Chapter 14 Lecture Essential University Physics Richard Wolfson 2nd Edition Wave Motion © 2012 Pearson Education, Inc. Slide 14-1 In this lecture you’ll learn • To explain waves as traveling disturbances that transport energy but not matter • To describe waves quantitatively in terms of frequency, period, wavelength, and amplitude • To describe specific types of waves – Waves on strings – Sound waves • To describe interference, reflection, and standing waves • To describe the Doppler effect and shock waves © 2012 Pearson Education, Inc. Slide 14-2 What’s a Wave? • A wave is a traveling disturbance that transports energy but not matter. – Mechanical waves are disturbances of a material medium. • The medium moves briefly as the wave goes by, but the medium itself isn’t transported any distance. • The wave propagates as the disturbance of the medium is communicated to adjacent parts of the medium. – Electromagnetic waves, including light, do not require a medium. • Nevertheless, they share many of the properties of mechanical waves. © 2012 Pearson Education, Inc. Slide 14-3 Longitudinal and Transverse Waves • In a longitudinal wave, the disturbance is parallel to the wave motion. Longitudinal wave on a mass-spring system: • In a transverse wave, the disturbance is perpendicular to the wave motion. Transverse wave on a mass-spring system: • Some waves, like surface waves on water, involve both longitudinal and transverse motions. © 2012 Pearson Education, Inc. Slide 14-4 Properties of Waves • Wavelength is the distance over which a wave repeats in space. • Period T is the time for a complete cycle of the wave at a fixed position: – Frequency f = 1/T • Amplitude A is the peak value of the wave disturbance. • Wave speed is the rate at which the wave propagates: v = /T = f • Wave equation: 2 y 1 2 y 2 2 2 x v t © 2012 Pearson Education, Inc. Slide 14-5 Simple Harmonic Waves • A simple harmonic wave has a sinusoidal shape. – A simple harmonic wave is described by a sinusoidal function of space and time: y x t A kx t • y measures the wave disturbance at position x and time t. • k = 2p / is the wave number, a measure of the rate at which the wave varies in space. • = 2pf = 2p /T is the angular frequency, a measure of the rate at which the wave varies in time. • The wave speed is v = f = /k. These two waves have the same speed. How do their wavenumbers, angular frequencies, and periods compare? © 2012 Pearson Education, Inc. Slide 14-6 Waves on Strings • On strings, fibers, long springs, cables, wires, etc., tension provides the restoring force that helps transverse waves propagate. – Newton’s second law gives mv 2 2 R v 2 2 F 2 v 2 R R where F is the tension and is the mass per unit length. – The speed of such waves is v= © 2012 Pearson Education, Inc. F m Slide 14-7 Wave Power and Intensity • The power carried by a wave is proportional to the wave speed and to the square of the wave amplitude. – Details depend on the type of wave; for waves on a string, the average power is P = 1 mw 2 A2 v. 2 • Wave intensity is the power per unit area. – In a plane wave, the intensity remains constant. • The plane wave is a good approximation to real waves far from their source. – A spherical wave spreads in three dimensions, so its intensity drops as the inverse square of the distance P P from its source: I= © 2012 Pearson Education, Inc. A = 4p r 2 Slide 14-8 Sound • Sound waves are longitudinal mechanical waves that propagate through gases, liquids, and solids. – Sound waves in air involve small changes in air pressure and density, associated with back-and-forth motion of the air as the wave passes. – Sound intensity levels are measured in decibels, a logarithmic unit based on comparison with a reference intensity I0= 10–12 W/m2: b = 10 log I I 0 . ( ) – The human ear responds to a broad range of sound intensities and frequencies. © 2012 Pearson Education, Inc. Slide 14-9 Wave Interference • Unlike particles, two waves can be in the same place at the same time. • When they are, they interfere. – In most cases, the waves superpose, or simply add. • When wave crests coincide, the interference is constructive. • When crests coincide with troughs, the interference is destructive. © 2012 Pearson Education, Inc. Slide 14-10 Interference Phenomena • When waves of slightly different frequencies interfere, they alternate between constructive and destructive interference. – This results in beats at the difference of their frequencies. • Interference from two closely spaced sources results in patterns of high- and low-amplitude waves. – The photo shows such an interference pattern with water waves. © 2012 Pearson Education, Inc. Slide 14-11 Wave Reflection • Waves reflect at an interface with a different medium. – The outgoing wave interferes with the incoming wave. – The reflected wave is inverted, depending on properties of the second medium. – The diagram shows waves on a string reflecting at clamped and free ends. – More generally, a wave is partially reflected and partially transmitted at an interface between different media. © 2012 Pearson Education, Inc. Slide 14-12 Partial Reflection and Refraction • Partial reflection of light occurs at an interface between air and glass. © 2012 Pearson Education, Inc. • Waves striking an interface at an oblique angle undergo refraction, a change in the direction of propagation. Slide 14-13 Standing Waves • Waves on a confined medium reflect at both ends. – The result is standing waves that oscillate but don’t propagate. – The length of the medium restricts the allowed wavelengths and frequencies to discrete values. On a string clamped at both ends, the string length must be an integer multiple of a half-wavelength: L = m/2, with m an integer. © 2012 Pearson Education, Inc. On a string clamped at one end, the string length must be an odd integer multiple of a halfwavelength: L = m/4, with m odd. Slide 14-14 Standing Waves in Musical Instruments • Stringed instruments are analogous to the strings of the previous slide: The string length determines the allowed wavelengths and, together with the wave speed, the allowed frequencies. • Wind instruments are analogous, with sound waves in their air columns. – Wind instruments are typically open at one end or both. © 2012 Pearson Education, Inc. Slide 14-15 The Doppler effect • When a wave source moves through the wave medium, a stationary observer experiences a shift in wavelength and frequency. – The frequency increases for an approaching source. – The frequency decreases for a receding source. – The shifted frequencies are given by f f 1 u v . • Here u is the source speed and v is the wave speed. • A similar effect occurs for a moving observer, but there’s no wavelength shift. • The Doppler effect for light is similar but slightly different because light has no medium. The formula above applies only for speeds much less than light. © 2012 Pearson Education, Inc. Slide 14-16 Shock Waves • Shock waves occur when a wave source moves through the medium at a speed u greater than the wave speed v. – The ratio u/v is called the Mach number. – Mach angle is defined by sin = u/v. – Examples include sonic booms from aircraft, wakes of boats, and astrophysical bodies moving through interplanetary and interstellar gas. © 2012 Pearson Education, Inc. Slide 14-17 Summary • A wave is a traveling disturbance that carries energy but not matter. – Mechanical waves involve the disturbance of a material medium. • These include sound waves. – Electromagnetic waves, including light, have no medium. – Simple harmonic waves are sinusoidal in shape. y xt A kx t – The speed of a wave follows from its frequency and wavelength or from its angular frequency and wavenumber: v = f = /k. – Important wave phenomena include • • • • • Reflection and refraction Interference Standing waves The Doppler effect Shock waves © 2012 Pearson Education, Inc. Slide 14-18
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