24.5 The Doppler Effect and Electromagnetic Waves Electromagnetic (EM) waves also can exhibit a Doppler effect: 1. Increase in observed frequency for source and observer approaching one another 2. Decrease in observed frequency for source and observer receding from one another But Doppler Shift of EM waves differs from that of sound for two reasons: a) Sound waves travels in a medium, whereas electromagnetic waves can travel in a vacuum (and in some transparent medium) b) For sound, it is the motion relative to the medium that is important. For electromagnetic waves, only the relative motion of the source and observer is important. vo 1± v fo = f s 1 vs v For sound Not for light Electromagnetic waves vrel f o = f s 1 ± c Observed frequency Source frequency if vrel << c Very much less than 1 24.5 The Doppler Effect and Electromagnetic Waves Example Radar Guns and Speed Traps. The radar gun of a police car emits an electromagnetic wave with a frequency of 8.0x109Hz. The approach is essentially head on. The wave from the gun reflects from the speeding car and returns to the police car, where onboard equipment measures its frequency to be greater than the emitted wave by 2100 Hz. Find the speed of the car with respect to the highway. The police car is parked. v 2 24.5 The Doppler Effect and Electromagnetic Waves Example Radar Guns and Speed Traps. The radar gun of a police car emits an electromagnetic wave with a frequency of 8.0x109Hz. The approach is essentially head on. The wave from the gun reflects from the speeding car and returns to the police car, where onboard equipment measures its frequency to be greater than the emitted wave by 2100 Hz. Find the speed of the car with respect to the highway. The police car is parked. v 3 24.5 The Doppler Effect and Electromagnetic Waves Example Radar Guns and Speed Traps The radar gun of a police car emits an electromagnetic wave with a frequency of 8.0x109Hz. The approach is essentially head on. The wave from the gun reflects from the speeding car and returns to the police car, where on-board equipment measures its frequency to be greater than the emitted wave by 2100 Hz. Find the speed of the car with respect to the highway. The police car is parked. v frequency “observed” by speeding car v f o = f s 1 + rel c ∆f = f o′ − f s = f o 1 + v − fs c v v = f s 1 + 1 + − f s c c v v2 = f s 1 + 2 + 2 − 1 c c v≈c v f o′ = f o 1 + rel c v v2 = f s 2 + 2 c c frequency observed by police car v v2 = f s 1 + 2 + 2 − f s c c 2v v << 1 → ∆f ≈ f s c c 2100 Hz ∆f = (3.0 × 108 m s ) = 39 m s 2 fs 2(8.0 × 10 9 Hz) →v≈c ∆f 2 fs 4 19.5 Capacitors and Dielectrics Electrical Energy stored in a capacitor can be thought of in two different ways: (1) Electrical potential energy between the excess +q and –q charges spread evenly separated by distance d, RELATIVE to the situation where the two plates are neutral. (2) Potential energy stored in the electric field (which exists only between the plates, and is zero outside!!! Energy = 12 CV 2 V = Ed Volume = Ad C= κε 0 A d κε o A 2 2 Energy = (Ed ) = (12 κε o E )( Ad ) = u( volume) d 1 2 u = Energy density = Energy Volume = 12 κε o E 2 = 12 ε o E 2 in vacuum Electric field carries energy of “density” Formulation done for a parallel plate capacitor but generally applicable 5 22.8 Self Inductance Magnetic Energy: (1) Inductance Take an IDEAL solenoid of N turns, crosssectional area A, length h and carrying current I. We now want to increase the current by ∆I over time interval ∆t. N turns Crosssectional area A This will cause the magnetic field generated by the solenoid to change, and then induce a backEMF that tends to prevent the increase in current (Lenz’s Law!). h Increasing current E = −N ∆Φ ∆B = − NA ∆t ∆t E = − NA − + E = −N ∆Φ ∆t “−” sign indicates “back”-emf B = µ 0 nI = µ0 NI h 1 µ 0 NI µ 0 N ∆I ∆ = − NA ∆t h h ∆t µ0 N 2 A ∆I E = −L , L= ∆t h SI Unit of L 1V ⋅ s A = 1 H (Henry) Where L is defined to be the (self-) inductance of the solenoid 6 22.8 Self Inductance 2 µ N A ∆ I 0 (2) The energy stored in an inductor E = − L , L= ∆t h The work required to increase the current from I by a small ∆I is given by: ∆W = −E∆q = −E ( I∆t ) ∆I = L ( I∆t ) = (LI )∆I ∆t ∆W = LI ∆I Total magnetic potential energy (MPE) stored is then equal to the total work required to ramp up the current from 0 to I, which is given by the triangular area under the line ∆W ∆I = LI ∆W ∆I ∆W = (LI )∆I ∆I I ∆W = LI ∆I ∆W ∆I 1 2 1 µ0 N 2 A 2 MPE = LI = I 2 2 h 2 1 2 1 µ0 N 2 I 2 = = Ah B ( Volume) 2 2µ0 h 2µ0 MPE = 1 1 ∆2I( LI )( I ) = 2 LI 2 7 I 24.4 The Energy Carried by Electromagnetic Waves From Ch. 20 electric energy density Total EPE 1 = εoE 2 uE = Volume 2 u( x, t ) = The total energy density carried by an electromagnetic wave (which is itself a function of location and time) u ( x, t ) = Averaging over space and time: 1 1 2 2 u = ε o E0 + B0 4 4 µo EPE = MPE From Ch. 22 magnetic energy density Total MPE 1 2 = B Volume 2 µo Total ( EPE + MPE ) 1 1 2 [B( x, t )]2 = ε o [E ( x, t )] + Volume 2 2 µo 1 2πx 1 2πx 2 2 + sin 2 B ft ε o Eo 2 sin 2 2πft π 2 λ 2 µo o λ 2πx 1 sin 2πft = λ 2 2 uB = →u = 1 1 2 1 1 2 ε o E0 + B0 2 2 2 µo 2 E0 2 2 = ε o µo E0 → B0 = ε o µo E0 But B0 = c 1 2 u = ε o E0 2 and u= → B0 2 µo 1 2 µo = ε o E0 B0 2 2 8 24.4 The Energy Carried by Electromagnetic Waves A related quantity: Intensity of EM waves (How bright is the light hitting you?) Analogous to sound intensity (how loud is the sound wave arriving at you)? Intensity: S (unit: W/m2) S= = y x z area A Power Total EM energy = (Area) ∆t Area (EM energy density)(Volume) (Area) ∆t We compute the intensity by finding the energy contained the gray box (of length c∆t, and area A) passing through the yellow frame (area A) in time ∆t. ∆x = c∆t S= u ⋅ (c∆t ⋅ A) = c⋅u A∆t → S = c⋅u Average intensity of an electromagnetic wave: 1 2 S = c ⋅ ε o E0 2 and S = c⋅ 1 2 µo B0 2 9 Example: Sunlight enters the top of the earth's atmosphere with an electric field whose RMS value is Erms = 720 N/C. Find (a) the average intensity of this electromagnetic wave and (b) the rms value of the sunlight's magnetic field At the Earth, orbiting the Sun at 1.00 a.u. (c) Repeat (a) and (b) for Venus, which orbits the Sun at a radius of 0.723 a.u. *** a.u. = astronomical unit. 10 Example: Sunlight enters the top of the earth's atmosphere with an electric field whose RMS value is Erms = 720 N/C. Find (a) the average intensity of this electromagnetic wave and (b) the rms value of the sunlight's magnetic field At the Earth, orbiting the Sun at 1.00 a.u. (c) Repeat (a) and (b) for Venus, which orbits the Sun at a radius of 0.723 a.u. *** a.u. = astronomical unit. C 2 N 1 2 2 8 m −12 3 W 720 1 . 38 10 (a ) S = cε o E0 = cε o E rms = 3.00 × 10 = × 8.85 × 10 s N ⋅ m 2 C m2 2 E E 720 N/C ( b) B0 = 0 → Brms = rms = = 2.40 × 10 −6 T 8 c 3.00 × 10 m/s c 2 −2 PSUN PSUN SV rE2 rV rV 0.723 a.u. = → = = (c) SV = and , = = 0.723 S E 4π rV2 4π rE2 1.00 a.u. S E rV2 rE rE r SV = V rE S = c⋅ −2 SE 1.38 × 108 W/m 8 2 S E = = = 2 . 63 × 10 W/m (0.723) 2 (rV / rE )2 1 2 µo B0 = → Brms = c 2 µo µo S c Brms = 2 ( 4π × 10 −7 T ⋅ m/A)(2.63 × 10 3 W/m 2 ) = 3.32 × 10 -6 T 8 3.00 × 10 m/s 11 24.6 Polarization POLARIZED ELECTROMAGNETIC WAVES In (linearly) polarized light, the electric field oscillates along a single transverse direction. In unpolarized light, the electric field oscillates along random transverse direction at a given moment in time. 12 24.6 Polarization Polarized light may be produced from unpolarized light with the aid of polarizing material. Average Intensity of light: S= 1 cε 0 E02 2 E0 ' = E0 cos θ Absorption and retransmission by antennae in polarizer Primed = after polarizer Unprimed = before polarizer 1 1 2 2 