Resonance and Sound Waves
| 站点: | Young Education |
| 课程: | Oscillations and Resonance |
| 图书: | Resonance and Sound Waves |
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| 日期: | 2026年11月9日 星期一 16:39 |
1. Standing Waves
Learning outcomes
- I can describe how standing waves are formed through the interference of waves traveling in opposite directions.
- I can identify and distinguish between nodes and antinodes in standing wave patterns.
- I can explain the relationship between harmonics and the fundamental frequency in vibrating systems.
- I can determine the wavelengths and frequencies of different harmonics in strings and air columns.
- I can explain resonance and describe how systems oscillate with maximum amplitude at their natural frequency.
Standing Waves
A standing wave is a wave pattern that appears to remain fixed in position rather than traveling through a medium. Standing waves are produced when two waves with the same frequency, wavelength, and approximately equal amplitude travel in opposite directions and interfere.
Standing waves are important in many vibrating systems, including:
- guitar, violin, and piano strings
- organ pipes and wind instruments
- air columns
- microwave cavities
- antennas
- bridges and buildings
- laboratory wave experiments
Standing waves also provide a clear connection between interference, resonance, wavelength, and frequency.
How Standing Waves Form
Imagine a wave traveling along a stretched string.
When the wave reaches a fixed end, it reflects and travels back along the string. The incoming wave and reflected wave now travel in opposite directions.
The two waves overlap and interfere.
At certain frequencies, this interference creates a stable pattern in which some points remain stationary while other points oscillate strongly.
This pattern is a standing wave.
The individual waves are still traveling. It is the resulting interference pattern that appears stationary.
Conditions for a Stable Standing Wave
A clear standing-wave pattern is produced when the two interfering waves have:
- the same frequency
- the same wavelength
- similar or equal amplitudes
- opposite directions of travel
The waves continuously undergo both constructive and destructive interference.
At particular locations, the interference is always destructive.
At other locations, the interference alternates to produce maximum oscillation.
These locations are called nodes and antinodes.
Nodes
A node is a point on a standing wave where the displacement is always zero.
At a node, the two traveling waves interfere destructively.
If one wave attempts to displace the medium upward, the other produces an equal downward displacement.
The resulting displacement is:
zero
Nodes therefore appear stationary.
Antinodes
An antinode is a point where the oscillation has maximum amplitude.
At an antinode, the interfering waves produce maximum constructive interference during the oscillation.
The particles of the medium move through the largest range.
Therefore:
- nodes → minimum displacement
- antinodes → maximum displacement
Nodes and Antinodes Alternate
Along a standing wave, nodes and antinodes alternate.
A typical pattern is:
Node — Antinode — Node — Antinode — Node
The distance relationships are important.
Distance between adjacent nodes:
λ/2
Distance between adjacent antinodes:
λ/2
Distance from a node to the nearest antinode:
λ/4
where λ represents wavelength.
Determining Wavelength from a Standing Wave
Suppose adjacent nodes are separated by:
0.40 m
Since adjacent nodes are separated by λ/2:
λ/2 = 0.40 m
Therefore:
λ = 0.80 m
If the wave speed is 120 m/s:
v = fλ
120 = f(0.80)
f = 150 Hz
Therefore:
f = 150 Hz
Standing-wave patterns can therefore be used to determine wavelength and frequency experimentally.
Waves on a String
Consider a string fixed at both ends.
The ends cannot move, so both ends must be:
nodes
Only certain wavelengths can fit between these fixed endpoints.
This means the string cannot form a stable standing wave at every possible frequency.
Instead, it has a set of allowed frequencies called its natural frequencies.
Fundamental Frequency
The simplest standing-wave pattern on a string is called the fundamental mode or first harmonic.
For a string fixed at both ends, the fundamental pattern contains:
- a node at each end
- one antinode in the middle
- half of one wavelength along the string
Therefore:
L = λ₁/2
so:
λ₁ = 2L
where:
- L = length of the string
- λ₁ = wavelength of the fundamental
Fundamental Frequency of a String
Using:
v = fλ
and:
λ₁ = 2L
we obtain:
f₁ = v/(2L)
Therefore:
f₁ = v/(2L)
The fundamental frequency is the lowest natural frequency at which the string can form a standing wave.
Example: Fundamental Frequency
A string is:
0.80 m
long.
Wave speed along the string is:
240 m/s
Fundamental wavelength:
λ₁ = 2L
λ₁ = 2(0.80)
λ₁ = 1.60 m
Now:
f₁ = v/λ₁
f₁ = 240/1.60
f₁ = 150 Hz
Harmonics
Higher-frequency standing-wave patterns are called harmonics.
For a string fixed at both ends:
first harmonic = fundamental
second harmonic = 2 × fundamental frequency
third harmonic = 3 × fundamental frequency
and so on.
In general:
fₙ = nf₁
where n is the harmonic number.
Harmonics on a String
For a string fixed at both ends:
| Harmonic | Wavelength | Frequency |
|---|---|---|
| 1st | λ₁ = 2L | f₁ |
| 2nd | λ₂ = L | 2f₁ |
| 3rd | λ₃ = 2L/3 | 3f₁ |
| 4th | λ₄ = L/2 | 4f₁ |
The general wavelength relationship is:
λₙ = 2L/n
Therefore:
fₙ = nv/(2L)
Understanding the Harmonic Number
For a string fixed at both ends, the harmonic number tells us how many half-wavelengths fit along the string.
First harmonic:
L = λ/2
Second harmonic:
L = 2(λ/2)
Third harmonic:
L = 3(λ/2)
In general:
L = nλ/2
This leads directly to:
λₙ = 2L/n
Nodes and Antinodes in String Harmonics
For a string fixed at both ends:
First harmonic:
- 2 nodes
- 1 antinode
Second harmonic:
- 3 nodes
- 2 antinodes
Third harmonic:
- 4 nodes
- 3 antinodes
In general, for the nth harmonic:
- number of antinodes = n
- number of nodes = n + 1
including the fixed endpoints.
Worked Example: Third Harmonic
A string has length:
L = 1.20 m
Find the wavelength of its third harmonic.
Use:
λₙ = 2L/n
λ₃ = 2(1.20)/3
λ₃ = 2.40/3
λ₃ = 0.80 m
If the wave speed is:
v = 200 m/s
then:
f₃ = v/λ₃
f₃ = 200/0.80
f₃ = 250 Hz
Finding the Fundamental from a Higher Harmonic
Suppose the fourth harmonic of a string is:
480 Hz
Since:
f₄ = 4f₁
480 = 4f₁
Therefore:
f₁ = 120 Hz
The other harmonics would include:
f₂ = 240 Hz
f₃ = 360 Hz
f₄ = 480 Hz
f₅ = 600 Hz
Standing Waves in Air Columns
Standing waves can also form in columns of air.
This occurs in musical instruments such as:
- flutes
- clarinets
- recorders
- trumpets
- trombones
- organ pipes
The boundary conditions depend on whether the end of the air column is:
- open
- closed
This changes the allowed standing-wave patterns.
Open Ends and Closed Ends
For the common displacement representation of air-column standing waves:
At an open end, air particles can move freely.
Therefore, an open end is a:
displacement antinode
At a closed end, air particles cannot move freely.
Therefore, a closed end is a:
displacement node
This distinction determines which wavelengths fit inside the air column.
Pressure Nodes and Antinodes
Sound waves can also be described using variations in pressure.
For pressure standing waves:
- an open end is approximately a pressure node
- a closed end is a pressure antinode
Therefore, it is important to know whether a diagram represents:
particle displacement
or:
pressure variation
The node and antinode locations are reversed between these two descriptions.
Open-Open Air Columns
An air column open at both ends has displacement antinodes at both ends.
For the fundamental mode:
L = λ₁/2
Therefore:
λ₁ = 2L
and:
f₁ = v/(2L)
This is the same mathematical relationship as a string fixed at both ends, even though the boundary conditions are physically different.
Harmonics in an Open-Open Pipe
An ideal open-open pipe supports:
- first harmonic
- second harmonic
- third harmonic
- fourth harmonic
- and so on
The relationships are:
λₙ = 2L/n
and:
fₙ = nv/(2L)
Therefore:
fₙ = nf₁
All integer harmonics are possible in the ideal model.
Example: Open Pipe
An open pipe has length:
L = 0.85 m
Take the speed of sound as:
v = 340 m/s
Fundamental wavelength:
λ₁ = 2L
λ₁ = 1.70 m
Fundamental frequency:
f₁ = 340/1.70
f₁ = 200 Hz
Second harmonic:
f₂ = 400 Hz
Third harmonic:
f₃ = 600 Hz
Fourth harmonic:
f₄ = 800 Hz
Closed-Open Air Columns
Now consider an air column that is:
- closed at one end
- open at the other
For displacement:
- closed end = node
- open end = antinode
The shortest standing-wave pattern that satisfies these conditions contains:
one quarter of a wavelength
Therefore:
L = λ₁/4
so:
λ₁ = 4L
Fundamental Frequency of a Closed-Open Pipe
Using:
v = fλ
and:
λ₁ = 4L
we obtain:
f₁ = v/(4L)
This is half the fundamental frequency of an open-open pipe of the same length, assuming the same wave speed.
Harmonics in a Closed-Open Pipe
A closed-open pipe supports only the odd harmonics in the ideal model.
Its frequencies are:
f₁, 3f₁, 5f₁, 7f₁, ...
The allowed frequencies can be written:
fₙ = nv/(4L)
where:
n = 1, 3, 5, 7, ...
The allowed wavelengths are:
λₙ = 4L/n
for odd n.
Why Even Harmonics Are Missing
A closed-open pipe must always have:
- a displacement node at the closed end
- a displacement antinode at the open end
Patterns corresponding to the even harmonics of the fundamental cannot satisfy both boundary conditions simultaneously.
Therefore, the allowed modes correspond to:
1st harmonic
3rd harmonic
5th harmonic
7th harmonic
and so on.
Important Harmonic Numbering
The second allowed mode of a closed-open pipe is actually the:
third harmonic
The third allowed mode is the:
fifth harmonic
This distinction is important.
For example:
First mode → f₁
Second mode → 3f₁
Third mode → 5f₁
Do not automatically assume that the second mode means the second harmonic.
Example: Closed Pipe
A closed-open pipe has length:
L = 0.50 m
Take:
v = 340 m/s
Fundamental frequency:
f₁ = v/(4L)
f₁ = 340/[4(0.50)]
f₁ = 340/2
f₁ = 170 Hz
The next allowed frequency is the third harmonic:
f₃ = 3(170)
f₃ = 510 Hz
The next is:
f₅ = 5(170)
f₅ = 850 Hz
Comparing Standing-Wave Systems
| System | Fundamental Wavelength | Fundamental Frequency | Allowed Harmonics |
|---|---|---|---|
| String fixed at both ends | 2L | v/(2L) | 1, 2, 3, 4... |
| Open-open pipe | 2L | v/(2L) | 1, 2, 3, 4... |
| Closed-open pipe | 4L | v/(4L) | 1, 3, 5, 7... |
This table is one of the most useful summaries for solving standing-wave problems.
Resonance
Every vibrating system has one or more natural frequencies.
If an external periodic force drives the system at or near one of these natural frequencies, the system can oscillate with a much larger amplitude.
This phenomenon is called:
resonance
Examples include:
- pushing a playground swing at the correct rhythm
- vibrating a guitar string
- blowing across an air column
- tuning a radio circuit
- vibration of mechanical structures
Natural Frequency
A natural frequency is a frequency at which a system tends to oscillate when disturbed.
For example, if a stretched string is plucked, it naturally vibrates using combinations of its allowed frequencies.
These frequencies are determined by physical properties such as:
- length
- tension
- mass
- shape
- material
- boundary conditions
Different systems therefore have different natural frequencies.
Driving Frequency
A driving frequency is the frequency of an external force acting repeatedly on a system.
Suppose a swing has a natural frequency.
If someone pushes it randomly, the motion may remain relatively small.
If the pushes occur at an appropriate frequency and phase, energy is transferred efficiently to the swing.
The amplitude increases.
This is resonance.
Maximum Amplitude at Resonance
When the driving frequency is close to the natural frequency:
f_drive ≈ f_natural
the amplitude becomes large.
In an idealized system:
maximum response occurs at resonance
Real systems experience damping, so the exact frequency of maximum amplitude can differ slightly from the undamped natural frequency.
For introductory problems, it is normally treated as occurring at the natural frequency.
Energy Transfer During Resonance
Resonance occurs because energy is transferred efficiently from the driving source to the oscillating system.
