7. Electromagnetic Waves 7A. Plane Waves Complex Notation • Consider Maxwell’s Equations with no sources • We are going to search for waves of the form f r, t cos k r t or f r, t sin k r t • To make things as general as possible, we write f r, t Re feik r it 1 2 feik r it 12 f *e ik r it D 0 B E B t H D t • To save ourselves work, we will simply keep track of feikr it – Just remember to take the real part at the end k D 0 k B • Space derivatives of expressions like this become ik k E B • Time derivatives of expressions like this become –i k H D • Maxwell equations are now Linear Media E, D, H, B ~ eikxit • The reaction of the medium will generally have the same frequency as the fields only if the material is linear D E • We therefore assume the medium is linear B H • In general, and will depend on frequency k D 0 k B k E B k H D • It is possible for there to be a phase shift between D and E or B and H – Similar to a phase shift for a damped, driven harmonic oscillator • This can be show up as complex and • We will (for now) assume they are both real k E 0 k B • Most common situation is = 0 and > 0 k E B • With these assumptions, our equations become k B E Finding the Wave Velocity • Multiply second equation by E, B ~ eikxit • Substitute third equation 2B k E k k B k k B k 2B • • • • • 1 2B k 2B Use kB = 0 k We therefore have We define the phase velocity v and the index of refraction n as We therefore have c v Recall that c200 = 1, so n k n • What does phase velocity mean? k E 0 k B k E B k B E 1 c v n 0 0 E, B ~ Re eik x it ~ cos k x t cos kkˆ x kvt cos k kˆ x vt • It’s the speed at which the peaks, valleys, and nodes move The Electric Field and Magnetic Flux Density ik x it c E , B ~ e v k n • Electric field will take the form E E0 eik x it – E0 is a constant vector • From the first equation, we see that E0 k E0 k k E 0 k B k E B k B E • The magnetic field can be nˆ ik x it 1 i k x i t B k E e found from second equation 0 B k E0 e c • Magnetic field is also transverse • Given k, the index of refraction n, and the constant transverse vector E0, we have completely described the wave Time-Averaged Energy Density E E0 eik x it B B 0 eik x it • First rewrite B u Re E0e E0e 1 8 nˆ k E0 eik x it c B0 kˆ E0 • Energy density is 1 2 B ik x it 2 ik x it Re B0e 1 2 * ik x it 2 0 E e ik x it 2 18 1 B0eikxit B*0eikxit 14 E0 E*0 14 1B 0 B*0 14 Re E02 e2ik x 2it 1B 02 e2ik x 2it • The last terms oscillate at frequency 2 - too fast to measure • If we do a time average, these terms go away, so u 14 E0 E*0 14 1B0 B*0 14 E0 E*0 14 1 E0 E*0 u 12 E0 E*0 1 c v n Time-Averaged Poynting Vector B B 0 eik x it E E0 eik x it B0 kˆ E0 • The Poynting vector is 1 ik x it ik x it 1 Re E e Re B e 0 0 S E H E B 1 4 1 E e ik x it 0 E e 14 1 E0 B*0 E*0 B0 • If we time average, we get S 1 4 1 E 0 • We note that: B E B0 * 0 S B e 2 Re E B e * ik x it 0 * 0 1 ik x it 0 0 * ik x it 2 0 B e 2ik x 2it 0 1 1ˆ * * ˆ ˆ E0 k E0 E0 k E0 k E0 E*0 2 4 kˆ u vkˆ u • Energy moves in direction of k at phase velocity v 7B. Polarization and Stokes Parameters The Polarization Vectors The electric field is transverse E0 k We define two polarization vectors ε1 and ε 2 * k ε 0 ε ε They are chosen to be orthogonal to k and to each other: i 1 2 If we use real polarization vector 1, typically define the other to be ε kˆ ε 2 1 For example, if k is in z-direction, ε1 xˆ , ε 2 yˆ then we could pick E0 E1ε1 E2ε2 • An arbitrary wave is then described