Learning Objectives

Learning Objectives

By the end of this section, you will be able to do the following:

  • Describe a simple harmonic oscillator
  • Relate physical characteristics of a vibrating system to aspects of simple harmonic motion and any resulting waves

The information presented in this section supports the following AP® learning objectives and science practices:

  • 3.B.3.1 The student is able to predict which properties determine the motion of a simple harmonic oscillator and what the dependence of the motion is on those properties. (S.P. 6.4, 7.2)
  • 3.B.3.4 The student is able to construct a qualitative and/or a quantitative explanation of oscillatory behavior given evidence of a restoring force. (S.P. 2.2, 6.2)
  • 6.A.3.1 The student is able to use graphical representation of a periodic mechanical wave to determine the amplitude of the wave. (S.P. 1.4)
  • 6.B.1.1 The student is able to use a graphical representation of a periodic mechanical wave (position versus time) to determine the period and frequency of the wave and describe how a change in the frequency would modify features of the representation. (S.P. 1.4, 2.2)

The oscillations of a system in which the net force can be described by Hooke’s law are of special importance, because they are very common. They are also the simplest oscillatory systems. Simple Harmonic Motion (SHM) is the name given to oscillatory motion for a system where the net force can be described by Hooke’s law, and such a system is called a simple harmonic oscillator. If the net force can be described by Hooke’s law and there is no damping (by friction or other non-conservative forces), then a simple harmonic oscillator will oscillate with equal displacement on either side of the equilibrium position, as shown for an object on a spring in Figure 16.9. The maximum displacement from equilibrium is called the amplitude XX size 12{X} {}. The units for amplitude and displacement are the same, but depend on the type of oscillation. For the object on the spring, the units of amplitude and displacement are meters; whereas for sound oscillations, they have units of pressure (and other types of oscillations have other units). Because amplitude is the maximum displacement, it is related to the energy in the oscillation.

Take-Home Experiment: SHM and the Marble

Find a bowl or basin that is shaped like a hemisphere on the inside. Place a marble inside the bowl and tilt the bowl periodically so the marble rolls from the bottom of the bowl to equally high points on the sides of the bowl. Get a feel for the force required to maintain this periodic motion. What is the restoring force and what role does the force you apply play in the simple harmonic motion (SHM) of the marble?

The figure a shows a spring on a frictionless surface attached to a bar or wall from the left side. On the right side of the spring, an object attached to it with mass m, its amplitude is given by X, and X is equal to zero at the equilibrium level. Force F is applied to it from the right side, shown with left direction pointed red arrow and velocity v is equal to zero. A direction point showing the north and west direction is also given alongside this figure as well as with other four figures. In figure b
Figure 16.9 An object attached to a spring sliding on a frictionless surface is an uncomplicated simple harmonic oscillator. When displaced from equilibrium, the object performs simple harmonic motion that has an amplitude XX size 12{X} {} and a period TT size 12{T} {}. The object’s maximum speed occurs as it passes through equilibrium. The stiffer the spring is, the smaller the period TT size 12{T} {}. The greater the mass of the object is, the greater the period TT size 12{T} {}.

What is so significant about simple harmonic motion? One special thing is that the period TT size 12{T} {} and frequency ff size 12{f} {} of a simple harmonic oscillator are independent of amplitude. The string of a guitar, for example, will oscillate with the same frequency whether plucked gently or hard. Because the period is constant, a simple harmonic oscillator can be used as a clock.

Two important factors do affect the period of a simple harmonic oscillator. The period is related to how stiff the system is. A very stiff object has a large force constant kk size 12{k} {}, which causes the system to have a smaller period. For example, you can adjust a diving board’s stiffness—the stiffer it is, the faster it vibrates, and the shorter its period. Period also depends on the mass of the oscillating system. The more massive the system is, the longer the period. For example, a heavy person on a diving board bounces up and down more slowly than a light one.

In fact, the mass mm size 12{m} {} and the force constant kk size 12{k} {} are the only factors that affect the period and frequency of simple harmonic motion.

Period of Simple Harmonic Oscillator

The period of a simple harmonic oscillator is given by

16.15 T = m k T = m k size 12{T=2π sqrt { { {m} over {k} } } } {}

and, because f=1/Tf=1/T size 12{f=1/T} {}, the frequency of a simple harmonic oscillator is

16.16 f = 1 k m . f = 1 k m . size 12{f= { {1} over {2π} } sqrt { { {k} over {m} } } } {}

Note that neither TT size 12{T} {} nor ff size 12{f} {} has any dependence on amplitude.