If the driving force repeatedly acts in a way that reinforces the motion, the system gains energy.
The amplitude increases until energy supplied by the driving force is balanced by energy losses.
These losses may result from:
- friction
- air resistance
- internal deformation
- sound production
- thermal energy transfer
Damping
Damping is the loss of mechanical energy from an oscillating system.
Greater damping generally:
- reduces the maximum resonant amplitude
- makes the resonance less sharp
- causes oscillations to die away more quickly
A lightly damped system can produce a much larger resonant response than a heavily damped system.
Resonance Curve
If amplitude is plotted against driving frequency, the graph typically shows a peak near the natural frequency.
Far from resonance:
amplitude is relatively small
Near resonance:
amplitude increases
At resonance:
amplitude reaches its maximum
The width and height of the peak depend strongly on damping.
Resonance and Musical Instruments
Musical instruments depend heavily on resonance.
When a guitar string is plucked, the string vibrates at its natural frequencies.
The body of the guitar also vibrates and transfers energy to the surrounding air.
In wind instruments, the air column resonates at particular frequencies determined partly by:
- tube length
- whether the ends are open or closed
- air temperature
- instrument geometry
This produces the instrument's characteristic notes.
Harmonics and Musical Tone
Two instruments can play the same fundamental frequency but sound different.
This occurs partly because they produce different combinations and strengths of harmonics.
The fundamental largely determines the perceived pitch.
The mixture of harmonics contributes to the instrument's:
timbre
or tone quality.
Changing the Length of a String
For a string:
f₁ = v/(2L)
If wave speed remains constant, decreasing L increases the fundamental frequency.
Therefore:
shorter string → higher frequency
longer string → lower frequency
This is why pressing a guitar string against a fret changes its pitch.
The vibrating portion of the string becomes shorter.
Changing Wave Speed on a String
Wave speed on a stretched string depends on tension and linear mass density.
A commonly used relationship is:
v = √(T/μ)
where:
- T = tension
- μ = mass per unit length
Increasing tension increases wave speed.
Since:
f₁ = v/(2L)
increasing the tension generally increases the resonant frequencies.
This is why tightening a musical string raises its pitch.
Changing the Length of an Air Column
For an open-open pipe:
f₁ = v/(2L)
For a closed-open pipe:
f₁ = v/(4L)
In both cases:
longer air column → lower fundamental frequency
shorter air column → higher fundamental frequency
This principle is used in wind instruments.
Speed of Sound and Temperature
The speed of sound in air depends on temperature.
At typical room conditions, it is approximately:
340–343 m/s
As air temperature increases, the speed of sound increases.
Since:
f = v/λ
changes in sound speed can slightly change the resonant frequencies of air columns.
This is one reason temperature can affect the tuning of some instruments.
Worked Problem: String Harmonics
A string is:
L = 1.50 m
long and has wave speed:
v = 180 m/s
Find the fundamental frequency.
f₁ = v/(2L)
f₁ = 180/[2(1.50)]
f₁ = 180/3
f₁ = 60 Hz
Third harmonic:
f₃ = 3f₁
f₃ = 3(60)
f₃ = 180 Hz
Third-harmonic wavelength:
λ₃ = v/f₃
λ₃ = 180/180
λ₃ = 1.0 m
Check:
λ₃ = 2L/3
λ₃ = 3/3
λ₃ = 1.0 m
Worked Problem: Open Air Column
An open-open pipe is:
L = 0.75 m
long.
Take:
v = 330 m/s
Fundamental frequency:
f₁ = 330/[2(0.75)]
f₁ = 330/1.50
f₁ = 220 Hz
Third harmonic:
f₃ = 3(220)
f₃ = 660 Hz
Third-harmonic wavelength:
λ₃ = 2L/3
λ₃ = 1.50/3
λ₃ = 0.50 m
Worked Problem: Closed-Open Air Column
A pipe closed at one end has:
L = 0.40 m
and:
v = 320 m/s
Fundamental frequency:
f₁ = v/(4L)
f₁ = 320/[4(0.40)]
f₁ = 320/1.60
f₁ = 200 Hz
The next allowed harmonic is the third:
f₃ = 3(200)
f₃ = 600 Hz
The next is the fifth:
f₅ = 5(200)
f₅ = 1000 Hz
There is no second or fourth harmonic in the ideal closed-open model.
Worked Problem: Identifying a Harmonic from Nodes
A string fixed at both ends shows:
5 antinodes
Since the nth harmonic has n antinodes:
n = 5
Therefore, the string is vibrating in its:
fifth harmonic
It will also contain:
6 nodes
including the two endpoints.
Worked Problem: Finding Wavelength from Nodes
Adjacent nodes in a standing wave are:
0.25 m apart
Since:
node-to-node distance = λ/2
then:
λ/2 = 0.25
λ = 0.50 m
If:
v = 150 m/s
then:
f = v/λ
f = 150/0.50
f = 300 Hz
Standing Waves Do Not Transport Energy Like Traveling Waves
A traveling wave carries energy from one region to another.
In an ideal standing wave, there is no net energy transfer along the medium averaged over time.
Energy is instead exchanged locally between different forms as parts of the medium oscillate.
This is another important distinction between traveling and standing waves.
Standing Waves in Structures
Standing-wave and resonance effects are important in engineering.
Structures such as:
- bridges
- towers
- aircraft
- machines
- buildings
have natural frequencies.
If repeated forces occur near one of those frequencies, large oscillations may develop.
Engineers therefore analyze natural frequencies and resonance when designing structures.
Preventing Unwanted Resonance
Engineers can reduce dangerous resonance by:
- increasing damping
- changing the mass of the system
- changing stiffness
- changing dimensions
- altering natural frequencies
- isolating vibrations
The goal is often to prevent external driving frequencies from matching important natural frequencies.
Useful Problem-Solving Relationships
For all waves:
v = fλ
For a string fixed at both ends:
λₙ = 2L/n
fₙ = nv/(2L)
For an open-open pipe:
λₙ = 2L/n
fₙ = nv/(2L)
For a closed-open pipe:
λₙ = 4L/n
fₙ = nv/(4L)
where n = 1, 3, 5, 7...
Distance between adjacent nodes:
λ/2
Distance between adjacent antinodes:
λ/2
Distance from node to nearest antinode:
λ/4
A Reliable Strategy for Standing-Wave Problems
First identify the system:
- string fixed at both ends
- open-open pipe
- closed-open pipe
Then determine the boundary conditions.
Ask:
- Where must nodes occur?
- Where must antinodes occur?
- Which harmonics are allowed?
Next determine how much of a wavelength fits into the length L.
Then:
- calculate λ
- use v = fλ
- calculate f
- check that the harmonic number is allowed
- include correct units
Drawing the standing-wave pattern can make the problem much easier.
Common Mistakes
Thinking a standing wave is not made from traveling waves
Standing waves result from interference between waves traveling in opposite directions.
Confusing nodes and antinodes
Nodes have zero displacement. Antinodes have maximum displacement.
Thinking adjacent nodes are one wavelength apart
Adjacent nodes are separated by:
λ/2
Thinking a node and neighboring antinode are λ/2 apart
They are separated by:
λ/4
Assuming L = λ for the fundamental of a fixed string
For the first harmonic:
L = λ/2
so:
λ = 2L
Using open-open formulas for a closed-open pipe
Closed-open fundamental:
λ = 4L
not 2L.
Including even harmonics in an ideal closed-open pipe
Only odd harmonics occur:
1, 3, 5, 7...
Calling the second allowed mode of a closed-open pipe the second harmonic
It is the:
third harmonic
Confusing displacement and pressure nodes in air columns
At an open end there is approximately a displacement antinode but a pressure node.
Assuming resonance means frequency increases
Resonance describes a large response when the driving frequency matches or approaches a natural frequency.
Ignoring units
Length should normally be converted to metres when using wave speed in m/s.
Key Terms
Standing wave — stationary interference pattern produced by waves of the same frequency traveling in opposite directions.
Interference — combination of overlapping waves.
Constructive interference — interference that produces increased displacement.
Destructive interference — interference that reduces or cancels displacement.
Node — point in a standing wave where displacement remains zero.
Antinode — point where the oscillation has maximum amplitude.
Fundamental frequency — lowest natural frequency of a vibrating system.
First harmonic — fundamental mode of vibration.
Harmonic — allowed frequency related to the fundamental frequency.
Natural frequency — frequency at which a system naturally tends to oscillate.
Resonance — large-amplitude response produced when a system is driven near one of its natural frequencies.
Driving frequency — frequency of an external periodic force.
Damping — reduction of oscillation caused by energy loss.
Air column — column of air capable of supporting sound-wave standing patterns.
Open-open pipe — air column open at both ends.
Closed-open pipe — air column closed at one end and open at the other.
Boundary condition — physical restriction determining whether a node or antinode must occur at a boundary.
Displacement node — location where particle displacement is zero.
Pressure node — location where sound-pressure variation is minimal.
Mode — particular allowed standing-wave pattern of a system.
Timbre — characteristic quality of a sound influenced by its harmonic content.
Key Takeaways
- Standing waves form when waves of the same frequency and wavelength travel in opposite directions and interfere.
- Nodes are locations of zero displacement.
- Antinodes are locations of maximum displacement.
- Adjacent nodes are separated by λ/2.
- Adjacent antinodes are separated by λ/2.
- A node and its nearest antinode are separated by λ/4.
- Strings fixed at both ends have nodes at both ends.
- The fundamental wavelength of a fixed string is λ₁ = 2L.
- The fundamental frequency of a fixed string is f₁ = v/(2L).
- Fixed strings support all integer harmonics.
- For strings, fₙ = nf₁ and λₙ = 2L/n.
- An ideal open-open air column also supports all integer harmonics.
- An open end is a displacement antinode and approximately a pressure node.
- A closed end is a displacement node and approximately a pressure antinode.
- A closed-open pipe has fundamental wavelength λ₁ = 4L.
- A closed-open pipe has fundamental frequency f₁ = v/(4L).
- Ideal closed-open pipes support only odd harmonics.
- Resonance occurs when a system is driven near one of its natural frequencies.
- Resonance produces a large amplitude because energy is transferred efficiently to the oscillating system.
- Damping limits resonant amplitude.
- Standing waves explain important aspects of musical instruments, acoustics, engineering, and mechanical vibration.
Check Your Understanding
- Explain how two traveling waves can combine to produce a standing wave.
- Describe the difference between a node and an antinode.
- The distance between two adjacent nodes is 0.60 m. Determine the wavelength.
- A node and its nearest antinode are 0.20 m apart. Determine the wavelength.
- A string fixed at both ends is 1.2 m long. Determine the wavelength of its fundamental mode.
- A 0.80 m string has a wave speed of 240 m/s. Calculate its fundamental frequency.
- The fundamental frequency of a string is 120 Hz. Determine the frequencies of its second, third, and fifth harmonics.
- A string fixed at both ends displays four antinodes. Which harmonic is present? How many nodes are there?
- A string is 1.5 m long and supports waves traveling at 300 m/s. Calculate the wavelength and frequency of its third harmonic.
- An open-open pipe is 0.50 m long. Using a sound speed of 340 m/s, calculate its fundamental frequency and second harmonic frequency.
- A closed-open pipe is 0.50 m long. Using a sound speed of 340 m/s, calculate its fundamental frequency and the next two allowed harmonic frequencies.
- Explain why an ideal closed-open pipe does not support the second harmonic.
- Explain the difference between displacement nodes and pressure nodes at the open and closed ends of an air column.
- Describe resonance in terms of natural frequency, driving frequency, energy transfer, and amplitude.
- A vibrating system has a natural frequency of 250 Hz. Predict what happens to its amplitude as a driving frequency is gradually increased from 100 Hz through 250 Hz and then to 400 Hz. Explain how damping would affect the maximum response.
2. Waves on Strings
Learning outcomes
- I can describe how standing waves form on vibrating strings fixed at both ends.
- I can identify the fundamental frequency and higher harmonics produced by vibrating strings.
- I can explain how tension, length, and mass per unit length affect wave speed and frequency on a string.
- I can calculate relationships between wavelength, frequency, and wave speed for standing waves on strings.
- I can relate standing waves on strings to the operation of musical instruments such as guitars, violins, and pianos.
Waves on Strings
A stretched string can carry transverse waves. When the string is fixed at both ends, waves traveling along the string reflect from the ends and interfere with one another. At certain frequencies, this interference produces stable standing-wave patterns.
