Chapter 18 Waves and Sound

1. Chapter 18 Waves and Sound

2. Objectives • 18.1Sketch a transverse wave and identify its characteristics • 18.1 Discuss the relationship between the frequency and wavelength in a transverse wave • 18.1 Using the relationship among wavelength, frequency, and velocity, find one variable when two are given.

3. Objectives • 18.2Describe the transmission of sound through medium • 18.2 Recognize the relationships between intensity and loudness and frequency and pitch • 18.2 Illustrate the Doppler effect with a practical example

4. Objectives • 18.3Explain how sound waves can be used to create images of organs inside the body • 18.3 Describe some of the uses of ultrasound technology in medicine • 18.4 Distinguish between music and noise • 18.4 Describe why different instruments produce sounds of different quality • 18.4 Explain two types of wave interference

5. What is a Wave? • How would you define what a “wave” is?

6. Waves • Transfer energy without transferring material • Some types of waves transfer energy through material, others transfer energy without needing material • Sound waves  Need a medium • Light waves  Don’t need a medium

7. Types of Waves Transverse waves: the motion of the particles is perpendicular to the wave motion. Longitudinal waves: the motion of the particles is parallel to the wave motion.

8. Transverse • Wave moves to side, matter moves up and down

9. Compression: Matter moves in same direction as wave

10. Terms of Waves • Period: How long it takes to go from crest to crest (back to start) • Crests: The high points of a wave (compression in longitudinal) • Troughs: The low points (rarefaction in longitudinal)

11. Terms of Waves • Midpoint: The “Home position,” the middle of the wave • Amplitude: Distance from midpoint to crest (or trough) • Wavelength: Length of wave, generally measured from one crest to another • Frequency: How many times a second a wave goes through a cycle

12. Random Knowledge • AM radio waves are broadcast in kilohertz (960 AM is 960 kHz or 960,000 Hz) • FM radio waves are broadcast in megahertz (so 100.7 FM is 100.7 MHz or 100,700,000 Hz) • Bumblebees flap at 130 Hz • Honeybees about 225 Hz • Mosquitos about 600 Hz (or 0 Hz after you squash it)

13. Wave Equation • Velocity of the wave is equal to the wavelength times the frequency of the wave • A wave is generated in a wave pool. The wavelength is 3.2 m and the frequency is 0.60 Hz. What is the speed of the wave?

14. Wave Equation • The speed of sound is 340 m/s at room temperature. Calculate the wavelength for the following notes • Middle range pitch: 256 Hz • Low range pitch: 128 Hz • High range pitch: 512 Hz

15. Earthquakes

19. Types of Waves • S- Waves are transverse waves and are not transmitted through fluids. • P- Waves are longitudinal waves and can be transmitted through fluids • S-Waves travel slower than P-Waves. Geologists are able to pinpoint the epicenter by recording when the waves arrive (P waves travel 4-8 km/s and S waves 2-5 km/s)

20. Richter Scale • The Richter Scale is logarithmic. • An earthquake of 3.0 is 10x stronger (more powerful than a 2.0 earthquake and 100x a 1.0 earthquake.

21. Question • How much more energy (by ratio) is released by a 7.2 earthquake on the Richter scale than a 4.2? • How much more energy (by ratio) is released by a 8.0 earthquake compared to 4.0?

22. Intensity of Waves • As you get farther away from the source of the wave, the intensity drops because of energy absorbed by the medium being traveled through and mostly because the wave spreads out. • Air does not absorb much energy from sound waves so they can be heard from great distances.

23. As the distance from the sound increases, the arc length of the angle increases • 1 / d squared • Double distance = ¼ intensity

24. Sound Waves • Sound Waves • Areas of compression and rarefaction. • Audible range for humans is 20 Hz to 20 kHz. • Infrasound refers to waves below 20 Hz and ultrasound refers to waves above 20 kHz.

