Wavepackets Outline - Review: Reflection & Refraction - Superposition of Plane Waves - Wavepackets - Δ Δkk −– Δxx Relations 1 Sample Midterm 2 (one of these would be Student X’s Problem) Q1: Midterm 1 re-mix (Ex: actuators with dielectrics) Q2: Lorentz oscillator (absorption / reflection / dielectric constant / index of refraction / phase velocity) Q3: EM Waves (Wavevectors / Poynting / Polarization / Malus' Law / Birefringence /LCDs) Q4: Reflection & Refraction (Snell's Law, Brewster angle, Fresnel Equations) Q5: Interference / Diffraction 2 Electromagnetic Plane Waves The Wave Equation ω k= c ∂ 2 Ey ∂ 2 Ey = μ 2 2 ∂t ∂z Ey = A1 cos (ωt − kz) + A2 cos (ωt + kz) A1 A2 cos (ωt − kz) + cos (ωt + kz) Hx = − η η E H t 3 E H Reflection of EM Waves at Boundaries E1 (z = 0) = E2 (z = 0) incident wave • Write traveling wave terms in each region • Determine boundary condition transmitted wave • Infer relationship of ω1,2 & k1,2 reflected wave Medium 1 • Solve for Ero (r) and Eto (t) Medium 2 i + Er E1 = E −jk1 z +jk1 z =a ˆx Ei0 e + Er0 e −jk1 z +jk1 z =a ˆx Ei0 e + rEi0 e 4 2 = E t E =a ˆx Et0 e−jk2 z =a ˆx tEi0 e−jk2 z E H Reflection of EM Waves at Boundaries 1 (z = 0) = E 2 (z = 0) E incident 1 (z = 0) = H 2 (z = 0) wave H transmitted wave reflected wave • Write traveling wave terms in each region • Determine boundary condition • Infer relationship of ω1,2 & k1,2 • Solve for Ero (r) and Eto (t) Medium 1 Medium 2 −jk1 z +jk1 z ˆx Ei0 e + Er0 e E1 = a Ei0 −jk1 z Er0 +jk1 z H1 = a ˆy e − e η1 η1 At normal incidence.. 5 2 = a ˆx Et0 e−jk2 z E Et0 −jk2 z H2 = a ˆy e η2 η2 − η1 E0r r= i = η2 + η1 E0 Oblique Incidence at Dielectric Interface E-field polarization perpendicular to the plane of incidence (TE) • Write traveling wave terms in each region • Determine boundary condition • Infer relationship of ω1,2 & k1,2 • Solve for Ero (r) and Eto (t) i = ây E i0 e−jkix x−jkiz z E E-field polarization parallel to the plane of incidence (TM) x z y• i = a ˆy Hi0 e−jkix x−jkiz z H 6 Oblique Incidence at Dielectric Interface • Write traveling wave terms in each region • Determine boundary condition • Infer relationship of ω1,2 & k1,2 r = ây Er0 e−jkrx x+jkrz z E • Solve for Ero (r) and Eto (t) t = ây Et0 e−jktx x−jktz z E x z y• i = ây Ei0 e−jkix x−jkiz z E 7 Oblique Incidence at Dielectric Interface • Write traveling wave terms in each region • Determine boundary condition • Infer relationship of ω1,2 & k1,2 r = ây Er0 e−jkrx x+jkrz z E • Solve for Ero (r) and Eto (t) t = ây Et0 e−jktx x−jktz z E x z y• i = ây Ei0 e−jkix x−jkiz z E Tangential field is continuous (z=0).. Ei0 e−jkix x + Er0 e−jkrx x = Et0 e−jktx x 8 Snell’s Law Tangential E-field is continuous … Ei0 e−jkix x + Er0 e−jkrx x = Et0 e−jktx x n1 n2 REMINDER: ω ωn k= = vp c x z y• kix = krx n1 sin θi = n1 sin θr θ i = θr kix = ktx n1 sin θi = n2 sin θt 9 Reflection of Light (Optics Viewpoint … μ1 = μ2) TE i E E-field perpendicular to the plane of Ht incidence t E r E t H TM x i E i H TM: n2 cos θi − n1 cos θt r = n2 cos θi + n1 cos θt t E i H r H n1 cos θi − n2 cos θt r⊥ = n1 cos θi + n2 cos θt y• E-field parallel to the plane of incidence θc Reflection Coefficients r E r H TE: n1 = 1.44 n2 = 1.00 |r⊥ | θB |r | Incidence Angle z 10 θi Electromagnetic Plane Waves The Wave Equation ω k= c ∂ 2 Ey ∂ 2 Ey = μ 2 2 ∂t ∂z Ey = A1 cos (ωt − kz) + A2 cos (ωt + kz) A1 A2 cos (ωt − kz) + cos (ωt + kz) Hx = − η η E H • When did this plane wave turn on? t • Where is there no plane wave? 11 Superposition Example: Reflection E H incident wave transmitted wave reflected wave Medium 1 Medium 2 How do we get a wavepacket (localized EM waves) ? 