This behaviour explains how many stringed musical instruments produce sound, including:
- guitars
- violins
- cellos
- harps
- pianos
The frequencies produced by a string depend mainly on its length, tension, and mass per unit length.
Waves Traveling Along a String
If one end of a stretched string is disturbed, a transverse wave travels along it.
The particles of the string move perpendicular to the direction in which the wave travels.
For example, the wave may travel horizontally while sections of the string move vertically.
The speed of the wave depends on the physical properties of the string rather than simply on how quickly the source vibrates.
Reflection at a Fixed End
When a traveling pulse reaches a fixed end, it reflects.
A reflected pulse at a fixed end is inverted.
If the original pulse is upward, the reflected pulse is downward.
With continuous waves, the incident and reflected waves travel in opposite directions along the same string.
They then overlap and interfere.
Formation of a Standing Wave
A standing wave forms when two waves with the same frequency and wavelength travel in opposite directions and interfere.
On a string fixed at both ends:
- the original wave travels toward an end
- the wave reflects
- the reflected wave travels back
- the two waves overlap
- interference produces nodes and antinodes
At particular frequencies, the reflected wave reinforces a stable standing-wave pattern.
These frequencies are the natural frequencies of the string.
Nodes
A node is a point on a standing wave that remains at zero displacement.
The two ends of a string fixed at both ends must always be nodes because the string cannot move there.
At a node, the two traveling waves continuously interfere destructively.
Nodes can also occur between the ends of the string in higher harmonics.
Antinodes
An antinode is a point where the string oscillates with maximum amplitude.
Antinodes occur halfway between neighboring nodes.
Therefore:
node → antinode → node → antinode → node
The string does not physically remain in the curved shape shown in a standing-wave diagram. Instead, it oscillates between opposite extreme positions.
Spacing of Nodes and Antinodes
For a standing wave:
Adjacent nodes are separated by:
λ/2
Adjacent antinodes are separated by:
λ/2
A node and its nearest antinode are separated by:
λ/4
These relationships allow wavelength to be determined from a standing-wave pattern.
Example: Finding Wavelength from Nodes
Two neighboring nodes are:
0.35 m apart
Since:
node spacing = λ/2
then:
λ/2 = 0.35
Therefore:
λ = 0.70 m
If the wave speed is 140 m/s:
v = fλ
140 = f(0.70)
f = 200 Hz
Why Only Certain Standing Waves Are Possible
Both ends of the string must be nodes.
Therefore, the string length must contain an exact whole number of half-wavelengths.
The condition is:
L = nλ/2
where:
- L = string length
- λ = wavelength
- n = 1, 2, 3, 4, ...
This boundary condition means that only certain wavelengths and frequencies can form stable standing waves.
The Fundamental Mode
The simplest possible standing wave has:
- a node at each end
- one antinode
- one half-wavelength along the string
This is called the:
fundamental mode
or:
first harmonic
For the fundamental:
L = λ₁/2
Therefore:
λ₁ = 2L
Fundamental Frequency
All waves obey:
v = fλ
For the fundamental:
λ₁ = 2L
Therefore:
f₁ = v/(2L)
So:
f₁ = v/(2L)
The fundamental frequency is the lowest natural frequency of the string.
It usually provides the main perceived pitch of a vibrating musical string.
Example: Fundamental Frequency
A string has:
L = 0.75 m
and wave speed:
v = 240 m/s
Fundamental wavelength:
λ₁ = 2L
λ₁ = 2(0.75)
λ₁ = 1.50 m
Frequency:
f₁ = v/λ₁
f₁ = 240/1.50
f₁ = 160 Hz
Higher Harmonics
A string can also vibrate with more than one half-wavelength fitting along its length.
These patterns are called higher harmonics.
Second harmonic:
two half-wavelengths fit along the string
Third harmonic:
three half-wavelengths fit along the string
Fourth harmonic:
four half-wavelengths fit along the string
In general:
L = nλₙ/2
Wavelength of the nth Harmonic
Rearranging:
L = nλₙ/2
gives:
λₙ = 2L/n
As harmonic number increases, wavelength decreases.
For example:
| Harmonic | Wavelength |
|---|---|
| 1st | 2L |
| 2nd | L |
| 3rd | 2L/3 |
| 4th | L/2 |
| 5th | 2L/5 |
Frequency of the nth Harmonic
Since:
v = fλ
and:
λₙ = 2L/n
then:
fₙ = nv/(2L)
Because:
f₁ = v/(2L)
we can also write:
fₙ = nf₁
Therefore:
f₂ = 2f₁
f₃ = 3f₁
f₄ = 4f₁
and so on.
Harmonic Patterns
For a string fixed at both ends:
| Harmonic | Antinodes | Nodes | Frequency |
|---|---|---|---|
| 1st | 1 | 2 | f₁ |
| 2nd | 2 | 3 | 2f₁ |
| 3rd | 3 | 4 | 3f₁ |
| 4th | 4 | 5 | 4f₁ |
| nth | n | n + 1 | nf₁ |
The two fixed ends are included when counting nodes.
Identifying a Harmonic from a Diagram
Suppose a standing-wave pattern contains:
4 antinodes
For a string fixed at both ends:
number of antinodes = harmonic number
Therefore:
n = 4
The pattern is the:
fourth harmonic
It contains:
5 nodes
including the endpoints.
Worked Harmonic Example
A string is:
L = 1.20 m
and waves travel along it at:
v = 180 m/s
Find the fundamental frequency.
f₁ = v/(2L)
f₁ = 180/[2(1.20)]
f₁ = 180/2.40
f₁ = 75 Hz
Third harmonic:
f₃ = 3f₁
f₃ = 3(75)
f₃ = 225 Hz
Third-harmonic wavelength:
λ₃ = 2L/3
λ₃ = 2(1.20)/3
λ₃ = 0.80 m
Check:
v = fλ
v = 225(0.80)
v = 180 m/s
Wave Speed on a String
The wave speed on a stretched string depends mainly on:
- tension
- mass per unit length
The relationship is:
v = √(T/μ)
where:
- v = wave speed in m/s
- T = tension in N
- μ = mass per unit length in kg/m
The symbol μ is the Greek letter mu.
Mass per Unit Length
Mass per unit length is also called linear mass density.
It describes how much mass is contained in each metre of string.
The relationship is:
μ = m/L
where:
- m = mass of the string
- L = length of the string
Units:
kg/m
A thicker or denser string generally has a larger μ than a thin, light string.
Example: Linear Mass Density
A 2.0 m string has mass:
0.010 kg
Then:
μ = m/L
μ = 0.010/2.0
μ = 0.0050 kg/m
This value can then be used to calculate wave speed.
Effect of Tension on Wave Speed
Wave speed is:
v = √(T/μ)
If μ remains constant:
increasing tension increases wave speed
A tightly stretched string transmits disturbances faster than the same string under lower tension.
However, because T is inside a square root, doubling tension does not double wave speed.
Example: Changing Tension
Suppose the tension increases by a factor of 4.
Since:
v ∝ √T
then:
v_new/v_old = √4
Therefore:
v_new = 2v_old
The wave speed doubles.
Effect of Linear Mass Density on Wave Speed
From:
v = √(T/μ)
we see:
v ∝ 1/√μ
Therefore:
larger μ → lower wave speed
smaller μ → higher wave speed
A heavier string per unit length carries waves more slowly when tension is unchanged.
Example: Changing Linear Mass Density
Suppose μ becomes four times larger while tension remains unchanged.
Then:
v_new/v_old = 1/√4
Therefore:
v_new = 1/2 v_old
The wave speed is halved.
Combining Wave Speed and Fundamental Frequency
We know:
f₁ = v/(2L)
and:
v = √(T/μ)
Substituting gives:
f₁ = (1/2L)√(T/μ)
This equation shows the three major factors controlling the fundamental frequency of a string:
- length L
- tension T
- linear mass density μ
Effect of String Length on Frequency
From:
f₁ = (1/2L)√(T/μ)
if tension and linear mass density remain constant:
f₁ ∝ 1/L
Therefore:
longer string → lower frequency
shorter string → higher frequency
If the vibrating length is halved:
frequency doubles
Example: Changing Length
A string has fundamental frequency:
220 Hz
Its vibrating length is reduced to half while tension and μ remain constant.
Since:
f ∝ 1/L
the new frequency is:
2(220)
= 440 Hz
Halving the vibrating length raises the frequency by one octave.
Effect of Tension on Frequency
If L and μ remain constant:
f ∝ √T
Therefore:
higher tension → higher frequency
lower tension → lower frequency
If tension becomes four times larger:
frequency changes by:
√4 = 2
Therefore:
frequency doubles
Effect of Mass per Unit Length on Frequency
If L and T remain constant:
f ∝ 1/√μ
Therefore:
heavier string → lower frequency
lighter string → higher frequency
If μ becomes four times larger:
frequency becomes:
1/√4 = 1/2
Therefore:
frequency is halved
Comparing the Three Factors
| Change | Effect on Fundamental Frequency |
|---|---|
| Increase L | Frequency decreases |
| Decrease L | Frequency increases |
| Increase T | Frequency increases |
| Decrease T | Frequency decreases |
| Increase μ | Frequency decreases |
| Decrease μ | Frequency increases |
The complete relationship is:
f₁ = (1/2L)√(T/μ)
Proportional Reasoning
Suppose the string length doubles.
Since:
f ∝ 1/L
the frequency becomes:
1/2 as large
Suppose tension increases by a factor of 9.
Since:
f ∝ √T
the frequency becomes:
3 times larger
Suppose μ increases by a factor of 9.
Since:
f ∝ 1/√μ
the frequency becomes:
1/3 as large
Recognizing these proportional relationships can often avoid lengthy calculations.
Worked Example: Wave Speed from Tension
A string has:
T = 100 N
μ = 0.0040 kg/m
Calculate wave speed.
v = √(T/μ)
v = √(100/0.0040)
v = √25,000
v ≈ 158 m/s
Worked Example: Fundamental Frequency from String Properties
A string has:
L = 0.80 m
T = 144 N
μ = 0.0040 kg/m
First calculate wave speed:
v = √(144/0.0040)
v = √36,000
v ≈ 190 m/s
Now:
f₁ = v/(2L)
f₁ = 190/[2(0.80)]
f₁ = 190/1.60
f₁ ≈ 119 Hz
Worked Example: Higher Harmonic
Using the same string with:
f₁ ≈ 119 Hz
find the fourth harmonic.
f₄ = 4f₁
f₄ ≈ 4(119)
f₄ ≈ 476 Hz
Alternatively:
f₄ = 4v/(2L)
which gives the same result.
Solving for Tension
The wave-speed equation can be rearranged.
Starting with:
v = √(T/μ)
Square both sides:
v² = T/μ
Therefore:
T = μv²
This allows the required tension to be calculated when wave speed and linear mass density are known.
Example: Finding Tension
A string carries waves at:
v = 200 m/s
and has:
μ = 0.0030 kg/m
Then:
T = μv²
T = 0.0030(200²)
T = 0.0030(40,000)
T = 120 N
Finding Tension from Frequency
Suppose:
L = 0.60 m
μ = 0.0050 kg/m
and the desired fundamental frequency is:
f₁ = 200 Hz
First use:
v = 2Lf₁
v = 2(0.60)(200)
v = 240 m/s
Then:
T = μv²
T = 0.0050(240²)
T = 0.0050(57,600)
T = 288 N
String Length and Musical Pitch
Stringed instruments use the relationship between length and frequency.
On a guitar or violin, pressing a string against the fingerboard or fretboard reduces the length of string that is free to vibrate.
Since:
f ∝ 1/L
a shorter vibrating length produces a higher frequency.
This allows one string to produce many different notes.
Guitar Strings
A guitar string is fixed approximately at:
- the bridge
- the nut or selected fret
These locations act as boundaries for the vibrating portion of the string.
When the player presses the string against a fret:
- vibrating length decreases
- fundamental wavelength decreases
- fundamental frequency increases
- pitch rises
This is one of the main ways guitarists select notes.
Guitar Tuning
A guitar's tuning pegs change the tension in the strings.
Increasing tension:
- increases wave speed
- increases fundamental frequency
- raises pitch
Decreasing tension:
- decreases wave speed
- decreases frequency
- lowers pitch
The player adjusts tension until the string reaches the required frequency.
Different Guitar Strings
Guitar strings are not all identical.
Lower-pitched strings generally have greater mass per unit length.
Since:
f ∝ 1/√μ
a larger μ helps produce a lower fundamental frequency without requiring an extremely long string.