27. Decibel Scale • The decibel scale is a log rhythmic scale. • The lowest intensity of sound that the human ear can hear is the threshold of hearing. • The value is 1E-12W/m2. • 0 dBels is 1E-12W/m2. • The equation to figure out how many decibels loud something is

29. The Human Ear

30. The Human Ear • Pinna = Funnel, collecting waves at opening of Auditory canal (ear canal) • Resonance occurs in the ear canal to boost the ear’s sensitivity to sound frequencies between 2 and 5 kHz (this helps us understand speech)

31. The Human Ear • Tympanic membrane = Vibrates in response to the sound waves reaching it. • This vibration is transmitted through tiny bones (three of them, called the Auditory ossicles) to the Cochlea The ossicles act as levers, and have a mechanical advantage to amplify the sound waves for the cochlea. (The hammer)

32. The Human Ear • Cochlea = Spiral shaped organ filled with fluid. The pounding of the ossicles on the cochlea produce a compressional wave (longitudinal) which goes through the cochlea. This wave collides with the basilar membrane (not shown on diagram), which functions much like the eyes do in focusing. Based off of the frequency of the waves, it tightens or relaxes to vibrate at its maximum resonance.

33. The Human Ear • On this membrane are the organs of corti. There are a whole bunch of tiny hair cells which bend in response to waves. The bending of the hair cells causes neurons to send electrical signals to the brain.

34. The Human Ear • Other Interesting information: When exposed to loud noises, the muscles which hold the hammer will tighten and pull the hammer away from the drum and make our ears less sensitive to noise. • The sound waves which reach the ears are often complex, composed of many frequencies. Our brain does some quick mental math to break the frequency down to its individual frequencies (your brain is smarter than a calculator)

35. Timbre • Timbre • A tuning fork produces one single frequency. However, most instruments and our voices produce a complex sound, with many frequencies overlapping on one another. • Why does a middle C on an Oboe sound different than middle C on a Trumpet? Timbre.

36. Timbre • The lowest frequency of a sound wave is called the fundamental. • The rest of the frequencies are overtones • All overtones are integral multiples of the fundamental: ie If the fundamental is 30 Hz, the overtones could be 60, 90, and 120 Hz but could not be 40, 50, or 70 • Even if the fundamental is not being produced, our ear “hears” the fundamental and makes the fundamental itself.

38. Loudness • While related to intensity, it also depends on frequency, as our ears hear different frequencies better than others. Our ears hear best between 3-4 kHz. Take note, a person with no hearing loss and excellent hearing cannot hear below the bottom line.

39. 120 • 0 dB • 0 Hz 2-4000 Hz 20k Hz

40. Pitch • Our perception of frequency. Our sense of pitch and frequency is logarithmic, just as loudness is logarithmic with intensity. • If you were to play a piano from the lowest note (27.5 Hz) to the highest note (4,190 Hz) you hear equal steps of pitch, but the steps are not equal. The frequency of each note is 5.95% higher than the previous note.

41. Localization • How the ear localizes sound: •  Head shadow: Noise is more intense on side of noise as our head is a shadow •  Shape of pinna: Faces front, helps with back-front localization •  For low frequency sounds, phase difference between the waves helps in localization

42. Beats • When two frequencies are close to one another (< 15 Hz), the waves produce a pulsation called beats. The frequencies are so close that the superposition seems to produce many amplitudes • Like turn signal blinkers

44. Beats • The waves do not stay in phase forever, and the wave with a higher frequency gets ahead of the lower frequency one. When they are 180 degrees out of phase, destructive interference occurs, and in phase, constructive. • At frequency differences greater than 15 Hz, we hear separate tones.

45. Standing Waves, Nodes, Antinodes and Interference • While matter can not exist in the same space and time as other matter (Two rocks can not exist in the same place), waves can and do (right now our bodies have bazillions of waves passing through them). If you drop two rocks in a pond, the waves can overlap and form an interference pattern. The wave effects are increased, decreased, or even neutralized.

46. Types of Interference • When a crest hits another crest, they add together and increase amplitude. This is calledconstructive interference. When a crest hits a trough, the waves are cancelled out, the crest “fills in” the trough. This is called Destructive interference.

47. Constructive Interference Destructive Interference Phase Shift High Pressure Waves can be out of phase. This essentially means that one lags slightly behind another. This can cause varying amounts of interference. High and low pressure areas from both waves match up causing a maximum amount of constructive interference Sound wave with high and low pressures. High pressures line up with the low pressures of a second wave, causing destructive interference. Low Pressure

50. Out of Phase (180 degrees)