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# ECE 106: Electricity and Magnetism
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## MATH 117 review
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!!! definition
A definite integral is composed of:
- the **upper limit**, $b$,
- the **lower limit**, $a$,
- the **integrand**, $f(x)$, and
- the **differential element**, $dx$.
$$\int^b_a f(x)\ dx$$
The original function **cannot be recovered** from the result of a definite integral unless it is known that $f(x)$ is a constant.
## N-dimensional integrals
Much like how $dx$ represents an infinitely small line, $dx\cdot dy$ represents an infinitely small rectangle. This means that the surface area of an object can be expressed as:
$$dS=dx\cdot dy$$
Therefore, the area of a function can be expressed as:
$$S=\int^x_0\int^y_0 dy\ dx$$
where $y$ is usually equal to $f(x)$, changing on each iteration.
!!! example
The area of a circle can be expressed as $y=\pm\sqrt{r^2-x^2}$. This can be reduced to $y=2\sqrt{r^2-x^2}$ because of the symmetry of the equation.
$$
\begin{align*}
A&=\int^r_0\int^{\sqrt{r^2-x^2}}_0 dy\ dx \\
&=\int^r_0\sqrt{r^2-x^2}\ dx
\end{align*}
$$
!!! warning
Similar to parentheses, the correct integral squiggly must be paired with the correct differential element.
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These rules also apply for a system in three dimensions:
| Vector | Length | Area | Volume |
| --- | --- | --- | --- |
| $x$ | $dx$ | $dx\cdot dy$ | $dx\cdot dy\cdot dz$ |
| $y$ | $dy$ | $dy\cdot dz$ | |
| $z$ | $dz$ | $dx\cdot dz$ | |
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 $\pi=4$.
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Therefore, further approximations can be made using the Pythagorean theorem to represent the perimeter.
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$$dl=\sqrt{(dx^2) + (dy)^2}$$
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### Polar coordinates
Please see [MATH 115: Linear Algebra#Polar form](/1a/math115/#polar-form) for more information.
In polar form, the difference in each "rectangle" side length is slightly different.
| Vector | Length difference |
| --- | --- |
| $\hat r$ | $dr$ |
| $\hat\phi$ | $rd\phi$ |
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Therefore, the change in surface area can be approximated to be a rectangle and is equal to:
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$$dS=(dr)(rd\phi)$$
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!!! example
The area of a circle can be expressed as $A=\int^{2\pi}_0\int^R_0 r\ dr\ d\phi$.
$$
\begin{align*}
A&=\int^{2\pi}_0\frac{1}{2}R^2\ d\phi \\
&=\pi R^2
\end{align*}
$$
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If $r$ does not depend on $d\phi$, part of the integral can be pre-evaluated:
$$
\begin{align*}
dS&=\int^{2\pi}_{\phi=0} r\ dr\ d\phi \\
dS^\text{ring}&=2\pi r\ dr
\end{align*}
$$
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So long as the variables are independent of each other, their order does not matter. Otherwise, the dependent variable must be calculated first.
!!! tip
There is a shortcut for integrals of cosine and sine squared, **so long as $a=0$ and $b$ is a multiple of $\frac\pi 2$**:
$$
\int^b_a\cos^2\phi=\frac{b-a}{2} \\
\int^b_a\sin^2\phi=\frac{b-a}{2}
$$
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The side length of a curve is as follows:
$$dl=\sqrt{(dr^2+(rd\phi)^2}$$
!!! 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:
$$dI=(r_\perp)^2dm$$
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If the axis of rotation is perpendicular to the plane of the object, $r_\perp=r$. If the axis is parallel, $r_\perp$ is the shortest distance to the axis. Setting an axis along the axis of rotation is easier.
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!!! 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.
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**Coulomb's law** states that for point charges $Q_1, Q_2$ with distance from the first to the second $\vec R_{12}$:
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$$\vec F_{12}=k\frac{Q_1Q_2}{||R_{12}||^2}\hat{R_{12}}$$
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!!! warning
Because Coulomb's law is an experimental law, it does not quite cover all of the nuances of electrostatics. Notably:
- $Q_1$ and $Q_2$ must be point charges, making distributed charges inefficient to calculate, and
- the formula breaks down once charges begin to move (e.g., if a charge moves a lightyear away from another, Coulomb's law says the force changes instantly. In reality, it takes a year before the other charge observes a difference.)