This is why bass strings are usually thicker than treble strings.
Violin Strings
A violin operates using the same physical principles.
The musician changes pitch by pressing a string against the fingerboard.
This changes the effective vibrating length.
Unlike a guitar, a violin typically has no frets, so the player must control the vibrating length very precisely using finger position.
Small changes in length produce changes in frequency and therefore pitch.
Piano Strings
A piano also uses stretched strings, but the strings are struck by hammers rather than plucked or bowed.
Different notes use strings with different combinations of:
- length
- tension
- linear mass density
Low-frequency piano strings are often:
- longer
- heavier per unit length
- wound with additional material
High-frequency strings are generally:
- shorter
- thinner
These design choices allow a piano to produce a very large range of frequencies.
Fundamental and Harmonics in Musical Sound
When a string is plucked, struck, or bowed, it generally does not vibrate in only one mode.
Several standing-wave modes can exist at the same time.
The resulting sound can contain:
- fundamental frequency
- second harmonic
- third harmonic
- fourth harmonic
- higher harmonics
The fundamental strongly influences the perceived pitch.
The relative strengths of the harmonics help determine the instrument's timbre.
Harmonics and Timbre
Suppose two instruments both play:
440 Hz
Both may have the same fundamental frequency.
However, one might have strong second and fourth harmonics while another has stronger third and fifth harmonics.
The waveforms and sounds will therefore be different.
This is one reason a violin and guitar can play the same note but remain easy to distinguish.
Harmonic Nodes on Musical Strings
Musicians can deliberately touch a string lightly at particular positions to force a node to occur there.
This suppresses some vibration modes while allowing particular harmonics to become prominent.
For example, lightly touching the midpoint of a string creates a node there.
The fundamental cannot exist because its midpoint is an antinode.
The second harmonic, however, naturally has a node at the midpoint.
This allows the second harmonic to be emphasized.
Resonance and the Instrument Body
A vibrating string alone moves relatively little air and therefore produces limited sound.
Musical instruments use other structures to improve sound production.
For example:
- a guitar uses its body and soundboard
- a violin uses its body
- a piano uses a large soundboard
The vibrating string transfers energy to these structures.
Their vibrations move more air and produce a much stronger sound.
Resonance plays an important role in this energy transfer.
Why Instruments Need a Soundboard or Body
A thin string has a small surface area.
Although it vibrates rapidly, it does not push a large volume of air.
When its vibration is transferred to a larger surface:
- more air is moved
- stronger pressure variations are produced
- the sound becomes louder
The instrument body also affects which frequencies are amplified most strongly, contributing to timbre.
Real Strings vs Ideal Strings
The simple equations assume an ideal string that is:
- perfectly flexible
- uniform
- under constant tension
- fixed exactly at both ends
Real strings are not perfectly ideal.
Factors such as:
- stiffness
- thickness
- imperfect supports
- material properties
can cause small deviations from the simple harmonic model.
Nevertheless, the ideal model provides an excellent approximation for many situations.
A Complete String Problem
A string has:
L = 1.00 m
T = 180 N
μ = 0.0050 kg/m
First calculate wave speed:
v = √(T/μ)
v = √(180/0.0050)
v = √36,000
v ≈ 190 m/s
Fundamental frequency:
f₁ = v/(2L)
f₁ = 190/2
f₁ ≈ 95 Hz
Third harmonic:
f₃ = 3f₁
f₃ ≈ 285 Hz
Third-harmonic wavelength:
λ₃ = 2L/3
λ₃ ≈ 0.667 m
A Complete Comparison Problem
Two strings have the same length and linear mass density.
String B has four times the tension of String A.
Since:
f ∝ √T
then:
f_B/f_A = √(T_B/T_A)
f_B/f_A = √4
f_B/f_A = 2
Therefore:
String B has twice the fundamental frequency of String A.
Changing More Than One Variable
Sometimes several string properties change simultaneously.
Suppose:
- string length is doubled
- tension becomes four times larger
- μ remains unchanged
Since:
f ∝ √T/L
the tension change multiplies frequency by:
√4 = 2
The length change multiplies frequency by:
1/2
Overall:
2 × 1/2 = 1
Therefore:
the fundamental frequency remains unchanged
This type of reasoning is useful when comparing strings.
Comparing Two Strings
For two strings:
f₁ = (1/2L)√(T/μ)
Therefore, frequency depends on all three variables.
A shorter string does not necessarily have a higher frequency if its tension or linear mass density is also different.
When comparing real strings, consider:
- L
- T
- μ
rather than looking at only one variable.
A Reliable Strategy for String Problems
First identify what is known:
- L
- T
- μ
- v
- λ
- f
- harmonic number n
Then determine which relationship is most useful.
For wave speed:
v = √(T/μ)
For all waves:
v = fλ
For standing waves on a string:
λₙ = 2L/n
For harmonic frequency:
fₙ = nf₁
For fundamental frequency:
f₁ = v/(2L)
or:
f₁ = (1/2L)√(T/μ)
Then:
- convert units if necessary
- identify the harmonic
- calculate the required quantity
- include units
- check whether the result matches the expected trend
Checking Answers Using Physical Reasoning
After calculating, ask whether the result makes sense.
If tension increased, frequency should generally:
increase
If string length increased, frequency should:
decrease
If μ increased, frequency should:
decrease
If harmonic number increased, frequency should:
increase
and wavelength should:
decrease
These qualitative checks can catch calculation errors.
Common Mistakes
Assuming the fundamental wavelength equals the string length
For a string fixed at both ends:
λ₁ = 2L
Forgetting that both ends are nodes
Fixed endpoints cannot oscillate.
Counting nodes instead of antinodes to identify the harmonic
For the nth harmonic:
- antinodes = n
- nodes = n + 1
Thinking adjacent nodes are one wavelength apart
They are separated by:
λ/2
Using the wrong harmonic wavelength
Use:
λₙ = 2L/n
Assuming wave speed depends on frequency
For a given ideal string under fixed conditions, wave speed is determined mainly by T and μ.
Thinking doubling tension doubles frequency
Because:
f ∝ √T
doubling tension multiplies frequency by √2, not 2.
Thinking doubling μ halves frequency
Doubling μ changes frequency by:
1/√2
not 1/2.
Confusing total string mass with linear mass density
Use:
μ = m/L
Using grams instead of kilograms
Convert mass to kilograms before calculating μ in kg/m.
Ignoring the vibrating length
Pressing a string against a fret changes the effective vibrating length.
Assuming a musical string vibrates only at its fundamental
Real strings normally contain several harmonics simultaneously.
Key Terms
Vibrating string — stretched string capable of supporting transverse waves and standing-wave patterns.
Standing wave — stationary interference pattern formed by waves traveling in opposite directions.
Incident wave — wave traveling toward a boundary.
Reflected wave — wave that travels away from a boundary after reflection.
Node — point of zero displacement in a standing wave.
Antinode — point of maximum displacement in a standing wave.
Fundamental frequency — lowest natural frequency of a vibrating system.
First harmonic — fundamental mode of a standing wave.
Harmonic — allowed standing-wave frequency that is an integer multiple of the fundamental for an ideal string fixed at both ends.
Natural frequency — frequency at which a system naturally tends to oscillate.
Wave speed — speed at which a disturbance travels through the string.
Tension — pulling force acting along a stretched string.
Linear mass density — mass per unit length of a string, represented by μ.
Vibrating length — portion of a string that is free to oscillate between its effective fixed boundaries.
Pitch — perception associated mainly with the fundamental frequency of a sound.
Timbre — sound quality influenced by the mixture and relative strength of harmonics.
Resonance — strong response when a system is driven near one of its natural frequencies.
Soundboard — larger vibrating surface that helps transfer energy from strings to the surrounding air.
Key Takeaways
- Waves on stretched strings are transverse waves.
- Reflection and interference can create standing waves on strings.
- A string fixed at both ends must have a node at each end.
- Standing waves occur only at particular allowed wavelengths and frequencies.
- The fundamental mode contains one antinode and two nodes.
- For the fundamental, λ₁ = 2L.
- For the nth harmonic, λₙ = 2L/n.
- The nth harmonic has n antinodes and n + 1 nodes.
- Harmonic frequencies follow fₙ = nf₁ for an ideal string.
- Wave speed and frequency are related by v = fλ.
- Wave speed on a stretched string is v = √(T/μ).
- Linear mass density is μ = m/L.
- Increasing tension increases wave speed and frequency.
- Increasing linear mass density decreases wave speed and frequency.
- Increasing vibrating length decreases the fundamental frequency.
- Fundamental frequency can be written as f₁ = (1/2L)√(T/μ).
- String instruments change pitch by controlling length, tension, and linear mass density.
- Pressing a guitar or violin string shortens its vibrating length and raises its frequency.
- Tuning pegs change tension and therefore frequency.
- Thick or heavy strings have greater linear mass density and generally produce lower frequencies.
- Musical strings usually vibrate in several harmonic modes simultaneously.
- Harmonic content contributes to the timbre of an instrument.
- Instrument bodies and soundboards improve the transfer of vibrational energy to the surrounding air.
Check Your Understanding
- Explain how reflection and interference produce a standing wave on a string fixed at both ends.
- Why must both ends of a string fixed at both ends be nodes?
- A standing wave has adjacent nodes separated by 0.45 m. Determine its wavelength.
- A string is 0.90 m long. Determine the wavelength of its fundamental mode.
- A string is 1.20 m long. Determine the wavelengths of its second, third, and fourth harmonics.
- A string has a fundamental frequency of 150 Hz. Determine the frequencies of its second, third, fifth, and eighth harmonics.
- A standing-wave pattern contains 6 antinodes. Identify the harmonic and determine the total number of nodes.
- A 0.80 m string carries waves at 320 m/s. Calculate its fundamental frequency.
- For the string in Question 8, calculate the frequency and wavelength of the fourth harmonic.
- A string has tension 125 N and linear mass density 0.0050 kg/m. Calculate the wave speed.
- A string is 1.5 m long and has mass 0.012 kg. Calculate its linear mass density.
- The tension in a string is increased from T to 9T while its length and linear mass density remain unchanged. By what factor do its wave speed and fundamental frequency change?
- Two strings have the same length and tension. String B has four times the linear mass density of String A. Compare their wave speeds and fundamental frequencies.
- Explain how a guitarist can raise the pitch of a string by changing either its vibrating length or its tension.
- A string has L = 0.75 m, T = 192 N, and μ = 0.0030 kg/m. Calculate its wave speed, fundamental frequency, third-harmonic frequency, and third-harmonic wavelength.
3. Pipes and Air Columns
Learning outcomes
- I can distinguish between open pipes and closed pipes based on their standing wave patterns and boundary conditions.
- I can identify the harmonics that can form in open and closed air columns.
- I can calculate wavelengths and frequencies for standing waves in pipes using harmonic relationships.
- I can explain how resonance produces amplified sound in air columns and wind instruments.
- I can compare standing wave patterns in strings and air columns, including similarities and differences in their harmonics.
Pipes and Air Columns
Standing waves can form not only on strings but also in columns of air. When sound waves travel through a pipe, they can reflect from the ends of the pipe and interfere with incoming waves. At particular frequencies, this interference creates stable standing-wave patterns.
The possible patterns depend strongly on the boundary conditions at the ends of the pipe. A pipe may be:
- open at both ends
- closed at one end and open at the other
These two systems support different wavelengths and different sets of harmonics.
This physics is central to instruments such as flutes, recorders, clarinets, saxophones, trumpets, trombones, and organ pipes.
Sound Waves in Air
Sound in air is a longitudinal wave.
Air particles oscillate back and forth approximately parallel to the direction in which the wave travels.
As they move, they create alternating regions of:
- compression
- rarefaction
The disturbance transfers energy through the air without the air itself traveling with the wave over large distances.
Standing Waves in an Air Column
A sound wave traveling along a pipe reflects when it reaches an end or boundary.
The incoming and reflected waves overlap.
At certain frequencies, their interference creates a stable standing-wave pattern.
These frequencies are the natural frequencies of the air column.
The air column then resonates strongly at these frequencies.
Displacement Nodes and Antinodes
Standing waves in air can be represented in terms of air-particle displacement.
A displacement node is a position where air particles have minimum displacement.
A displacement antinode is a position where air particles have maximum displacement.
For the simplified pipe models used here:
closed end → displacement node
open end → displacement antinode
These boundary conditions determine which standing-wave patterns are possible.
Why a Closed End Is a Displacement Node
At a closed end, the air cannot move through the solid boundary.
Therefore, the air particles immediately next to the closed end have very little longitudinal displacement.
The closed end is therefore modeled as a:
displacement node
Why an Open End Is a Displacement Antinode
At an open end, the air is free to move.
The air particles can therefore undergo relatively large displacement.
The open end is modeled as a:
displacement antinode
Pressure Nodes and Antinodes
Sound can also be represented using pressure variations rather than particle displacement.
The pattern is reversed.
At an open end:
displacement antinode → pressure node
At a closed end:
displacement node → pressure antinode
Therefore:
| Pipe End | Displacement | Pressure |
|---|---|---|
| Open | Antinode | Node |
| Closed | Node | Antinode |
This distinction is important when interpreting standing-wave diagrams.
Open Pipes
An open pipe is open at both ends.
For particle displacement:
both ends must be antinodes
The standing-wave pattern must therefore fit between two displacement antinodes.
The simplest possible pattern is the fundamental mode.
Fundamental Mode of an Open Pipe
In the fundamental mode:
- there is an antinode at each end
- there is one node in the middle
- half a wavelength fits inside the pipe
Therefore:
L = λ₁/2
so:
λ₁ = 2L
where L is the length of the air column.
Fundamental Frequency of an Open Pipe
For any wave:
v = fλ
For an open pipe:
λ₁ = 2L
Therefore:
f₁ = v/(2L)
where:
- f₁ = fundamental frequency
- v = speed of sound
- L = pipe length
Example: Fundamental of an Open Pipe
An open pipe has length:
L = 0.85 m
Take the speed of sound as:
v = 340 m/s
Fundamental wavelength:
λ₁ = 2(0.85)
λ₁ = 1.70 m
Frequency:
f₁ = 340/1.70
f₁ = 200 Hz
Harmonics in an Open Pipe
An ideal open pipe supports all integer harmonics:
1st, 2nd, 3rd, 4th, 5th, ...
The general wavelength relationship is:
λₙ = 2L/n
The frequency relationship is:
fₙ = nv/(2L)
or:
fₙ = nf₁
where n = 1, 2, 3, 4, ...
Open-Pipe Harmonic Relationships
| Harmonic | Wavelength | Frequency |
|---|---|---|
| 1st | 2L | f₁ |
| 2nd | L | 2f₁ |
| 3rd | 2L/3 | 3f₁ |
| 4th | L/2 | 4f₁ |
| nth | 2L/n | nf₁ |
As harmonic number increases:
- frequency increases
- wavelength decreases
Second Harmonic in an Open Pipe
For the second harmonic:
L = λ₂
Therefore:
λ₂ = L
and:
f₂ = 2f₁
The displacement pattern contains:
antinode → node → antinode → node → antinode
across the pipe.
Third Harmonic in an Open Pipe
For the third harmonic:
L = 3λ₃/2
Therefore:
λ₃ = 2L/3
and:
f₃ = 3f₁
More nodes and antinodes appear as the harmonic number increases.
Worked Example: Open-Pipe Harmonics
An open pipe has:
L = 1.00 m
and:
v = 340 m/s
Fundamental:
f₁ = 340/[2(1.00)]
f₁ = 170 Hz
Second harmonic:
f₂ = 340 Hz
Third harmonic:
f₃ = 510 Hz
Fourth harmonic:
f₄ = 680 Hz
The corresponding third-harmonic wavelength is:
λ₃ = 2(1.00)/3
λ₃ ≈ 0.667 m
Check:
v = fλ
v ≈ 510(0.667)
v ≈ 340 m/s
Closed Pipes
In introductory standing-wave problems, a closed pipe usually means a pipe:
- closed at one end
- open at the other
The closed end must be a displacement node.
The open end must be a displacement antinode.
These different boundary conditions produce a different set of allowed standing waves.
Fundamental Mode of a Closed Pipe
The shortest standing-wave pattern that can connect:
node → antinode
contains one quarter of a wavelength.
Therefore:
L = λ₁/4
so:
λ₁ = 4L
This is different from an open pipe, where:
λ₁ = 2L.
Fundamental Frequency of a Closed Pipe
Using:
v = fλ
and:
λ₁ = 4L
we obtain:
f₁ = v/(4L)
Therefore, for pipes of the same length and with the same sound speed:
a closed pipe has half the fundamental frequency of an open pipe
Example: Closed-Pipe Fundamental
A closed pipe has:
L = 0.50 m
Take:
v = 340 m/s
Fundamental wavelength:
λ₁ = 4(0.50)
λ₁ = 2.00 m
Frequency:
f₁ = 340/2.00
f₁ = 170 Hz
Harmonics in a Closed Pipe
An ideal closed pipe supports only the odd harmonics:
1st, 3rd, 5th, 7th, ...
The allowed wavelengths are:
λₙ = 4L/n
where:
n = 1, 3, 5, 7, ...
The allowed frequencies are:
fₙ = nv/(4L)
or:
fₙ = nf₁
for odd n only.
Closed-Pipe Harmonic Relationships
| Harmonic | Wavelength | Frequency |
|---|---|---|
| 1st | 4L | f₁ |
| 3rd | 4L/3 | 3f₁ |
| 5th | 4L/5 | 5f₁ |
| 7th | 4L/7 | 7f₁ |
The ideal closed pipe does not support:
- second harmonic
- fourth harmonic
- sixth harmonic
Why Even Harmonics Are Missing
A closed pipe must always satisfy both boundary conditions:
closed end = displacement node
and:
open end = displacement antinode
A second-harmonic pattern would not satisfy these two different conditions at the ends.
Only an odd number of quarter-wavelength sections can fit while maintaining a node at one end and an antinode at the other.
Therefore:
L = λ/4, 3λ/4, 5λ/4, 7λ/4, ...
This produces only the odd harmonics.
Modes vs Harmonic Numbers
This distinction is especially important for closed pipes.
The first allowed mode is:
1st harmonic
The second allowed mode is:
3rd harmonic
The third allowed mode is:
5th harmonic
The fourth allowed mode is:
7th harmonic
Therefore, the phrase second mode does not mean second harmonic for a closed pipe.
Worked Example: Closed-Pipe Harmonics
A closed pipe has:
L = 0.80 m
and:
v = 320 m/s
Fundamental frequency:
f₁ = 320/[4(0.80)]
f₁ = 320/3.20
f₁ = 100 Hz
Next allowed harmonic:
f₃ = 3(100)
f₃ = 300 Hz
Next:
f₅ = 5(100)
f₅ = 500 Hz
Next:
f₇ = 7(100)
f₇ = 700 Hz
Finding Wavelength in a Closed Pipe
Using the same pipe:
L = 0.80 m
For the third harmonic:
λ₃ = 4L/3
λ₃ = 4(0.80)/3
λ₃ = 3.20/3
λ₃ ≈ 1.07 m
Check:
v = fλ
v ≈ 300(1.07)
v ≈ 320 m/s
The small difference results from rounding.
Comparing Open and Closed Pipes
The major differences can be summarized as follows:
| Property | Open Pipe | Closed Pipe |
|---|---|---|
| Ends | Open-open | Closed-open |
| Displacement at left end | Antinode | Node |
| Displacement at right end | Antinode | Antinode |
| Fundamental wavelength | 2L | 4L |
| Fundamental frequency | v/(2L) | v/(4L) |
| Harmonics | All integer harmonics | Odd harmonics only |
These differences come directly from the different boundary conditions.
Same Length, Different Fundamental Frequency
Suppose an open pipe and a closed pipe both have:
L = 1.00 m
and:
v = 340 m/s
Open pipe:
f₁ = 340/[2(1.00)]
f₁ = 170 Hz
Closed pipe:
f₁ = 340/[4(1.00)]
f₁ = 85 Hz
Therefore:
f_closed = 1/2 f_open
for equal lengths and sound speeds.
Finding Pipe Length from Frequency
The equations can also be rearranged.
For an open pipe:
f₁ = v/(2L)
Therefore:
L = v/(2f₁)
For a closed pipe:
f₁ = v/(4L)
Therefore:
L = v/(4f₁)
Example: Designing an Open Pipe
An open pipe must have a fundamental frequency of:
425 Hz
Take:
v = 340 m/s
Then:
L = 340/[2(425)]
L = 340/850
L = 0.40 m
An ideal open pipe approximately 0.40 m long would therefore have the required fundamental frequency.
Example: Designing a Closed Pipe
A closed pipe must have a fundamental frequency of:
170 Hz
Take:
v = 340 m/s
Then:
L = 340/[4(170)]
L = 340/680
L = 0.50 m
Resonance in an Air Column
An air column has natural frequencies determined by:
- its length
- its boundary conditions
- the speed of sound
If the air column is driven at one of these frequencies, a large-amplitude standing wave can form.
This is resonance.
At resonance, energy is transferred efficiently from the source to the vibrating air column.
Resonance with a Tuning Fork
A common experiment uses a tuning fork and an adjustable air column.
The tuning fork produces sound at a fixed frequency.
As the air-column length changes, certain lengths satisfy the standing-wave condition.
At these lengths:
- a standing wave forms
- resonance occurs
- the sound becomes noticeably louder
The increase in volume provides evidence that the air column is resonating.
Why Resonance Amplifies Sound
When the driving frequency matches or closely approaches a natural frequency, each cycle of the source transfers energy efficiently to the air column.
The oscillation builds.
This produces:
- larger pressure variations
- larger particle oscillations
- stronger sound
The amplitude does not increase forever because energy is continually lost through processes such as:
- sound radiation
- friction
- viscosity
- thermal effects
Eventually, energy input and energy loss balance.
Wind Instruments
Wind instruments use resonating air columns to produce sound.
Examples include:
- flute
- recorder
- clarinet
- saxophone
- trumpet
- trombone
- organ pipes
The musician creates vibrations that excite particular natural frequencies of the air column.
The resulting resonances determine which frequencies are strongly produced.
Changing Pitch by Changing Air-Column Length
For an open pipe:
f₁ = v/(2L)
For a closed pipe:
f₁ = v/(4L)
In both cases:
f ∝ 1/L
Therefore:
longer air column → lower frequency
shorter air column → higher frequency
This principle is used throughout wind instruments.
Flutes and Recorders
Opening and closing holes changes the effective length of the resonating air column.
Opening a hole closer to the mouthpiece can shorten the effective air column.
A shorter effective length produces:
higher frequency
Closing holes can increase the effective length and produce:
lower frequency
Real instruments are more complicated than ideal pipes, but the standing-wave model explains the basic behaviour.
Trombones
A trombone changes pitch by moving its slide.
Extending the slide increases the effective air-column length.
Therefore:
longer air column → lower frequency
Moving the slide inward shortens the air column and raises the frequency.
Trumpets and Similar Instruments
Instruments such as trumpets use valves to change the effective length of the air path.
Pressing different valve combinations adds sections of tubing.
Increasing the air-column length generally lowers the resonant frequencies.
The player's lips provide the vibrating source that excites resonances in the instrument.
Clarinet and Closed-Pipe Behaviour
A clarinet is often introduced as an approximate example of a closed-open air column because the reed end behaves approximately like a closed end.
This helps explain why its resonance pattern strongly emphasizes odd harmonics.
Real clarinets are more complicated because of:
- tone holes
- bell shape
- bore geometry
- reed behaviour
The ideal closed-pipe model nevertheless captures important features.
Flute and Open-Pipe Behaviour
A flute is often modeled approximately as an open-open air column.
This means it can support a sequence resembling:
f₁, 2f₁, 3f₁, 4f₁, ...
Again, real instruments have corrections due to their geometry and openings.
Organ Pipes
Organ pipes provide particularly clear examples of open and closed air columns.
An organ can contain both:
- open pipes
- stopped or closed pipes
A closed pipe can produce a lower fundamental frequency than an open pipe of the same length.
This allows organ builders to obtain low frequencies using shorter pipes.
Temperature and the Speed of Sound
The speed of sound in air depends on temperature.
At approximately room temperature, it is often taken as:
340–343 m/s
As temperature increases, the speed of sound increases.
Since:
f = v/λ
a change in sound speed can change the resonant frequencies of an air column whose physical length remains fixed.
End Correction
The simple pipe equations assume that the displacement antinode occurs exactly at an open end.
In reality, the oscillating air extends slightly beyond the physical opening.
Therefore, the effective length of the air column is slightly longer than its physical length.
This effect is called:
end correction
For many introductory calculations, end correction is ignored.
For precise acoustic measurements, it can become important.
Strings and Air Columns
Strings and air columns both support standing waves, but their physical waves are different.