cε 0 (E0 ' ) = cε 0 (E0 cosθ ) 2 2 1 2 S ' = cε 0 E 0 cos 2 θ = S cos 2 θ 2 S'= E0’=E0cosθ E0 θ Malus’ Law For unpolarized incident light Random Input polarization: cos 2θ → cos 2θ = ( ) S ' = S cos 2θ = 1 S 2 1 2 13 24.6 Polarization MALUS’ LAW (general case) E0 θ = angle between polarization before and after analyzer E0cosθ S = S o cos 2 θ intensity after analyzer The textbook’s notational convention intensity before analyzer 14 24.6 Polarization Example Using Polarizers and Analyzers What value of θ should be used so the average intensity of the polarized light reaching the photocell is one-tenth the average intensity of the unpolarized light? 1 10 S o = (12 S o )cos 2 θ 1 5 = cos 2 θ cos θ = 1 5 θ = 63.4 15 24.6 Polarization THE OCCURANCE OF POLARIZED LIGHT IN NATURE 16 Chapter 25 The Reflection of Light: Mirrors We will start to treat light in terms of “rays” -technical for the poetic “beam” of light. This works as long as the “width” of our rays are significantly larger than the wavelength of the light 17 25.1 Wave Fronts and Rays A hemispherical view of a sound wave emitted by a small pulsating sphere (i.e. a point-like source). The rays are perpendicular to the wave fronts (locations where the wave is at the same phase angle, e.g. at the maxima or compressions. At large distances from the source, the wave fronts become less and less curved. They become plane-waves described by: ψ ( x, t ) = ψ 0 sin 2πft − 2πx λ 18 25.2 The Reflection of Light LAW OF REFLECTION 2 types of reflecting surfaces: (a) smooth surface The incident ray, the reflected ray, and the normal to the surface all lie in the same plane, and the angle of incidence equals the angle of reflection. Specular reflection: the reflected rays are parallel to each other. (b) rough surface Diffuse reflection Plane mirror Law of reflection still applies locally, where the normal is the direction perpendicular to the tangent plane 19 25.4 Spherical Mirrors Mirrors cut from segments of a sphere (Spherical mirrors) are used in many optical instruments. If the inside surface of the spherical mirror is silvered or polished, it is a concave mirror. B If the outside surface is silvered or polished, it is a convex mirror. B The principal axis of the mirror is a straight line drawn through the center (C) and the midpoint of the mirror (B). Just as it does for a plane mirror, the Law of reflection still applies locally, where the normal is the direction perpendicular to the tangent plane 20 Applications of spherical mirrors 8.2 m diameter (largest single Large radius-of-curvature (R) piece) reflector (concave concave mirrors tomirror***) enlarge of the SUBARU Telescope nearby object. National Astronomical Observatory of e.g. compact Japan (Mauna mirror Kea Hawaii) Wide-angle rear-view convex mirror found on many vehicles. *** actually the SUBARU main mirror is closer to an hyperboloid 21 25.4 Spherical Mirrors Light rays near and parallel to the principal axis are reflected from the concave mirror and converge at the focal point. In Class Demo The focal length, f , is the distance between the focal point and the middle of the mirror. The focal point of a spherical concave mirror is (approximately) halfway between the center of curvature of the mirror (C) and the middle of the mirror at B. f = 12 R 22 25.4 Spherical Mirrors Rays that lie close to the principal axis are called paraxial rays. Rays that are far from the principal axis do not converge to a single point. The effect is called spherical aberration. When paraxial light rays that are parallel to the principal axis strike a convex mirror, the rays appear to originate from the focal point behind the mirror. Since the light rays do not really converge to this point, it is a virtual focus f = − 12 R In Class Demo The SIGN convention is to assign a negative value to virtual quantities 23