Refraction of Obliquely Incident Electromagnetic Waves

Tackling oblique-incidence EM wave refraction by ripping E and B fields into normal and parallel boundary components, then matching all four boundary conditions.

Haa………… Let me take one loo~~~ng sigh and get into it: electromagnetic waves refracting at oblique incidence.

We’ll use two homogeneous, isotropic, lossless media, with no free surface charge or current. The electric field is in the plane of incidence: this is p polarization.

I described the situation like this.

Equation from the original notes

This time I’m ditching the way we described it before, a wave traveling in the $z$ direction, and describing it as an electromagnetic wave traveling through 3D space (really 2D), then going through the boundary conditions.

(Unlike normal incidence, I’ll have to use all 4 boundary conditions, right?)

Equation from the original notes

Now here too, even if we don’t know for sure, we can guess that it’ll be one of these two, like this: fixed-end reflection or free-end reflection.

And what I’m also going to do is rip the vector (at the boundary) apart into the direction normal to the boundary ($z$) and the direction parallel to the boundary ($x$), and then try to match the boundary conditions. (Not sure if it’ll work.) So first, let’s rip each of the electric and magnetic fields apart and describe them, go go go!

Equation from the original notes

Equation from the original notes

Equation from the original notes

Applying the boundary conditions

Boundary conditions~~

Eq

Haa…….. the second sigh, go go go. Now I’m going to apply those one by one…… T_T ugh. T_T

1 !

Equation from the original notes

2 !

Equation from the original notes

3 !

Eq

Phew~ no $B$ perpendicular to the boundary! Yessss!!

4 !

Equation from the original notes

Blasting the exponentials away

Excluding number 3, we got three equations, and here’s what I’m going to do now: I’m going to blast all of these e^{i(\vec{k}\cdot\vec{r}-\omega t)} away.

The logic by which we can blast them is this: those 3 equations have to hold anywhere on the boundary $z=0$, and when $x$, $y$ change just a teeeeeeny bit, those terms each turn out different!

In that case, the only way they can survive as equalities is that those terms containing the variables all have to be the same!

Equation from the original notes

With this, those equations can alllll hold anywhere on $z=0$! And \theta_{inc} = \theta_{ref}: using this, let me clean up those 3 equations a bit more.

1

Equation from the original notes

2

Equation from the original notes

3

Equation from the original notes

If you mess around with and manipulate the first equation, it comes out the same as the third equation. So we’ll use the second equation and the third equation to work out the relationship between incident and reflected, and between incident and transmitted.

Before that,

Equation from the original notes

///////

Eq

let’s make these little agreements and write the equations a bit more comfortably:

Equation from the original notes

Equation from the original notes

That’s the result for our p-polarized wave.

Brewster’s angle

But!!! But there’s a cool case!! (When is that!?)

There’s a special case where \alpha = \beta holds and no reflection happens at all!!!!! (oh my, for real!?) Let me work it out.

Equation from the original notes

Here’s the trick I’m going to pull: the Pythagorean theorem

Equation from the original notes

and Snell’s law

Equation from the original notes

I’m going to play with these. That is,

Equation from the original notes

and if I plug this into that very first equation up there

Equation from the original notes

So there’s an angle of incidence at which alpha and beta are equal!!!! Apparently that angle is called Brewster’s angle!

Reflectance and transmittance

Well, anyway, getting back on track,,,, now:

“How much is reflected, and how much is refracted and transmitted??~!?~!?”

Okay then, we just need the magnitudes of the energy fluxes normal to the boundary, right?! The reflected wave travels toward negative $z$, so we use the positive magnitude of its $z$ component here~~~~~

Equation from the original notes

Oh, and you haven’t forgotten this, right?

Equation from the original notes

Equation from the original notes

Reflectance ($R$)

Equation from the original notes

Transmittance ($T$)

Equation from the original notes

Eq

Here too (of course) $R + T = 1$ is still satisfied!!


Heads-up. The figures here are the original notes, slips and all. A few things to watch for:

  • Snell’s law has a sine on both sides: $n_1 \sin\theta_{inc} = n_2 \sin\theta_{trans}$ (one picture writes $n_1 \cos\theta_{inc}$); the pictures after it use the right form.

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