Example 16.4 Mechanical Waves

What do sound waves, water waves, and seismic waves have in common? They are all governed by Newton’s laws and they can exist only when traveling in a medium, such as air, water, or rocks. Waves that require a medium to travel are collectively known as mechanical waves.

Take-Home Experiment: Mass and Ruler Oscillations

Find two identical wooden or plastic rulers. Tape one end of each ruler firmly to the edge of a table so that the length of each ruler that protrudes from the table is the same. On the free end of one ruler tape a heavy object such as a few large coins. Pluck the ends of the rulers at the same time and observe which one undergoes more cycles in a time period, and measure the period of oscillation of each of the rulers.

Example 16.5 Calculate the Frequency and Period of Oscillations: Bad Shock Absorbers in a Car

If the shock absorbers in a car go bad, then the car will oscillate at the least provocation, such as when going over bumps in the road and after stopping (See Figure 16.10). Calculate the frequency and period of these oscillations for such a car if the car’s mass (including its load) is 900 kg and the force constant (kk size 12{k} {}) of the suspension system is 6.53×104N/m6.53×104N/m size 12{6 "." "53" times "10" rSup { size 8{4} } `"N/m"} {}.

Strategy

The frequency of the car’s oscillations will be that of a simple harmonic oscillator as given in the equation f=1kmf=1km size 12{f= { {1} over {2π} } sqrt { { {k} over {m} } } } {}. The mass and the force constant are both given.

Solution

  1. Enter the known values of k and m.
    16.17 f = 1 k m = 1 6 . 53 × 10 4 N/m 900 kg f = 1 k m = 1 6 . 53 × 10 4 N/m 900 kg size 12{f= { {1} over {2π} } sqrt { { {k} over {m} } } = { {1} over {2π} } sqrt { { {6 "." "53" times "10" rSup { size 8{4} } "N/m"} over {"900"" kg"} } } } {}
  2. Calculate the frequency.
    16.18 1 72. 6 / s –2 = 1 . 3656 / s –1 1 . 36 / s –1 = 1.36 Hz 1 72. 6 / s –2 = 1 . 3656 / s –1 1 . 36 / s –1 = 1.36 Hz size 12{ { {1} over {2π} } sqrt {"72" "." 6/s rSup { size 8{2} } } =1 "." "36"/s=1 "." "36 Hz"} {}
  3. You could use T=mkT=mk size 12{T=2π sqrt { { {m} over {k} } } } {} to calculate the period, but it is simpler to use the relationship T=1/fT=1/f size 12{T=1/f} {} and substitute the value just found for ff size 12{f} {}.
    16.19 T = 1 f = 1 1 . 356 Hz = 0 . 738 s T = 1 f = 1 1 . 356 Hz = 0 . 738 s size 12{T= { {1} over {f} } = { {1} over {1 "." "36"" Hz"} } =0 "." "737"" s"} {}

Discussion

The values of TT size 12{T} {} and ff size 12{f} {} both seem about right for a bouncing car. You can observe these oscillations if you push down hard on the end of a car and let go.

The Link between Simple Harmonic Motion and Waves

The Link between Simple Harmonic Motion and Waves

If a time-exposure photograph of the bouncing car were taken as it drove by, the headlight would make a wavelike streak, as shown in Figure 16.10. Similarly, Figure 16.11 shows an object bouncing on a spring as it leaves a wavelike "trace of its position on a moving strip of paper. Both waves are sine functions. All simple harmonic motion is intimately related to sine and cosine waves.

The figure shows the front right side of a running car on an uneven rough surface which also shows the driver in the driving seat. There is an oscillating sine wave drawn from left to the right side horizontally throughout the figure.
Figure 16.10 The bouncing car makes a wavelike motion. If the restoring force in the suspension system can be described only by Hooke’s law, then the wave is a sine function. The wave is the trace produced by the headlight as the car moves to the right.
There are two iron paper roll bars standing vertically with a paper strip stitched from one bar to the other. There is a vertical hanging spring just over the middle of the two bars, perpendicular to the strip of the paper, having an object with mass m tied to it. There is a line graph with amplitude scale as X, zero and negative X on the left side of the paper strip, vertically over each other with their points marked. A perpendicular line is drawn through this amplitude scale toward the right with a poi
Figure 16.11 The vertical position of an object bouncing on a spring is recorded on a strip of moving paper, leaving a sine wave.