A string supports primarily:
transverse waves
Sound in an air column consists of:
longitudinal waves
Both systems can nevertheless be analyzed using:
- nodes
- antinodes
- wavelength
- frequency
- harmonics
- resonance
Fixed String vs Open Pipe
A string fixed at both ends has:
nodes at both ends
An open pipe, using displacement representation, has:
antinodes at both ends
Despite this difference, both have the same fundamental wavelength relationship:
λ₁ = 2L
Both also support:
all integer harmonics
Therefore:
fₙ = nf₁
for both ideal systems.
Fixed String vs Closed Pipe
A string fixed at both ends supports:
all integer harmonics
A closed-open pipe supports:
odd harmonics only
The difference comes from the boundary conditions.
String:
node → node
Closed pipe:
node → antinode
The node-antinode requirement changes the allowed wavelengths.
Comparison of Standing-Wave Systems
| Feature | Fixed String | Open Pipe | Closed Pipe |
|---|---|---|---|
| Wave type | Transverse | Longitudinal sound | Longitudinal sound |
| First end | Node | Displacement antinode | Displacement node |
| Second end | Node | Displacement antinode | Displacement antinode |
| λ₁ | 2L | 2L | 4L |
| f₁ | v/(2L) | v/(2L) | v/(4L) |
| Harmonics | 1, 2, 3, 4... | 1, 2, 3, 4... | 1, 3, 5, 7... |
This comparison shows why boundary conditions are so important in standing-wave systems.
Similarities Between Strings and Air Columns
Both systems:
- form standing waves through interference
- have natural frequencies
- exhibit resonance
- contain nodes and antinodes
- support a fundamental mode
- can support higher harmonics
- obey v = fλ
- produce different frequencies when their effective length changes
These shared principles allow the same wave ideas to explain many different musical instruments.
Important Differences
The physical oscillation is different.
For strings:
the material of the string moves transversely
For sound in pipes:
air particles oscillate longitudinally
Wave speed is also controlled differently.
On a string:
v = √(T/μ)
and depends on tension and linear mass density.
In air:
wave speed depends mainly on properties such as:
- temperature
- gas composition
The boundary conditions are also different.
Complete Open-Pipe Problem
An open pipe is:
L = 0.60 m
Take:
v = 360 m/s
Fundamental:
f₁ = v/(2L)
f₁ = 360/[2(0.60)]
f₁ = 300 Hz
Third harmonic:
f₃ = 3(300)
f₃ = 900 Hz
Third-harmonic wavelength:
λ₃ = 2L/3
λ₃ = 1.20/3
λ₃ = 0.40 m
Check:
v = fλ
v = 900(0.40)
v = 360 m/s
Complete Closed-Pipe Problem
A closed pipe is:
L = 0.75 m
Take:
v = 330 m/s
Fundamental:
f₁ = v/(4L)
f₁ = 330/[4(0.75)]
f₁ = 330/3.00
f₁ = 110 Hz
Third harmonic:
f₃ = 3(110)
f₃ = 330 Hz
Fifth harmonic:
f₅ = 5(110)
f₅ = 550 Hz
There is no second or fourth harmonic in the ideal model.
Complete Comparison Problem
An open pipe and a closed pipe both have length:
0.50 m
Take:
v = 340 m/s
Open pipe:
f₁ = 340/[2(0.50)]
f₁ = 340 Hz
Closed pipe:
f₁ = 340/[4(0.50)]
f₁ = 170 Hz
Therefore:
the open pipe has twice the fundamental frequency of the closed pipe
when their lengths and sound speeds are equal.
Identifying a Pipe from Its Harmonics
Suppose a pipe has resonant frequencies:
120 Hz, 360 Hz, 600 Hz, 840 Hz
These frequencies are:
1 × 120
3 × 120
5 × 120
7 × 120
Only odd harmonics are present.
This strongly suggests an ideal:
closed-open pipe
By contrast, frequencies such as:
120 Hz, 240 Hz, 360 Hz, 480 Hz
match the pattern expected from an ideal:
open-open pipe
A Reliable Strategy for Pipe Problems
First identify the pipe.
Open-open pipe:
λₙ = 2L/n
fₙ = nv/(2L)
n = 1, 2, 3, 4, ...
Closed-open pipe:
λₙ = 4L/n
fₙ = nv/(4L)
n = 1, 3, 5, 7, ...
Then:
- identify the harmonic
- determine the correct wavelength relationship
- use v = fλ if necessary
- check whether the harmonic is allowed
- include units
- verify that the answer fits the boundary conditions
Checking Answers Physically
After calculating, ask:
- Does a longer pipe give a lower fundamental frequency?
- Does a shorter pipe give a higher frequency?
- Does an open pipe include all integer harmonics?
- Does a closed pipe include only odd harmonics?
- Is the open-pipe fundamental wavelength 2L?
- Is the closed-pipe fundamental wavelength 4L?
- Does the standing-wave pattern satisfy the required nodes and antinodes?
These checks can reveal mistakes before the final answer is accepted.
Common Mistakes
Treating every pipe as an open pipe
First identify the boundary conditions.
Calling both ends of an open pipe nodes
For displacement, open ends are antinodes.
Calling the open end of a closed pipe a node
For displacement, it is an antinode.
Confusing pressure and displacement diagrams
Pressure nodes correspond approximately to displacement antinodes, and vice versa.
Using λ = 2L for a closed-pipe fundamental
For a closed-open pipe:
λ₁ = 4L
Including even harmonics in an ideal closed pipe
Closed-open pipes support:
1, 3, 5, 7...
Calling the second allowed mode the second harmonic
For a closed pipe, the second allowed mode is the third harmonic.
Forgetting that open pipes support all integer harmonics
Ideal open-open pipes support:
1, 2, 3, 4...
Confusing string boundary conditions with open-pipe conditions
Fixed string ends are nodes.
Open pipe ends are displacement antinodes.
Ignoring the speed of sound
Use the value provided in the question rather than automatically assuming 340 m/s.
Ignoring end correction in precise experiments
The effective length of a real open pipe can be slightly greater than its physical length.
Key Terms
Air column — volume of air within a pipe that can support standing sound waves.
Open pipe — pipe open at both ends.
Closed pipe — in this context, a pipe closed at one end and open at the other.
Standing wave — stationary interference pattern produced by waves traveling in opposite directions.
Displacement node — location where air-particle displacement is minimal.
Displacement antinode — location where air-particle displacement is maximum.
Pressure node — location where pressure variation is minimal.
Pressure antinode — location where pressure variation is maximum.
Boundary condition — physical requirement imposed at the end of a standing-wave system.
Fundamental frequency — lowest natural frequency of a system.
Harmonic — allowed frequency related to the fundamental frequency.
Natural frequency — frequency at which a system naturally tends to oscillate.
Resonance — large-amplitude oscillation produced when a system is driven near a natural frequency.
Driving frequency — frequency supplied by an external vibrating source.
Effective length — length of the air column that behaves acoustically as though it were vibrating.
End correction — adjustment accounting for vibration extending slightly beyond an open end.
Longitudinal wave — wave in which particles oscillate parallel to the direction of wave travel.
Transverse wave — wave in which particles oscillate perpendicular to the direction of wave travel.
Key Takeaways
- Standing sound waves can form when waves reflect and interfere inside air columns.
- Pipe boundary conditions determine the allowed standing-wave patterns.
- An open end is a displacement antinode and approximately a pressure node.
- A closed end is a displacement node and approximately a pressure antinode.
- An open-open pipe has displacement antinodes at both ends.
- The fundamental wavelength of an open pipe is λ₁ = 2L.
- The fundamental frequency of an open pipe is f₁ = v/(2L).
- Open pipes support all integer harmonics.
- For an open pipe, λₙ = 2L/n and fₙ = nf₁.
- A closed-open pipe has a displacement node at the closed end and an antinode at the open end.
- The fundamental wavelength of a closed pipe is λ₁ = 4L.
- The fundamental frequency of a closed pipe is f₁ = v/(4L).
- Ideal closed pipes support only odd harmonics.
- The second allowed mode of a closed pipe is the third harmonic.
- Resonance occurs when a driving frequency matches or approaches a natural frequency of the air column.
- Resonance produces a large-amplitude standing wave and amplified sound.
- Longer air columns generally produce lower frequencies.
- Shorter air columns generally produce higher frequencies.
- Wind instruments control pitch partly by changing their effective air-column length.
- Fixed strings and open pipes both have λ₁ = 2L and support all integer harmonics, despite having different boundary conditions.
- Closed pipes differ because their node-antinode boundary conditions allow only odd harmonics.
- Standing waves in strings are transverse, while sound waves in air columns are longitudinal.
- The same principles of interference, natural frequency, harmonics, and resonance connect strings, pipes, and musical instruments.
Check Your Understanding
- Explain how a standing wave forms inside an air column.
- For particle displacement, identify whether an open end and a closed end are nodes or antinodes.
- Explain why pressure nodes and displacement nodes occur at different locations in an air column.
- An open pipe is 0.80 m long. Determine the wavelength of its fundamental mode.
- An open pipe is 0.75 m long and the speed of sound is 330 m/s. Calculate its fundamental frequency.
- For the pipe in Question 5, calculate the frequencies of the second, third, and fourth harmonics.
- A closed pipe is 0.60 m long. Determine the wavelength of its fundamental mode.
- A closed pipe is 0.50 m long and the speed of sound is 340 m/s. Calculate its fundamental frequency.
- For the pipe in Question 8, calculate the frequencies of the next three allowed harmonics after the fundamental.
- Explain why an ideal closed pipe supports only odd harmonics.
- An open pipe and a closed pipe are each 1.00 m long. If the speed of sound is 340 m/s, calculate and compare their fundamental frequencies.
- An open pipe has a fundamental frequency of 400 Hz. If the speed of sound is 320 m/s, determine the pipe length.
- A pipe produces strong resonances at 150 Hz, 450 Hz, 750 Hz, and 1050 Hz. Determine whether the pipe behaves more like an ideal open pipe or closed pipe and explain your reasoning.
- Explain how changing the effective length of an air column allows a flute, clarinet, or trombone to produce different pitches.
- Compare a string fixed at both ends, an open-open pipe, and a closed-open pipe. Include their boundary conditions, fundamental wavelengths, allowed harmonics, type of wave, and one musical-instrument application of each.
4. Beats and Interference
Learning outcomes
- I can explain constructive and destructive interference using the principle of superposition.
- I can describe how beats are formed when two waves with slightly different frequencies interfere.
- I can calculate beat frequency from the frequencies of interfering sound waves.
- I can explain how musicians use beats to tune musical instruments accurately.
- I can analyze real-world examples of sound interference and describe their effects on wave amplitude and sound intensity.
Beats and Interference
When two or more waves meet, they combine according to the principle of superposition. The resulting displacement at any point is the sum of the individual wave displacements at that point.
This interaction is called interference.
Interference can make a wave temporarily larger, smaller, or even cancel it completely. In sound waves, interference affects the pressure variations reaching our ears, changing the amplitude and therefore the perceived loudness or sound intensity.
A particularly interesting form of sound interference occurs when two sounds have slightly different frequencies. Their interference produces regular changes in loudness called beats.
The Principle of Superposition
The principle of superposition states:
When two or more waves overlap, the resultant displacement is the algebraic sum of the individual displacements.
For two waves:
y_resultant = y₁ + y₂
This means that waves do not normally destroy one another permanently when they overlap.
Instead:
- the waves meet
- their displacements combine
- interference occurs
- the waves continue travelling afterward
The effect depends strongly on the relative phase of the waves.
Constructive Interference
Constructive interference occurs when waves overlap so that their displacements reinforce each other.
For example, if two crests arrive at the same place at the same time:
positive displacement + positive displacement = larger positive displacement
Similarly:
trough + trough = deeper trough
For two identical waves of amplitude A that are perfectly in phase:
resultant amplitude = 2A
Waves in Phase
Two waves are in phase when corresponding parts of the waves occur together.
For example:
- crest meets crest
- trough meets trough
- compression meets compression
- rarefaction meets rarefaction
For two identical sinusoidal waves, a phase difference of:
0°
produces maximum constructive interference.
A phase difference of:
360°
also represents the same relative phase after one complete cycle.
Destructive Interference
Destructive interference occurs when overlapping waves have displacements in opposite directions.
For example:
positive displacement + negative displacement = smaller resultant displacement
If two waves have equal amplitudes and are exactly opposite in phase:
resultant amplitude = 0
This is called complete destructive interference.