by two complex numbers • That means four real parameters Re E1 , Im E1 , Re E2 , Im E2 • The magnetic field is then given by • • • • • B0 kˆ E0 E1ε 2 E2ε1 • The intensity (magnitude of time-averaged Poynting vector) is I 1 2 E1 E2 2 2 Linear, Circular, Elliptical Polarization E0 E1ε1 E2ε2 • If E1 and E2 are proportional with a real proportionality constant, then we say we have linear polarization E1 only E2 only E1 = E2 • If we let E2 = iE1 we get circular polarization • Most general case is called elliptical polarization Electric field Magnetic Field circular elliptical Polarization and Stokes Parameters E0 E1ε1 E2ε2 • Instead of using real polarization vectors, ε 12 ε1 iε 2 we could use complex ones – These are also called positive and negative helicity polarizations E0 Eε Eε • Then we would write • Any way you look at it, there are four real numbers describing E0 • One of these is the overall phase, corresponding to E ei E 0 0 – These correspond to tiny time shifts 2 2 2 2 s E E E E 0 1 2 • The remaining parameters are sometimes 2 2 described in terms of Stokes Parameters s1 E1 E2 2 Re E* E • Since there are only three independent s2 2 Re E1* E2 2 Im E* E parameters, these must be somehow related s02 s12 s22 s32 s3 2 Im E1* E2 E E 2 2 Measuring Polarization and Stokes Parameters • There are a variety of ways of measuring polarization, but one of the easiest is to put it through a polarizer – Blocks all the light of one polarization, lets much of the other polarization through • Easiest to only allow through one linear polarization, but you can also make them to only allow through one circular polarization Sample Problem 7.1 A pure wave moving in the z-direction is put through a variety of polarizers, and its intensity measured. The types of polarizers and the resulting intensities measured are x-polarization: Ix y-polarization: Iy; plus circular polarization: I+ Predict the intensity if you only allowed minus circular polarization I- 2 2 • Recall the intensity is the I 12 E1 E2 magnitude of the Poynting vector: • For our three 2 2 1 1 I x 2 E1 , I y 2 E2 , I measurements, we have 2 1 I E • We want to know 2 s0 E1 E2 E E 2 • The Stokes parameter s0 is given by • From which we can easily see I x I y I I • Therefore I I x I y I 2 2 1 2 2 E 2 7C. Refraction and Reflection Boundary Conditions and Waves • • • • What happens if our linear medium is not uniform? We will consider only the case of a planar barrier at z = 0 To simplify, we will assume = ' = 0 We therefore have 0n2 n 0 0 • In each region, we will have waves E E0 eik x it , B k E , ck n • We have to match boundary condition at z = 0 E E , D D , B B , H H • These must match at all t, x, and y • Since = ' = 0, last two conditions simplify to B B 0 n 2 0n2 Setting Up the Waves • We will consider a wave coming in from the +z direction in the xz-plane, reflecting in the xz-plane, and refracting in the xz-plane • Call the wave number for the incoming, refracted, and reflected wave k, k', and k", respectively k • Call their constant vector E0, E'0, and E"0 respectively • Then we have 2 ik x x ik z z it ik xx ik zz i t ik x x ik z z i t n 0 E E0 e E0 e , E E0 e • To make them match on the boundary, we need 0n2 k E0 eikx x it E0 eik xx i t E0 eik x x i t , k ik x x it ik xx i t ik x x i t 2 2 n E0 z e E0 z e n E0 z e , k E0 eikx x it k E0 eik xx i t k E0 eik x x i t • These must be valid at all x and all t and k x k x k x • The only way to