diff --git a/docs/1b/ece106.md b/docs/1b/ece106.md index c8c5a1f..a9d124f 100644 --- a/docs/1b/ece106.md +++ b/docs/1b/ece106.md @@ -49,10 +49,9 @@ These rules also apply for a system in three dimensions: Although differential elements can be blindly used inside and outside an object (e.g., area), the rules break down as the **boundary** of an object is approached (e.g., perimeter). Applying these rules to determine an object's perimeter will result in the incorrect deduction that $\pi=4$. -Therefore, further approximations can be made by making a length $\dl=\sqrt{(dx)^2+(dy)^2}$ to represent the perimeter. +Therefore, further approximations can be made using the Pythagorean theorem to represent the perimeter. -!!! example - This reduces to $dl=\sqrt{\left(\frac{dy}{dx}\right)^2+1}$. +$$dl=\sqrt{(dx^2) + (dy)^2}$$ ### Polar coordinates @@ -79,6 +78,15 @@ $$dS=(dr)(rd\phi)$$ \end{align*} $$ +If $r$ does not depend on $d\phi$, part of the integral can be pre-evaluated: + +$$ +\begin{align*} +dS&=\int^{2\pi}_{\phi=0} r\ dr\ d\phi \\ +dS^\text{ring}&=2\pi r\ dr +\end{align*} +$$ + So long as the variables are independent of each other, their order does not matter. Otherwise, the dependent variable must be calculated first. @@ -90,7 +98,72 @@ So long as the variables are independent of each other, their order does not mat \int^b_a\sin^2\phi=\frac{b-a}{2} $$ -## Cartesian coordinates +The side length of a curve is as follows: -The axes in a Cartesian coordinate plane must be orthogonal so that increasing a value in one axis does not affect any other. The axes must also point in directions that follow the **right hand rule**. +$$dl=\sqrt{(dr^2+(rd\phi)^2}$$ +!!! example + The side length of the curve $r=e^\phi$ (Archimedes' spiral) from $0$ to $2\pi$: + + \begin{align*} + dl &=d\phi\sqrt{\left(\frac{dr}{d\phi}\right)^2 + r^2} \\ + \tag{$\frac{dr}{d\phi}=e^\phi$}&=d\phi\sqrt{e^{2\phi}+r^2} \\ + &=???????? + \end{align*} + +Polar **volume** is the same as Cartesian volume: + +$$dV=A\ dr$$ + +!!! example + For a cylinder of radius $R$ and height $h$: + + $$ + \begin{align*} + dV&=\pi R^2\ dr \\ + V&=\int^h_0 \pi R^2\ dr \\ + &=\pi R^2 h + \end{align*} + $$ + +### Moment of inertia + +The **mass distribution** of an object varies depending on its surface density $\rho_s$. In objects with uniformly distributed mass, the surface density is equal to the total mass over the total area. + +$$dm=\rho_s\ dS$$ + +The formula for the **moment of inertia** of an object is as follows, where $r_\perp$ is the distance from the axis of rotation: + +$$dI=(r_\perp)^2dm$$ + +!!! example + In a uniformly distributed disk rotating about the origin like a CD with mass $M$ and radius $R$: + + $$ + \begin{align*} + \rho_s &= \frac{M}{\pi R^2} \\ + dm &= \rho_s\ r\ dr\ d\phi \\ + dI &=r^2\ dm \\ + &= r^2\rho_s r\ dr\ d\phi \\ + &= \rho_s r^3dr\ d\phi \\ + I &=\rho_s\int^{2\pi}_{\phi=0}\int^R_{r=0} r^3dr\ d\phi \\ + &= \rho_s\int^{2\pi}_{\phi=0}\frac{1}{4}R^4d\phi \\ + &= \rho_s\frac{1}{2}\pi R^4 \\ + &= \frac 1 2 MR^2 + \end{align*} + $$ + +## Electrostatics + +!!! definition + - The **polarity** of a particle is whether it is positive or negative. + +The law of **conservation of charge** states that electrons and charges cannot be created nor destroyed, such that the **net charge in a closed system stays the same**. + +The law of **charge quantisation** states that charge is discrete — electrons have the lowest possible quantity. + +Please see [SL Physics 1#Charge](/sph3u7/#charge) for more information. + +**Coulomb's law** states that for point charges $Q_1, Q_2$ with distance from the first to the second $\vec R_{12}$: + +$$\vec F_{12}=k\frac{Q_1Q_2}{||R_{12}||^2}\hat{R_{12}}$$ diff --git a/docs/1b/math119.md b/docs/1b/math119.md index a49366b..c53058f 100644 --- a/docs/1b/math119.md +++ b/docs/1b/math119.md @@ -56,7 +56,7 @@ In practice, this means that if any two paths result in different limits, the li Along $y=0$: - $$\lim_{(x,0)\to(0, 0) ... = 1$$ + $$\lim_{(x,0)\to(0, 0)} ... = 1$$ Along $x=0$: