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Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11.

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1 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11

2 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Periodic (vibrating) motion is repeated motion. –swing –pendulum –mass on a spring –metronome –pendulum clocks –oscillations –waves Chapter 11 Section 1 Simple Harmonic Motion

3 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu VIBRATIONS and WAVES Chapter 11

4 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Vibrations and Waves Chapter 11 Table of Contents Section 1 Simple Harmonic Motion Section 2 Measuring Simple Harmonic Motion Section 3 Properties of Waves Section 4 Wave Interactions

5 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 The Vibrating Spring One type of periodic motion is the motion of a mass attached to a spring. The direction of the force acting on the mass (F elastic ) is always opposite the direction of the mass’s displacement from equilibrium (x = 0). F el is a restoring force, because it acts to restore the system to equilibrium Section 1 Simple Harmonic Motion

6 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Hooke’s Law Measurements show that the spring force, or restoring force, is directly proportional to the displacement of the mass. This relationship is known as Hooke’s Law: F elastic = –kx spring force = –(spring constant  displacement) The quantity k is a positive constant called the spring constant with SI unit N/m. PE elastic = 1/2kx 2 PE max = 1/2kx 2 max Section 1 Simple Harmonic Motion

7 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Sample Problem Hooke’s Law If a mass of 0.55 kg attached to a vertical spring stretches the spring 2.0 cm from its original equilibrium position, what is the spring constant? Section 1 Simple Harmonic Motion

8 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Section 1 Simple Harmonic Motion Unknown: k = ? Determine the spring constant. Diagram: Given: m = 0.55 kg x = – 2.0 cm = – 0.02 m g = 9.81 m/s 2 F g = mg = 0.55 kg x 9.81 m/s 2 = 5.4 N F = -kx

9 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Section 1 Simple Harmonic Motion When the mass is attached to the spring, the equilibrium position changes. At the new equilibrium position, the net force acting on the mass is zero. So the spring force (given by Hooke’s law) must be equal and opposite to the weight of the mass. F net = 0 = F elastic + F g F elastic = –kx F g = – 5.4 N F elastic – 5.4 N = 0 F elastic = 5.4 N F elastic = –kx k = F elastic /–x k = 5.4 N /–(-.02 m) k = 270 N/m

10 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Section 1 Simple Harmonic Motion Evaluate your answer. The value of k implies that 270 N of force is required to displace the spring 1 m. A 270 N force is the weight of a 27.5 kg mass.

11 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Practice A p. 371 1.a. 15 N/mb. less stiff 2.3.2 x 10 2 N/m 3.2.7 x 10 3 N/m 4.81 N

12 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Simple Harmonic Motion All vibrating systems that obey Hooke’s law demonstrate simple harmonic motion. Simple harmonic motion describes any periodic motion that is the result of a restoring force that is proportional to displacement. (Hooke’s Law) Because simple harmonic motion involves a restoring force, every simple harmonic motion is a back-and-forth motion over the same path.

13 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Harmonic Oscillators A harmonic oscillator is an oscillator with a restoring force proportional to its displacement from equilibrium. Its period of oscillation depends only on the stiffness of that restoring force and on its mass, not on its amplitude of oscillation. Period (T) is the time for 1 complete oscillation and in measured in seconds. Any harmonic oscillator can be thought of as having a restoring force component that drives the motion and an inertial component that resists the motion. http://upload.wikimedia.org/wikipedia/commons/e/ea/Simple_Harmonic_Motion_Orbit.gif http://upload.wikimedia.org/wikipedia/commons/2/21/Pendulum_animation.gif

14 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Clocks are based on Simple Harmonic Oscillators Pendulum and Balance Clocks –The accuracy of pendulum and balance clocks is limited by friction, air resistance, and thermal expansion to about 10 s/year. Electronic Clocks –Quartz crystals are piezoelectric materials and respond mechanically to electrical stress and electrically to mechanical stress. –Loses or gains less than a 0.1 s/year Atomic Clocks ( Gain / lose 1 s/ 10 million years) –The second is the duration of 9 192 631 770 periods of the radiation corresponding to the transition between the two hyperfine levels of the ground state of the cesium 133 atom. –The meter is the length of the path travelled by light emitted by krypton-86 in vacuum during a time interval of 1/299 792 458 of a second.

15 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Simple Harmonic Motion y = A sin  t y = A sin 2  f http://webphysics.davidson.edu/physlet_resources/bu_semester1/c18_SHM_graphs.html

16 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 WAVES Section 3 Properties of Waves

17 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Objectives Distinguish local particle vibrations from overall wave motion. Differentiate between pulse waves and periodic waves. Interpret waveforms of transverse and longitudinal waves. Apply the relationship among wave speed, frequency, and wavelength to solve problems. Relate energy and amplitude. Section 3 Properties of Waves

18 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Wave Motion A wave is the motion of a disturbance. A medium is a physical environment through which a disturbance can travel. For example, water is the medium for ripple waves in a pond. Waves that require a medium through which to travel are called mechanical waves. Water waves and sound waves are mechanical waves. Electromagnetic waves such as visible light do not require a medium. Section 3 Properties of Waves

19 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Wave Types A wave that consists of a single traveling pulse is called a pulse wave. Whenever the source of a wave’s motion is a periodic motion, such as the motion of your hand moving up and down repeatedly, a periodic wave is produced. A wave whose source vibrates with simple harmonic motion is called a sine wave. Thus, a sine wave is a special case of a periodic wave in which the periodic motion is simple harmonic. Section 3 Properties of Waves

20 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Relationship Between SHM and Wave Motion Section 3 Properties of Waves As the sine wave created by this vibrating blade travels to the right, a single point on the string vibrates up and down with simple harmonic motion.

21 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Wave Types, continued A transverse wave is a wave whose particles vibrate perpendicularly to the direction of the wave motion. The crest is the highest point above the equilibrium position, and the trough is the lowest point below the equilibrium position. The wavelength ( ) is the distance between two adjacent similar points of a wave. Section 3 Properties of Waves

22 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Transverse Waves Section 3 Properties of Waves

23 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Wave Types, continued A longitudinal wave is a wave whose particles vibrate parallel to the direction the wave is traveling. A longitudinal wave on a spring at some instant t can be represented by a graph. The crests correspond to compressed regions, and the troughs correspond to stretched regions. The crests are regions of high density and pressure (relative to the equilibrium density or pressure of the medium), and the troughs are regions of low density and pressure. Section 3 Properties of Waves

24 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Longitudinal Waves Section 3 Properties of Waves

25 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Period, Frequency, and Wave Speed The frequency of a wave describes the number of waves that pass a given point in a unit of time. The period of a wave describes the time it takes for a complete wavelength to pass a given point. The relationship between period and frequency in SHM holds true for waves as well; the period of a wave is inversely related to its frequency. Section 3 Properties of Waves

26 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Characteristics of a Wave Section 3 Properties of Waves

27 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Period, Frequency, and Wave Speed, continued The speed of a mechanical wave is constant for any given medium. The speed of a wave is given by the following equation: v = f wave speed = frequency  wavelength This equation applies to both mechanical and electromagnetic waves. Section 3 Properties of Waves

28 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Practice D p. 387 1.0.081 m < < 12 m 2.a. 3.41 m b. 5.0 x 10 -7 m c. 1.0 x 10 -10 m 3.4.74 x 10 14 Hz 4.a. 346 m/sb. 5.86 m

29 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Waves and Energy Transfer Waves transfer energy by the vibration of matter. Waves are often able to transport energy efficiently. The rate at which a wave transfers energy depends on the amplitude. –The greater the amplitude, the more energy a wave carries in a given time interval. –For a mechanical wave, the energy transferred is proportional to the square of the wave’s amplitude. The amplitude of a wave gradually diminishes over time as its energy is dissipated. Section 3 Properties of Waves

30 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Objectives Apply the superposition principle. Differentiate between constructive and destructive interference. Predict when a reflected wave will be inverted. Predict whether specific traveling waves will produce a standing wave. Identify nodes and antinodes of a standing wave. Section 4 Wave Interactions

31 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Wave Interference Section 4 Wave Interactions Two different material objects can never occupy the same space at the same time. Because mechanical waves are not matter but rather are displacements of matter, two waves can occupy the same space at the same time. The combination of two overlapping waves is called superposition.

32 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Wave Interference, continued In constructive interference, individual displacements on the same side of the equilibrium position are added together to form the resultant wave. Section 4 Wave Interactions

33 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Wave Interference, continued In destructive interference, individual displacements on opposite sides of the equilibrium position are added together to form the resultant wave. Section 4 Wave Interactions

34 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Comparing Constructive and Destructive Interference Section 4 Wave Interactions

35 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Reflection What happens to the motion of a wave when it reaches a boundary? At a free boundary, waves are reflected. At a fixed boundary, waves are reflected and inverted. Section 4 Wave Interactions Free boundary Fixed boundary PhET Wave on a String - Interference, Harmonic Motion, Frequency, Amplitude

36 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Standing Waves Section 4 Wave Interactions

37 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Standing Waves Section 4 Wave Interactions A standing wave is a wave pattern that results when two waves of the same frequency, wavelength, and amplitude travel in opposite directions and interfere. Standing waves have nodes and antinodes. –A node is a point in a standing wave that maintains zero displacement. –An antinode is a point in a standing wave, halfway between two nodes, at which the largest displacement occurs.

38 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Standing Waves, continued Section 4 Wave Interactions Only certain wavelengths produce standing wave patterns. The ends of the string must be nodes because these points cannot vibrate. A standing wave can be produced for any wavelength that allows both ends to be nodes. In the diagram, possible wavelengths include 2L (b), L (c), and 2/3L (d).

39 Copyright © by Holt, Rinehart and Winston. All rights reserved. ResourcesChapter menu Chapter 11 Standing Waves Section 4 Wave Interactions This photograph shows four possible standing waves that can exist on a given string. The diagram shows the progression of the second standing wave for one-half of a cycle.


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