm{d} \lambda \mathrm{d} \theta \lambda r^2(\theta) |\hat{r} \times \hat{\theta}|=\lambda r^2(\theta).
The total area swept out by the radius vector from angle \theta_1 to \theta_2 thus is
F=\int_0^{1} \mathrm{d} \lambda \int_{\theta_1}^{\theta_2} \mathrm{d} \theta \; \lambda r^2(\theta)=\frac{1}{2} \int_{\theta_1}^{\theta_2} \mathrm{d} \theta \; r^2(\theta).
As you see, here one component of \partial_{\theta} \vec{r} doesn't contribute, because of the cross product in the formula for the area element!
 

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