make this work is to have • Then we have E0 E0 E0 , n2 E0 z E0 z n2E0 z , k E0 k E0 k E0 Snell’s Law and Law of Reflection and k x k x k x ck n , ck n , ck n n k k • Recall we also have • Combining these, k k , we see that c n c n • And therefore k k , nk nk • Define the angles as , ', and " k x k x • Then we have sin sin k k • We also have k x nk x n n sin n sin sin sin k nk n • It is then easy to see that k z k cos k cos k z • We also have 2 n k n kn 2 2 1 sin k z k cos 1 sin 2 n n n k 0 n 2 0n2 k k k z k z k z k n2 n 2 sin 2 Reflection Amplitudes: Perpendicular Case • We still have to find the magnitudes of the reflected and refracted waves • Case I: electric field E0 yˆ E , E0 yˆ E, E0 yˆ E perpendicular to the xz-plane: E0 E0 E0 E E E • One boundary condition: • Another boundary condition: k E0 k E0 k E0 E xˆ kx zˆ kz yˆ E xˆ kx zˆ kz yˆ E xˆ kx zˆ kz yˆ Ekz E E kz Ekz 2Ekz E kz kz • Rewrite using our expressions for k'z E 2n cos n cos n2 n2 sin 2 Ek z Ek z Ek z k z k z 2k z E E E E k z k z k z k z k z k n2 n 2 sin 2 E , E n cos n2 n2 sin 2 n cos n2 n2 sin 2 E Reflection Amplitudes: Parallel Case E0 E xˆ cos zˆ sin , E0 E xˆ cos zˆ sin , • Case II: electric field parallel to the xz-plane: E0 E xˆ cos zˆ sin • One boundary condition: E0 E0 E0 E E cos E cos • Another boundary condition: 2 2 2 2 n E E sin n E sin nE nE nE n E0 z E0 z n E0 z • First equation times n, plus second times cos: 2nE cos E n cos n cos • So we have 2n cos n cos n cos n E E E E E E • Solve for E" n cos n cos n cos n cos n • Rewrite using our expressions for cos' E 2nn cos n cos n n n sin 2 2 2 2 n cos n2 n2 sin 2 E , E n2 cos n n2 n2 sin 2 n cos n n n sin 2 2 2 2 E Brewster’s Angle and Polarization Perpendicular Parallel E 2n cos , 2 2 2 E n cos n n sin E n cos n2 n2 sin 2 E n cos n2 n2 sin 2 E 2nn cos , 2 2 2 2 E n cos n n n sin E n2 cos n n2 n2 sin 2 E n2 cos n n2 n2 sin 2 • Are there any cases where nothing is reflected? • For perpendicular, only if index of refraction matches • For parallel: n2 cos n n2 n2 sin 2 n4 cos 2 n 2 n2 n 4 sin 2 n 2 n2 cos 2 n 2 n2 sin 2 n 4 sin 2 n2 n2 n 2 cos 2 n 2 n2 n 2 sin 2 • Consider light reflected at Brewster’s Angle, defined by • At this angle, the reflected light is completely polarized • Evan at other angles, reflected light is partially polarized n cos n sin n tan P n Total Internal Reflection • • • • • • Suppose we are going from high index to low index Snell’s Law n sin n sin If n sin > n', this would yield sin ' > 1 What do we make of this? k z k n2 n 2 sin 2 We previously found This implies k'z is k z i ik sin 2 n2 n 2 pure imaginary • Substituting this in, we find E E0 eikx x it e z • Wave falls off exponentially in the disallowed region – The evanescent wave • The reflection amplitude in each case is 0 n 2 0n2 k E n cos i n2 sin 2 n2 E n2 cos in n 2 sin 2 n2 or E n cos i n2 sin 2 n2 E n2 cos in n 2 sin 2 n2 • These numbers are both complex numbers of magnitude one k Sample Problem 7.2 (1) Light of frequency is normally incident from a region of index n to a region of index n".. In order to avoid reflection, a coating of index n' of thickness d is placed between them. Show that this works for appropriate choice of n' and d. • Start by writing down electric field in each region – Let’s pick polarization in the x-direction • Fields going both directions in the middle region E Exˆ eikz it , E E1xˆ eik z it E2 xˆ e ik z it , E E xˆ eik z it • We also need magnetic fields