The displacement as a function of time t in any simple harmonic motion—that is, one in which the net restoring force can be described by Hooke’s law, is given by

16.20 x t = X cos 2 πt T , x t = X cos 2 πt T , size 12{x left (t right )=X"cos" { {2π`t} over {T} } } {}

where XX size 12{X} {} is amplitude. At t=0t=0 size 12{t=0} {}, the initial position is x0=Xx0=X size 12{x rSub { size 8{0} } =X} {}, and the displacement oscillates back and forth with a period TT. (When t=Tt=T, we get x=Xx=X size 12{x=X} {} again because cos=1cos=1.). Furthermore, from this expression for xx size 12{x} {}, the velocity vv size 12{v} {} as a function of time is given by

16.21 v(t)=vmaxsintT,v(t)=vmaxsintT, size 12{v \( t \) = - v rSub { size 8{"max"} } "sin" left ( { {2π`t} over {T} } right )} {}

where vmax=X/T=Xk/mvmax=X/T=Xk/m size 12{v rSub { size 8{"max"} } =2πX/T=X sqrt {k/m} } {}. The object has zero velocity at maximum displacement—for example, v=0v=0 size 12{v=0} {} when t=0t=0 size 12{t=0} {}, and at that time x=Xx=X size 12{x=X} {}. The minus sign in the first equation for v(t)v(t) size 12{v \( t \) } {} gives the correct direction for the velocity. Just after the start of the motion, for instance, the velocity is negative because the system is moving back toward the equilibrium point. Finally, we can get an expression for acceleration using Newton’s second law. [Then we have x(t), v(t), t,x(t), v(t), t, size 12{x \( t \) ,v \( t \) ,t} {} and a(t)a(t) size 12{a \( t \) } {}, the quantities needed for kinematics and a description of simple harmonic motion.] According to Newton’s second law, the acceleration is a=F/m=kx/ma=F/m=kx/m size 12{a=F/m= ital "kx"/m} {}. So, a(t)a(t) size 12{a \( t \) } {} is also a cosine function:

16.22 a ( t ) = kX m cos t T . a ( t ) = kX m cos t T . size 12{a \( t \) = - { { ital "kX"} over {m} } " cos " { {2π t} over {T} } } {}

Hence, a(t)a(t) size 12{a \( t \) } {} is directly proportional to and in the opposite direction to x(t)x(t).

Figure 16.12 shows the simple harmonic motion of an object on a spring and presents graphs of x(t), v(t), x(t), v(t), size 12{x \( t \) ,v \( t \) `} {} and a(t)a(t) size 12{`a \( t \) } {} versus time.

In the figure at the top there are ten springboards with objects of different mass values tied to them. This makes some springs highly compressed some as loosely stretched and some at equilibrium, which are shown as red spherical shaped. Alongside the figure there is a scale given for different amplitude values as x equal to positive X, zero and negative X. the upward and downward pointing arrows are shown with a few springboards.  In the second figure there are three graphs. The first graph shows distanc
Figure 16.12 Graphs of x(t),v(t),x(t),v(t), size 12{x \( t \) ,v \( t \) `} {} and a(t)a(t) size 12{`a \( t \) } {} versus tt size 12{t} {} for the motion of an object on a spring. The net force on the object can be described by Hooke’s law, and so the object undergoes simple harmonic motion. Note that the initial position has the vertical displacement at its maximum value XX size 12{X} {}; vv size 12{v} {} is initially zero and then negative as the object moves down; and the initial acceleration is negative, back toward the equilibrium position and becomes zero at that point.

The most important point here is that these equations are mathematically straightforward and are valid for all simple harmonic motion. They are very useful in visualizing waves associated with simple harmonic motion, including visualizing how waves add with one another.

Check Your Understanding

Suppose you pluck a banjo string. You hear a single note that starts out loud and slowly quiets over time. Describe what happens to the sound waves in terms of period, frequency and amplitude as the sound decreases in volume.

Solution

Frequency and period remain essentially unchanged. Only amplitude decreases as volume decreases.

Check Your Understanding

A babysitter is pushing a child on a swing. At the point where the swing reaches xx size 12{x} {}, where would the corresponding point on a wave of this motion be located?

Solution

xx size 12{x} {} is the maximum deformation, which corresponds to the amplitude of the wave. The point on the wave would either be at the very top or the very bottom of the curve.

PhET Explorations: Masses and Springs

A realistic mass and spring laboratory. Hang masses from springs and adjust the spring stiffness and damping. You can even slow time. Transport the lab to different planets. A chart shows the kinetic, potential, and thermal energy for each spring.

This icon links to a P H E T Interactive activity when clicked.
Figure 16.13 Masses and Springs