Waves Out of Phase
Two identical sinusoidal waves are completely out of phase when their phase difference is:
180°
Then:
- crest meets trough
- trough meets crest
If their amplitudes are equal, complete cancellation occurs at that location.
If the amplitudes are different, cancellation is only partial.
For example:
Wave 1 amplitude = 5 units
Wave 2 amplitude = 3 units in the opposite direction
Resultant amplitude:
5 − 3 = 2 units
Constructive and Destructive Interference Compared
| Constructive Interference | Destructive Interference |
|---|---|
| Waves reinforce | Waves oppose |
| Resultant amplitude increases | Resultant amplitude decreases |
| Crest meets crest | Crest meets trough |
| Identical waves: phase difference 0° | Identical waves: phase difference 180° |
| Can produce greater sound intensity | Can produce lower sound intensity |
Interference can also occur anywhere between these two extremes.
Interference of Sound Waves
Sound is a longitudinal wave involving variations in pressure.
When two sound waves reach the same location, their pressure variations combine.
Constructive interference can produce larger pressure variations.
Destructive interference can produce smaller pressure variations.
As a result, interference can create locations where sound is:
- louder
- quieter
- nearly cancelled
Amplitude and Sound Intensity
The intensity of a wave is related to the square of its amplitude:
I ∝ A²
where:
- I = intensity
- A = amplitude
This means changes in amplitude can produce much larger changes in intensity.
If the amplitude doubles:
I_new/I_old = (2A)²/A²
I_new = 4I_old
So doubling wave amplitude corresponds to four times the intensity, assuming the waves are otherwise comparable.
Worked Example: Constructive Interference
Two identical coherent sound waves each have amplitude:
A = 2.0 units
They arrive perfectly in phase.
Resultant amplitude:
A_resultant = 2.0 + 2.0
A_resultant = 4.0 units
Compared with one wave, the amplitude has doubled.
Since:
I ∝ A²
the intensity at perfect constructive interference is:
4 times the intensity of either individual wave
Worked Example: Destructive Interference
Two waves have amplitudes:
A₁ = 6 units
A₂ = 4 units
They arrive exactly opposite in phase.
Resultant amplitude magnitude:
A_resultant = |6 − 4|
A_resultant = 2 units
The waves partially cancel.
Complete cancellation would require equal amplitudes as well as the correct phase relationship.
Path Difference and Interference
Interference also depends on how far each wave travels before reaching a particular point.
The difference between the two travel distances is called the path difference.
For two coherent waves, constructive interference occurs when the path difference is:
Δd = nλ
where:
n = 0, 1, 2, 3, ...
Examples include:
0, λ, 2λ, 3λ ...
Destructive Interference and Path Difference
For two coherent waves initially in phase, destructive interference occurs when:
Δd = (n + ½)λ
Examples include:
λ/2, 3λ/2, 5λ/2 ...
The extra half-wavelength causes the waves to arrive out of phase.
This explains why sound can be louder at some locations and quieter at others.
Interference Patterns in Rooms
Sound waves can reach a listener by different paths.
For example, sound may travel:
- directly from a speaker
- after reflecting from a wall
- after reflecting from the floor
- after reflecting from the ceiling
The waves can then interfere.
At some locations:
constructive interference → greater amplitude
At other locations:
destructive interference → smaller amplitude
This can create uneven sound levels around a room.
What Are Beats?
Beats are regular variations in sound amplitude produced when two sound waves with slightly different frequencies interfere.
Suppose one source produces:
440 Hz
and another produces:
442 Hz
The waves repeatedly move:
in phase → out of phase → in phase → out of phase
The listener hears:
loud → quiet → loud → quiet
This repeating variation in loudness is the beat pattern.
Why Beats Form
Consider two waves that begin in phase.
At first:
crest + crest → constructive interference
The sound is relatively loud.
Because the frequencies are slightly different, one wave gradually moves ahead of the other.
Eventually:
crest + trough → destructive interference
The sound becomes relatively quiet.
The faster wave continues gaining phase.
Eventually the waves become aligned again:
crest + crest → constructive interference
The sound becomes loud again.
This cycle repeats.
Beat Frequency
The number of loudness cycles heard each second is called the beat frequency.
For two frequencies f₁ and f₂:
f_beat = |f₁ − f₂|
The absolute value is used because beat frequency is positive.
Worked Example: Beat Frequency
Two tuning forks have frequencies:
f₁ = 440 Hz
f₂ = 444 Hz
Beat frequency:
f_beat = |444 − 440|
f_beat = 4 Hz
The listener hears approximately:
4 beats per second
Worked Example: Close Frequencies
Two speakers produce:
f₁ = 512 Hz
f₂ = 515 Hz
Then:
f_beat = |515 − 512|
f_beat = 3 Hz
The loudness rises and falls three times each second.
Finding an Unknown Frequency
Beat frequency can also be used to determine an unknown frequency.
Suppose a known tuning fork produces:
440 Hz
An unknown source produces:
5 beats per second
Then:
|f_unknown − 440| = 5
Therefore:
f_unknown = 435 Hz
or:
f_unknown = 445 Hz
Beat frequency alone does not tell us whether the unknown frequency is above or below the known frequency.
Additional information is needed.
Resolving the Two Possible Frequencies
Suppose the unknown frequency produces 5 beats per second with a 440 Hz reference.
Possible frequencies are:
435 Hz or 445 Hz
Now suppose the unknown source is adjusted slightly upward in frequency.
If the beat frequency becomes smaller, the unknown frequency was probably below 440 Hz and is moving toward it.
If the beat frequency becomes larger, it may have been above 440 Hz and is moving farther away.
This principle is extremely useful when tuning musical instruments.
Beats and Musical Tuning
Musicians can use beats to compare the frequency of an instrument with a known reference frequency.
Suppose a tuning reference produces:
440 Hz
A string being tuned produces:
443 Hz
Beat frequency:
f_beat = |443 − 440|
f_beat = 3 Hz
The musician hears three beats each second.
Tuning by Reducing Beat Frequency
The musician adjusts the instrument.
Suppose the frequencies change:
443 Hz → 442 Hz → 441 Hz → 440 Hz
The beat frequencies become:
3 Hz → 2 Hz → 1 Hz → 0 Hz
As the instrument approaches the reference frequency, the beats become slower.
When the frequencies match:
f_beat = |440 − 440| = 0 Hz
The beats disappear.
This tells the musician that the frequencies match closely.
Why Beats Are Useful for Tuning
The human ear may have difficulty deciding whether one sustained tone is slightly higher or lower than another.
However, slow changes in loudness can be easy to detect.
Beats therefore transform a small frequency difference into a noticeable rhythm in amplitude.
The closer the two frequencies become:
smaller frequency difference → slower beats
When they match:
frequency difference = 0 → no beats
Tuning a Guitar
Suppose a reference tone is:
330 Hz
A guitar string produces:
326 Hz
Beat frequency:
f_beat = |330 − 326|
f_beat = 4 Hz
The guitarist tightens the string, raising its frequency.
At 328 Hz:
f_beat = 2 Hz
At 329.5 Hz:
f_beat = 0.5 Hz
At 330 Hz:
f_beat = 0 Hz
The disappearing beats indicate that the frequencies have matched.
Tuning Pianos
Beat patterns are also important in piano tuning.
A piano tuner can compare:
- strings with reference frequencies
- different strings producing related pitches
- intervals between notes
The rate of beating provides information about small differences in frequency.
In practical musical tuning, some intervals are intentionally adjusted according to the tuning system being used, so not every useful tuning comparison necessarily aims for zero beats.
The Beat Envelope
When two similar frequencies interfere, the resulting waveform has a rapidly oscillating wave whose amplitude slowly rises and falls.
The outer shape showing the amplitude variation is called the envelope.
The envelope corresponds to the pattern of:
loud → quiet → loud → quiet
The beat frequency describes how often the loudness maxima repeat.
Mathematical Description of Beats
Suppose two equal-amplitude waves are:
y₁ = A cos(2πf₁t)
and:
y₂ = A cos(2πf₂t)
Using superposition:
y = y₁ + y₂
The combination can be expressed as:
y = 2A cos[π(f₁ − f₂)t] cos[π(f₁ + f₂)t]
This shows two important features.
The rapidly changing part corresponds approximately to the average frequency:
f_average = (f₁ + f₂)/2
The slowly changing amplitude produces the beats.
The audible beat frequency is:
f_beat = |f₁ − f₂|
Average Frequency Example
Suppose:
f₁ = 500 Hz
f₂ = 506 Hz
Average frequency:
f_average = (500 + 506)/2
f_average = 503 Hz
Beat frequency:
f_beat = |506 − 500|
f_beat = 6 Hz
The listener therefore hears a tone near 503 Hz whose loudness varies about six times each second.
Beat Period
The time between successive loudness maxima is the beat period.
Since:
T = 1/f
the beat period is:
T_beat = 1/f_beat
For a beat frequency of 4 Hz:
T_beat = 1/4
T_beat = 0.25 s
A loudness maximum occurs approximately every 0.25 seconds.
Worked Example: Beat Period
Two sources produce:
f₁ = 300 Hz
f₂ = 302.5 Hz
Beat frequency:
f_beat = |302.5 − 300|
f_beat = 2.5 Hz
Beat period:
T_beat = 1/2.5
T_beat = 0.40 s
The sound reaches a loudness maximum approximately every 0.40 seconds.
Beats Require Similar Frequencies
The classic beat effect is most easily heard when the two frequencies are relatively close together.
If the frequency difference becomes large, the ear may begin to distinguish two separate tones rather than hearing a clear slow beat pattern.
Therefore, beats are particularly useful for detecting small frequency differences.
Coherence and Stable Interference
For a stable interference pattern, waves should have a predictable phase relationship.
Such waves are described as coherent.
Two independent sound sources may not maintain perfect coherence for long periods.
However, waves derived from related or stable sources can produce clear interference effects.
Beat formation does not require the frequencies to be identical; in fact, the small frequency difference is what produces the changing phase relationship.
Sound Interference in Speakers
Suppose two speakers produce the same frequency.
At one location, the sound waves may arrive in phase.
The listener experiences constructive interference.
At another location, the path difference may cause the waves to arrive out of phase.
The listener experiences destructive interference.
As a person moves around the room, the sound intensity may therefore change.
Noise-Cancelling Headphones
Active noise cancellation uses destructive interference.
A microphone detects unwanted sound.
Electronics produce another sound wave designed to oppose it.
Ideally:
noise wave + opposing wave → reduced resultant amplitude
The unwanted sound becomes quieter.
This is sometimes described as producing anti-noise.
Why Noise Cancellation Is Not Perfect
Perfect cancellation would require the cancelling wave to have exactly the correct:
- frequency
- amplitude
- phase
- timing
at the listener's ear.
Real environments contain complicated sounds arriving from many directions.
Therefore, noise cancellation usually reduces unwanted sound rather than eliminating every sound completely.
It tends to be especially effective for predictable, lower-frequency background noise.
Interference in Concert Halls
Sound interference is an important consideration in the design of:
- concert halls
- theatres
- classrooms
- recording studios
- stadiums
Reflected sound waves can interfere with direct sound.
Poor design can produce areas where certain frequencies become:
- unusually loud
- unusually quiet
- unclear
Acoustic design attempts to control these effects.
Multiple Speakers
Large venues often use many speakers.
If their sound arrives at different times or phases, interference can reduce sound quality.
Engineers therefore consider:
- speaker position
- distance
- timing
- phase
- frequency response
- reflections
Digital systems can introduce carefully controlled delays to coordinate sound arriving from different speakers.
Interference and Standing Waves
Reflected waves can interfere with incoming waves.
Under suitable conditions, this produces standing waves.
Standing waves contain:
- nodes
- antinodes
At a node, the wave amplitude is very small.
At an antinode, the amplitude is large.
Standing waves in rooms can therefore make certain frequencies noticeably louder or quieter at different locations.
Interference in Musical Instruments
Musical instruments depend on wave interference.
Reflections inside:
- strings
- pipes
- air columns
can produce standing waves.
Constructive interference reinforces frequencies that satisfy the instrument's resonance conditions.
This helps determine the frequencies that the instrument can produce strongly.
Sound Intensity and Distance
Interference should not be confused with the normal decrease in intensity as sound spreads.
A sound can become quieter because:
- energy spreads over a larger area
- energy is absorbed
- destructive interference occurs
These are different physical processes.
When analyzing a sound situation, it is important to identify which mechanism is responsible.
