From Last Time Wave Properties. Description of a Wave. Water waves? Water waves occur on the surface. They are a kind of transverse wave.

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From Last Time Wave Properties Amplitude is the maximum displacement from the equilibrium position Wavelength,, is the distance between two successive points that behave identically Period: time required to complete one cycle Frequency = 1/Period = rate at which cycles are completed Velocity = Wavelength/Period, v = / T, or v = f Description of a Wave Amplitude is the maximum displacement of string above the equilibrium position Wavelength,, is the distance between two successive points that behave identically Amplitude For instance, the distance between two crests Phy107 Fall 06 1 Phy107 Fall 06 2 More types of waves Transverse Waves on a rope Longitudinal (compressional) Sound waves Other examples of waves Water waves Seismic waves Water waves? Water waves occur on the surface. They are a kind of transverse wave. Phy107 Fall 06 3 On Earth On the sun Phy107 Fall 06 4 Water s Motion I The wave travels while the water circles! Water s Motion Circling strongest at surface Weak ~ 1/2 wavelength deep Depth and wavelength connected Phy107 Fall 06 5 Phy107 Fall 06 6 1

Wavelength of water wave The longer the wavelength of the wave the deeper it goes the more energy it contains for a given amplitude Tsunamis are very long wavelength, very deep, very high energy waves Generate by some disturbance Landslide Undersea earthquake Generates long-wavelength propagating water wave Tsunamis Phy107 Fall 06 7 Phy107 Fall 06 8 Tsunami is a wave As the wave approaches shallower water, the surface component becomes higher and steeper. December 26, 2004 tsunami was generated from the 9.0 Richter scale Sumatra earthquake Like all waves, tsunami transported energy but not mass. The water that impacted the beaches in Sri Lanka, for example, did not "come from" Sumatra; Just the energy "came from" Sumatra. Wavelength, period, and velocity: velocity = wavelength frequency Frequency = 1 / period: period of 40 minutes gives frequency of about 0.0004Hz (cycles per second). The wavelength of this tsunami in deep water is about 500km From this we can compute the tsunami velocity to be about 200m/s or 450 miles an hour - about as fast as a jet airplane! Phy107 Fall 06 9 Phy107 Fall 06 10 Seismic waves Waves in the earth generated by earthquake P (primary) wave: compressional v P ~ 6 km/s Detecting with seismometer P (transverse) wave travels faster than S (compressional) wave, so it registers first on seismometer. S (secondary) waves: transverse v S ~3.5 km/s Phy107 Fall 06 11 Phy107 Fall 06 12 2

Locating an earthquake Time difference between P arrival time and S arrival time due to difference in velocities. P travel time = distance / P-velocity S travel time = distance / S-velocity Arrival time difference = ( P travel time) ( S travel time) = distance distance P velocity S velocity t = d d = d 1 1 = d( 0.119 s/km) v S v P v S v P d = ( 8.4 km /s) t Phy107 Fall 06 13 Seismic Rayleigh wave (R-wave) Rayleigh wave: another wave from earthquakes Particle motion roughly circular. Amplitude decreases with depth. A surface wave. This is same as a water wave! But counterclockwise Phy107 Fall 06 14 Combining waves Two traveling waves can meet and pass through each other without being destroyed or even altered Waves obey the Superposition Principle If two or more traveling waves are moving through a medium, the resulting wave is found by adding together the displacements of the individual waves point by point Constructive interference: waves reinforce Destructive interference: waves tend to cancel Constructive Interference in a String Two pulses are traveling in opposite directions The net displacement when they overlap is the sum of the displacements of the pulses Note that the pulses are unchanged after the interference Phy107 Fall 06 15 Phy107 Fall 06 16 Constructive Interference Destructive Interference in a String Two waves, a and b, have the same frequency, amplitude, and start point Are in phase The combined wave, c, has the same frequency and a greater amplitude Combined wave + = Two pulses are traveling in opposite directions The net displacement when they overlap the displacements of the pulses subtract Note that the pulses are unchanged after the interference Phy107 Fall 06 17 Phy107 Fall 06 18 3

Destructive interference in a continuous wave Two waves, a and b, have the same amplitude and frequency They are 1/2 wavelength out of phase When they combine, the waveforms cancel + = Interference of sound waves Interference arises when waves change their phase relationship. Can vary phase relationship of two waves by changing physical location of speaker. in-phase 1/2 phase diff Phy107 Fall 06 19 Constructive Destructive Phy107 Fall 06 20 Example Interference Speed of sound ~ 340 m/s So f=340 Hz gives =v/f = 1 meter Change of 1/2 wavelength is 1/2 meter. Or can change phase relationship by changing relative distance from source. Water drop is a source of circular waves (twodimensions here) When the waves overlap, they superimpose. In some areas they cancel, in others they reinforce. This is called interference Phy107 Fall 06 21 Phy107 Fall 06 22 Sound waves again Sensing sound Sound is a compressional wave The crest is a local compression of the air, the trough a local rarefraction. Can be produced by objects transferring their vibratory motion to the air Tuning fork Speaker Musical instrument Phy107 Fall 06 23 Middle ear transmits sound to cochlea, which discriminates loudness and pitch Phy107 Fall 06 24 4

Discriminating pitch Your ear detects sound A mechanosensitive hair bundle in the cochlea of the ear. Each hair bundle is made up of 30-300 stereocilia (tiny hairs). Different locations host bundles that send different pitch signals. Vibrations of the basilar membrane Phy107 Fall 06 25 Phy107 Fall 06 26 Pitch Frequency Response Curves Pitch is related mainly, although not completely, to the frequency of the sound Pitch is not a physical property of the sound Frequency is the stimulus and pitch is the response It is a psychological reaction that allows humans to place the sound on a scale Bottom curve is the threshold of hearing Threshold of hearing is strongly dependent on frequency Easiest frequency to hear is about 3000 Hz When the sound is loud (top curve, threshold of pain) all frequencies can be heard equally well Phy107 Fall 06 27 Phy107 Fall 06 28 Timbre In music, the characteristic sound of any instrument is referred to as the quality of sound, or the timbre of the sound Not all sound is a pure tone. The quality depends on the mixture of harmonics in the sound. This is a mixture of other frequencies with the original. Can completely describe the sound by only including overtones Quality of Sound Tuning Fork Tuning fork produces only the fundamental frequency Phy107 Fall 06 29 Phy107 Fall 06 30 5

Quality of Sound Flute The same note played on a flute sounds differently Not a pure tone = Quality of Sound Clarinet The fifth harmonic is very strong The first and fourth harmonics are very similar, with the third being close to them + + Fundamental, Freq. f 1st harmonic, Freq. 2f 2nd harmonic Freq. 3f Phy107 Fall 06 31 Phy107 Fall 06 32 6