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### Dipoles
An **electric dipole** is composed of two equal but opposite charges $Q$ separated by a distance $d$. The dipole moment is the product of the two, $Qd$.
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The charge experienced by a positive test charge along the dipole line can be reduced to as the ratio between the two charges decreases to the point that they are basically zero:
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$$\vec F_q=\hat x\frac{2kQdq}{||\vec x||^3}$$
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## Maxwell's theorems
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Compared to Coulomb's law, $Q_1$ creates an electric field around itself — each point in space is assigned a vector that depends on the distance away from the charge. $Q_2$ *interacts* with the field. According to Maxwell, as a charge moves, it emits a wave that carries information to other charges.
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The **electric field strength** $\vec E$ is the force per unit *positive* charge at a specific point $p$:
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$$\vec E_p=\lim_{q\to 0}\frac{\vec{F}}{q}$$
Please see [SL Physics 1#Electric potential](/sph3u7/#electric-potential) for more information.
### Electric field calculations
If charge is distributed over a three-dimensional object, integration similar to moment of inertia can be used. Where $dQ$ is an infinitely small point charge at point $P$, $d\vec E$ is the electric field at that point, and $r$ is the vector representing the distance from any arbitrary point:
$$d\vec E = \frac{kdQ}{r^2}\hat r$$
!!! warning
As the arbitrary point moves, both the direction and the magnitude of the distance from the desired point $P$ change (both $\hat r$ and $r$).
Generally, if a decomposing the vector into Cartesian forms $d\vec E_x$, $d\vec E_y$, and $d\vec E_z$ is helpful even if it is easily calculated in polar form because of the significantly easier ability to detect symmetry in the shape. Symmetry about the axis allows deductions such as $\int d\vec E_y=0$, which makes calculations easier.
In a **one-dimensional** charge distribution (a line), the charge density is used in a similar way as moment of inertia's surface density:
$$dQ=\rho_\ell d\ell$$
**Two-dimensional** charge distributions are more or less the same, but polar or Cartesian forms of the surface area work depending on the shape.
$$dQ=\rho_s dS$$
!!! example
A rod of uniform charge density and length $L$ has a charge density of $p_\ell=\frac{Q}{L}$.
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1. Determine the formula for the charge density $\rho$
2. Choose an origin and coordinate system (along the axes of the object when possible)
3. Choose an arbitrary point $A$ on the charge
4. Create a right-angle triangle with $A$, the desired point, and usually the origin
5. Attempt to find symmetry
6. Solve
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## Gauss's law
!!! definition
- A **closed surface** is any closed three-dimensional object.
- **Electric flux** represents the number of electric field lines going through a surface.
At an arbitrary surface, the **normal** to the plane is its vector form:
$$\vec{dS}=\vec n\cdot dS$$
The **electric flux density** $\vec D$ is an alternate representation of electric field strength. In a vacuum:
$$\vec D = \epsilon_0\vec E$$
**Electric flux** is the electric flux density multiplied by the surface area at every point of an object.
$$\phi_e=\epsilon_0\int_s\vec E\bullet\vec{dS}$$
The flux from charges outside a closed surface will **always be zero at the surface**. A point charge in the centre of a closed space has a flux equal to its charge. Regardless of the charge distribution or shape, the **total flux** through a closed surface is equal to the **total charge within** the closed surface.
$$\oint \vec D\bullet\vec{dS}=Q_\text{enclosed}$$
This implies $\phi_e>0$ is a net positive charge enclosed.
!!! warning
Gauss's law only applies when $\vec E$ is from all charges in the system
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### Charge distributed over a line/cylinder
!!! warning "Limitations"
To apply this strategy, the following conditions must hold:
- $Q$ must not vary with the length of the cylinder or $\phi$
- The charge must be distributed over either a cylindrical surface or the volume of the cylinder.
- In the real world, $r$ must be significantly smaller than $L$ as an approximation.
- The strategy is more accurate for points closer to the centre of the wire.