from B nkˆ E c zd z 0 0 n2 0 n 2 0n2 B nEyˆ eikz it c , B nE1yˆ eik z it c nE2 yˆ e ik z it c , B nE yˆ eik z it c • Have to match E||, D and B at the boundaries E E1 E2 , nE nE1 nE2 , E1eik d E2e ik d E eik d , nE1eik d nE2e ik d nE eik d • Eliminate E" ik d ik d ik d ik d nE nE n E n E , n E e n E e n E e n E e 1 2 1 2 1 2 1 2 and E Sample Problem 7.2 (2) Light of frequency is normally incident from a region of index n to a region of index n".. In order to avoid reflection, a coating of index n' of thickness d is placed between them. Show that this works for appropriate choice of n' and d. nE1 nE2 nE1 nE2 , nE1eik d nE2e ik d nE1eik d nE2e ik d • Gather E1 and E2 on either side of the equations n n E2 n n E1 , n n E2eikd n n E1eikd • Solve E2 n n n n 2ik d e for E2/E1 E1 n n n n • Cross multiply n2 nn n n n n2 nn n n n e 2ik d • We note that assuming n n", we can conclude e 2ik d 1 • But it must be real, so e2ik d 1 k d 2n 1 • We therefore have n2 nn n n n n2 nn n n n 2n2 2nn n nn 7D. Wave Packets and Group Velocity Wave Packets • No wave is truly monochromatic – If it were, then the plane wave would go for all time and all space • To simplify our understanding, let’s work in one dimension • We’ll combine a number of waves of the form exp ikx i k t – Assume (k) is a known function • We then make a wave 1 function by superposing these: u x, t 2 f k exp ikx i k t dk 1 ikx • If you let t = 0, you see that u x, 0 f k e dk 2 • Or reversing the Fourier transform, we have 1 ikx f k u x , 0 e dx 2 Uncertainty Relation for Arbitrary Waves 1 u x, t 2 1 f k 2 f k exp ikx i k t dk u x, 0 eikx dx • At any given time, we can define the average position or average wave number 2 2 x u x dx k f k dk x , k 2 2 u x dx f k dk • We can similarly define the uncertainty in the position or the wave number x x u x x u x dx 2 2 2 2 k k f k k f k dk dx , 2 2 2 • There is an uncertainty relation between them x k 12 • Same relationship as in quantum mechanics • Any wave that is finite in extent has some spread in wave number 2 dk Dispersion and Group Velocity • • • • • 1 u x, t f k exp ikx i k t dk 2 k Each mode has a phase velocity given by vp k – Speed of the peaks and valleys of the modes If this is bigger than c, can we transmit information faster than light? Assume we have a nearly monochromatic wave, so f is only non-zero for a small region of k near k = k0 Assume (k) is well k 0 k k0 k0 approximated by Taylor series: Then we have 1 u x, t f k exp ikx i0t i k k0 k0 t dk 2 1 ik0 k0 t i0t e f k exp ikx ik k0 t dk 2 Dispersion and Group Velocity (2) 1 ik0 k0 t i0t u x, t e f k exp ikx ik k0 t dk 2 1 ikx f k u x , 0 e dx • Now substitute 2 1 ik0 k0 t i0t ikx u x, t e u x , 0 e dx exp ikx ik k0 t dk 2 • Fundamental theorem of Fourier transforms: • And therefore we have eikwdw 2 w ik k t i t e u x k0 t , 0 x x k t u x ,0 dx 0 • Define the group velocity as v k d g 0 u x, t e ik0 k0 t i0t 0 dk • Then we have u x, t e ik0 vg v p t u x vg t , 0 0 0 0 More About Group Velocity • Recall: c k n • We therefore have • • • • d vg dk 0 1 1 c c dk 1 d vg vg n n n n n d c d Under most circumstances, this is the speed at which signals can travel – Almost always, vg < c In circumstances where n'() is large and negative, this may be violated Under such circumstances, Taylor series approximation may be invalid In situations where n'() is large, usually you get lots of absorption as well – This leads to additional complications