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Today we continue with polar equations for Lab 15.
In particular, we want to talk about area of polar curves.
Let's start with a circle of radius r, centered at the origin, and see how we might adapt the "familiar formulas" to more exotic shapes:
So as $\theta$ varies from $a$ to $b$, the radius $r$ will vary as $f(\theta)$.
In the case of a circle, the formula for length swept out is $rd{\theta}$. If we integrate for a circle of fixed radius $r$, we get \[ L = \int_{0}^{2\pi} r d\theta = 2\pi r \] (the circumference formula!). How must we adapt things if $r$ varies as $r=f(\theta)$?
It turns out that we need to tweak that formula just a bit: \[ L = \int_{a}^{b}{ \sqrt{ r^2 + \left( \frac{dr}{d\theta} \right)^2 } }\ d\theta = \int_{a}^{b}{ \sqrt{ f(\theta)^2 + f'(\theta)^2 } }\ d\theta \]
Notice that this formula give the proper result in the case of a circle of radius $r$ centered at the origin, because in that case the second piece -- $\frac{dr}{d\theta}$ -- is 0! There is no change in $r$ as $\theta$ changes, so the rate of change is 0....
From this we see that going from the specific to the general can be dangerous. That being said, we often do dangerous things, and sometimes they work. See what happens in the case of area!:)
Thus, in the picture above, $\Delta A \approx r \frac{r \theta}{2}$ (recall arc length above is about $r \theta$).
Hence, when we have an infinitesimally small angle $d\theta$, the approximation should be exact: $dA=\frac{r^2}{2}d\theta$, and \[ A=\int_{a}^{b} \frac{1}{2}r^2\ d\theta=\int_{a}^{b} \frac{1}{2}f(\theta)^2 \ d\theta \] is indeed the area of that shaded region on the right above.