Please see [Maxwell's integral equations#Gauss's law](https://en.wikiversity.org/wiki/MyOpenMath/Solutions/Maxwell%27s_integral_equations) for more information.
**Outside** the radius $R$ of the cylinder of the Gaussian surface, the enclosed charge is, where $L$ is the length of the cylinder:
$$Q_{enc}=\pi R^2\rho_0L$
such that the field at any radius $r>R$ is equal to:
$$\vec E(r)=\frac{\rho_0\pi R^2}{2\pi\epsilon_0r}\hat r$$
**Inside** the radius $R$ of the cylinder, the enclosed charge depends on $r$. For a uniform charge density:
$$Q_{enc}=\pi r^2\rho_0L$$
such that the field at any radius $r< R$ is equal to:
$$\vec E(r)=\frac{\rho_0}{2\epsilon_0}r\hat r$$
The direction of $\vec E$ should always be equal to that of $\vec r$. Generally, where $lim$ is $r$ if $r$ is *inside* the cylinder or $R$ otherwise, $\rho_v$ is the function for charge density based on radius, and $r_1$ is hell if I know:
$$\epsilon_0 E2\pi rL=\int^{lim}_0\rho_v(r_1)2\pi r_1L\ dr_1$$
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### Charge distributed over a plane
!!! warning
To apply this strategy, the following conditions must hold:
- $Q$ must not vary with the lengths of the plane
- The charge must be distributed over a plane or slab
- In the real world, the thickness $z$ must be significantly smaller than the lengths as an approximation
Where $\rho_v$ is an **even** surface density function and $lim$ is from $0$ to $z$ if the desired field is outside of the charge, or $0$ to field height $h$ if it is inside the charge:
$$\epsilon_0 E=\int_{lim}\rho_v\ dh_1$$
Any two points have equal electric fields regardless of distance due to the construction of a uniform electric field.
Where $\rho_v$ is not an even surface density function, $d$ is the thickness of the slab, and $E$ is the electric field **outside** the slab:
$$2\epsilon_0E = \int^d_0\rho_v(A)dh_1$$
Where $E$ is the electric field **inside** the slab at some height $z$:
$$E=\frac{\rho_0}{4\epsilon_0}(2z^2-d^2),0\leq z\leq d$$
If $E$ is negative, it must point opposite the original direction ($\hat z$).
Generally:
1. Determine $\vec E$ outside the slab.
2. Set one outside surface and one inside surface as a pillbox and apply rules.
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## Electrostatic potential
At a point $P$, the electrostatic potential $V_p$ or voltage is the work done per unit positive test charge from infinity to bring it to point $P$ by an external agent.
$$
V_p=\lim_{q\to 0^+}\frac{W_i}{q} \\
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W_I=\int^p_\infty\vec F_I\bullet \vec{dl}=\Delta U=QV_p
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$$
Because the desired force acts opposite to the force from the electric field, as long as $\vec E$ is known at each point:
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$$
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V_p=-\int^p_\infty\vec E\bullet\vec{dl} \\
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V_p=-\int^p_\infty E\ dr
$$
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The work done only depends on initial and final positions — it is conservative, thus implying Kirchoff's voltage law.
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Where $\vec dl$ is the path of the test charge from infinity to the point, and $\vec dr$ is the direct path from the origin through the point to the charge, because $dr=-dl$:
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$$\vec E\bullet\vec{dl}=Edr$$
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Therefore, the potential due to a point charge is equal to:
$$V_p=-\int^p_\infty\frac{kQ}{r^2}dr=\frac{kQ}{r}$$
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**Positive** charges naturally move to **lower** potentials ($V$ decreases) while negative charges do the opposite. Potential energy always decreases.
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In order to calculate the voltage for charge distributions:
- If $\vec E$ is easy to find via Gauss law:
$$V_p=-\int^p_\infty\vec E\bullet\vec{dl}$$
- If the charge is asymmetric:
$$V_p=\int_\text{charge dist}\frac{kdQ}{r}$$
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The electric field always points in the direction of **lower** potential, and is equal to the **negative gradient** of potential.
$$\vec E=-\nabla V$$
If $\vec E$ is constant:
$$\vec E=\frac{Q_{enc\ net}}{\epsilon_0\oint dS}$$