12 Superposition Example: Interference Reflected Light Pathways Through Soap Bubbles Constructive Interference (Wavefronts in Step) Incident Reflected Light Light Path Paths Destructive Interference (Wavefronts out of Step) Incident Light Path Reflected Light Paths Outer Surface of Bubble Image by Ali T http://www.flickr .com/photos/77682540@N00/27 89338547/ on Flickr. Thin Part of Bubble Inner Surface of Bubble Thick Part of Bubble What if the interfering waves do not have the same frequency (ω, k) ? 13 Two waves at different frequencies … will constructively interfere and destructively interfere at different times time In Figure above the waves are chosen to have a 10% frequency difference. So when the slower wave goes through 5 full cycles (and is positive again), the faster wave goes through 5.5 cycles (and is negative). 14 Wavepackets: Superpositions Along Travel Direction 4π =E o ej(ω1 t−k1 z) + ej(ω2 t−k2 z) ŷ E | k2 + k 1 | 4π |k2 − k1 | REMINDER: n k= ω c SUPERPOSITION OF TWO WAVES OF DIFFERENT FREQUENCIES (hence different k’s) 15 Wavepackets: Superpositions Along Travel Direction WHAT WOULD WE GET IF WE SUPERIMPOSED WAVES OF MANY DIFFERENT FREQUENCIES ? =E o E +∞ −∞ f (k) e+j(ωt−kz) dk LET’S SET THE FREQUENCY DISTRIBUTION as GAUSSIAN f (k) 1 (k − ko ) f (k ) = √ exp − 2σk2 2πσk 2 REMINDER: σk ko k 16 n k= ω c Reminder: Gaussian Distribution σ √ 50% of data within ± 2 0.4 0.3 0.2 0.1 34.1% 34.1% 2.1% 0.1% 13.6% 13.6% μ (x−μ)2 1 f (x) = √ e− 2σ2 2πσ 2.1% μ specifies the position of the bell curve’s central peak σ specifies the half-distance between inflection points FOURIER TRANSFORM OF A GAUSSIAN IS A GAUSSIAN Fx e −ax 2 0.1% (k) = 17 π − π 2 k2 e a a Gaussian Wavepacket in Space t = to Re{En (z, to )} f (k) Re{En (z, to )} n SUM OF SINUSOIDS = WAVEPACKET 1 (k − ko ) f (k) = √ exp − 2σk2 2πσk σk ko k 2 WE SET THE FREQUENCY DISTRIBUTION as GAUSSIAN 18 Gaussian Wavepacket in Time 2 σk 2 E(z, t) = Eo exp − (ct − z) cos (ωo t − ko z) 2 GAUSSIAN ENVELOPE Re{En (z, to )} Re{En (z, t1 )} t = to z z kn t = t1 k n Re{En (z, t1 )} Re{En (z, to )} n n 19 Gaussian Wavepacket in Space σk2 2 E(z, t) = Eo exp − (ct − z) cos (ωo t − ko z) 2 WAVE PACKET λo λo = 2π ko GAUSSIAN ENVELOPE In free space … ω k= c … this plot then shows the PROBABILITY OF WHICH k (or frequency) EM WAVES are MOST LIKELY TO BE IN THE WAVEPACKET f (k) Δz = √ σk ko ΔkΔz = 1/2 k 20 1 2σk Gaussian Wavepacket in Time E(z, t) = Eo exp − σk2 2 (ct − z) 2 WAVE PACKET cos (ωo t − ko z) λo λo = 2π ko Δk Δz UNCERTAINTY RELATIONS c Δz = Δt n c Δk = Δω n ΔkΔz = 1/2 ΔωΔt = 1/2 If you want to LOCATE THE WAVEPACKET WITHIN THE SPACE Δz you need to use a set of EM-WAVES THAT SPAN THE WAVENUMBER SPACE OF Δk = 1/(2Δz) 21 Wavepacket Reflection E(z, t) Ec Ec∗ 22 Wavepackets in 2-D and 3-D E(x, z)E ∗ (x, z) Contours of constant amplitude E(x, z)E ∗ (x, z) t = to 2-D 3-D Spherical probability distribution for the magnitude of the amplitudes of the waves in the wave packet. 23 In the next few lectures we will start considering the limits of Light Microscopes incident photon and how these might affect our understanding of the world we live in electron Suppose the positions and speeds of all particles in the universe are measured to sufficient accuracy at a particular instant in time It is possible to predict the motions of every particle at any time in the future (or in the past for that matter) 24 WAVE PACKET Key Takeaways λo λo = GAUSSIAN WAVEPACKET IN SPACE 2 σ 2 E(z, t) = Eo exp − k (ct − z) cos (ωo t − ko z) 2 GAUSSIAN ENVELOPE UNCERTAINTY RELATIONS ΔkΔz = 1/2 ΔωΔt = 1/2 25 2π ko MIT OpenCourseWare http://ocw.mit.edu 6.007 Electromagnetic Energy: From Motors to Lasers Spring 2011 For information about citing these materials or our Terms of Use, visit: http://ocw.mit.edu/terms.