Real-World Example: Aircraft Cabins
Aircraft cabins contain relatively steady low-frequency noise from:
- engines
- airflow
- mechanical systems
Active noise-cancelling headphones can analyze this noise and generate an opposing waveform.
Destructive interference reduces the pressure variations reaching the listener.
The result is a quieter perceived environment.
Real-World Example: Vehicle Noise Control
Active noise-control systems can also be used in vehicles.
Microphones detect unwanted sound.
Speakers generate controlled sound waves.
The waves interfere destructively with selected noise frequencies.
The system must continuously adjust because vehicle conditions change with:
- speed
- engine operation
- road surface
- passenger position
Real-World Example: Speaker Placement
Imagine two speakers producing the same 600 Hz tone.
A listener at one position may receive both waves in phase.
The sound is relatively loud.
A second listener may be positioned where one wave travels an additional half-wavelength.
The waves can arrive approximately 180° out of phase.
The second listener may hear a much quieter sound.
This demonstrates that interference depends on location.
Worked Example: Wavelength and Destructive Interference
Suppose sound has:
f = 680 Hz
and the speed of sound is:
v = 340 m/s
Using:
v = fλ
Wavelength:
λ = v/f
λ = 340/680
λ = 0.50 m
For the first destructive interference condition:
Δd = λ/2
Δd = 0.50/2
Δd = 0.25 m
A path difference of 0.25 m can therefore produce destructive interference if the waves began in phase.
Worked Example: Constructive Interference
Using the same wavelength:
λ = 0.50 m
Constructive interference can occur for:
Δd = nλ
Possible path differences include:
0 m, 0.50 m, 1.00 m, 1.50 m ...
At these positions, the waves can arrive in phase.
Moving Through an Interference Pattern
Imagine walking through a room while two coherent speakers produce the same tone.
As your position changes:
- path difference changes
- phase difference changes
- interference changes
You might hear:
loud → quiet → loud → quiet
This is an interference pattern caused by position.
It should not be confused with beats, which result from waves having slightly different frequencies.
Beats vs Spatial Interference
These two effects can sound superficially similar but have different causes.
| Beats | Spatial Interference |
|---|---|
| Usually slightly different frequencies | Can use the same frequency |
| Loudness changes with time | Loudness changes with position |
| Relative phase continually changes | Phase difference depends on path difference |
| Beat rate = frequency difference | Pattern spacing depends on wavelength and geometry |
This distinction is important.
Interference Does Not Destroy Energy
When destructive interference produces a low-amplitude region, the energy has not simply disappeared.
Interference changes how wave energy is distributed through space.
In a larger wave system, regions of destructive interference are associated with energy being redistributed elsewhere.
This is another example of conservation of energy.
Interference in Other Waves
Interference is not limited to sound.
The principle of superposition applies to many types of waves, including:
- water waves
- electromagnetic waves
- light
- radio waves
- microwaves
The details differ, but constructive and destructive interference remain fundamental wave behaviours.
A Complete Beat Problem
Two sound sources produce:
f₁ = 438 Hz
f₂ = 442 Hz
Beat frequency:
f_beat = |442 − 438|
f_beat = 4 Hz
Average frequency:
f_average = (442 + 438)/2
f_average = 880/2
f_average = 440 Hz
Beat period:
T_beat = 1/4
T_beat = 0.25 s
Therefore, the listener hears a tone near 440 Hz whose amplitude rises and falls four times each second.
A Tuning Problem
A piano string is compared with a:
440 Hz
reference tone.
Initially, the musician hears:
6 beats per second
Possible string frequencies are:
434 Hz or 446 Hz
The musician slightly increases the string frequency.
The beat frequency falls to:
4 Hz
This indicates that the string is moving toward 440 Hz.
Therefore, the original string frequency was:
434 Hz
After adjustment:
436 Hz
would produce 4 beats per second.
The musician continues increasing the frequency until the beats disappear at approximately:
440 Hz
Common Mistakes
Thinking interference permanently changes the original waves
The waves superpose while overlapping and then continue propagating.
Thinking constructive interference means two waves have the same frequency
Constructive interference describes how their displacements combine at a particular place and time.
Thinking destructive interference always produces zero amplitude
Complete cancellation requires appropriate phase and equal amplitudes.
Confusing beats with ordinary interference patterns
Beats are produced by slightly different frequencies and create a time-varying amplitude.
Adding frequencies to find beat frequency
Beat frequency is the absolute difference:
f_beat = |f₁ − f₂|
Using the average frequency as the beat frequency
The average frequency describes the approximate pitch of the rapidly oscillating sound, not the beat rate.
Thinking zero beats means there is no sound
Zero beats means the frequencies match. The sound itself can still be strong.
Assuming a beat frequency identifies an unknown frequency uniquely
An unknown frequency may be either above or below the reference frequency.
Thinking destructive interference violates conservation of energy
Interference redistributes wave energy rather than destroying it.
Key Terms
Superposition — principle stating that overlapping wave displacements add algebraically.
Interference — combination of overlapping waves according to superposition.
Constructive interference — interference in which wave displacements reinforce one another.
Destructive interference — interference in which wave displacements oppose one another.
Phase — position of a point within a wave cycle relative to another wave or reference.
In phase — waves having corresponding parts of their cycles aligned.
Out of phase — waves having different positions within their cycles.
Path difference — difference between distances travelled by two waves to reach a point.
Coherent waves — waves maintaining a predictable phase relationship.
Beat — periodic variation in amplitude caused by interference between waves with slightly different frequencies.
Beat frequency — number of amplitude or loudness cycles per second, equal to the absolute difference between the two frequencies.
Beat period — time between successive beat maxima.
Envelope — slowly varying outline of the amplitude of a beat waveform.
Sound intensity — rate of sound energy transfer per unit area.
Active noise cancellation — use of controlled destructive interference to reduce unwanted sound.
Key Takeaways
- The principle of superposition states that overlapping wave displacements add algebraically.
- Constructive interference occurs when wave displacements reinforce each other.
- Destructive interference occurs when wave displacements oppose each other.
- Equal waves perfectly in phase can produce twice the individual amplitude.
- Equal waves 180° out of phase can completely cancel at a particular location.
- Wave intensity is proportional to amplitude squared.
- Path difference determines whether coherent waves arrive in or out of phase.
- For initially in-phase coherent waves, constructive interference occurs when Δd = nλ.
- Destructive interference occurs when Δd = (n + ½)λ.
- Beats result from interference between waves with slightly different frequencies.
- The changing phase relationship causes alternating constructive and destructive interference.
- Beat frequency is calculated using f_beat = |f₁ − f₂|.
- Beat period is T_beat = 1/f_beat.
- The approximate pitch of two nearby frequencies is related to their average frequency.
- Musicians can tune instruments by listening for beats.
- As two frequencies approach each other, the beats become slower.
- When the frequencies match, the beats disappear.
- Sound interference affects the amplitude and intensity heard at different locations.
- Active noise cancellation uses destructive interference to reduce unwanted sound.
- Acoustic engineers must consider interference when designing rooms and multi-speaker sound systems.
- Beats and spatial interference are related through superposition but should not be confused: beats vary mainly with time, while spatial interference patterns vary with position.
Check Your Understanding
- State the principle of superposition.
- Explain the difference between constructive and destructive interference.
- Two identical waves each have an amplitude of 3.0 cm and arrive perfectly in phase. What is their resultant amplitude?
- Two waves with amplitudes of 7.0 cm and 5.0 cm arrive exactly opposite in phase. Calculate the magnitude of their resultant amplitude.
- Explain why two equal-amplitude waves 180° out of phase can completely cancel.
- Two tuning forks produce frequencies of 440 Hz and 446 Hz. Calculate the beat frequency.
- Two sound sources produce 256 Hz and 259 Hz. Calculate both the beat frequency and beat period.
- A musician hears 4 beats per second when comparing an unknown note with a 500 Hz reference. What are the two possible frequencies of the unknown note?
- Explain how the musician could determine which of the two possible frequencies in Question 8 is correct.
- Explain why the beat frequency decreases as a musical instrument approaches the correct tuning.
- A sound wave has a wavelength of 0.80 m. Determine the smallest non-zero path difference that would produce constructive interference and the smallest path difference that would produce destructive interference for two initially in-phase waves.
- Two equal-amplitude sound waves interfere constructively and produce twice the amplitude of either individual wave. How does the resulting intensity compare with the intensity of one wave?
- Explain how active noise-cancelling headphones use destructive interference and why perfect cancellation is difficult in a real environment.
- A student walks through a room containing two speakers producing the same frequency and hears alternating loud and quiet regions. Explain why this is an interference pattern rather than a beat pattern.
- Two musical instruments produce frequencies of 392 Hz and 395 Hz. Analyze what a listener would hear, calculate the beat frequency and beat period, and explain how a musician could use the observed beats to tune the instruments to the same frequency.
5. The Doppler Effect
Learning outcomes
- I can explain how relative motion between a source and an observer causes a Doppler shift in observed frequency.
- I can distinguish between the effects of a moving source and a moving observer on wave frequency and wavelength.
- I can describe how radar and sonar systems use the Doppler effect to measure speed and motion.
- I can explain redshift and blueshift in electromagnetic waves and relate them to the motion of stars and galaxies.
- I can analyze applications of the Doppler effect in astronomy, medicine, navigation, and modern technology.
The Doppler Effect
The Doppler effect is the change in the observed frequency of a wave caused by relative motion between the wave source and the observer.
A familiar example is the sound of an emergency vehicle passing by. As it approaches, the siren sounds higher in pitch. After it passes and moves away, the siren sounds lower.
The siren itself does not suddenly change its emitted frequency. The difference occurs because motion changes how frequently the wavefronts reach the observer.
The basic pattern is:
approaching → higher observed frequency
moving away → lower observed frequency
The Doppler effect occurs with many types of waves, including sound, radio waves, microwaves, radar signals, ultrasound, and light.
Wave Speed, Frequency, and Wavelength
All waves follow the relationship:
v = fλ
where:
- v = wave speed
- f = frequency
- λ = wavelength
For sound travelling through still air, the wave speed is mainly determined by the properties of the air, including temperature.
A moving sound source does not normally make the sound travel faster through the air in front of it. Instead, the motion changes the spacing between successive wavefronts.
A Stationary Source
Consider a stationary sound source producing waves at a constant frequency.
Because the source remains in the same position between successive wave emissions, the wavefronts spread outward with equal spacing.
The wavelength is the same in every direction.
A stationary observer therefore detects the same frequency that the source emits:
f_observed = f_source
assuming there is no relative motion.
A Moving Source
Now suppose the source moves toward an observer.
Between producing one wavefront and the next, the source moves forward.
Therefore, each new wavefront begins slightly closer to the previous wavefront in front of the source.
The waves become compressed.
Therefore:
smaller λ → higher observed f
because the wave speed in the medium remains approximately constant.
Behind the moving source, the opposite occurs.
The wavefronts become more widely spaced:
larger λ → lower observed f
Approaching Source
When a sound source approaches a stationary observer:
- wavefronts are compressed
- wavelength decreases
- wavefronts arrive more frequently
- observed frequency increases
- observed pitch increases
Therefore:
f_observed > f_source
This explains the higher-pitched sound of an approaching siren.
Receding Source
When the source moves away:
- wavefronts are spread apart
- wavelength increases
- wavefronts arrive less frequently
- observed frequency decreases
- observed pitch decreases
Therefore:
f_observed < f_source
Doppler Equation for a Moving Sound Source
For a source moving toward a stationary observer:
f_observed = f_source × v/(v − v_source)
For a source moving away:
f_observed = f_source × v/(v + v_source)
where:
- f_observed = frequency detected by observer
- f_source = emitted frequency
- v = speed of sound
- v_source = speed of source
The signs reflect whether the source is approaching or receding.
Worked Example: Approaching Source
An ambulance siren produces:
f_source = 700 Hz
The ambulance approaches at:
v_source = 25 m/s
Take the speed of sound as:
v = 340 m/s
Then:
f_observed = 700 × 340/(340 − 25)
f_observed = 700 × 340/315
f_observed ≈ 756 Hz
The observer hears a frequency higher than 700 Hz.
Worked Example: Receding Source
After the ambulance passes, it moves away at the same speed.
f_observed = 700 × 340/(340 + 25)
f_observed = 700 × 340/365
f_observed ≈ 652 Hz
The observer therefore hears:
approaching: about 756 Hz
actual siren: 700 Hz
receding: about 652 Hz
This produces the familiar sudden change in pitch as the vehicle passes.
Moving Observer
The Doppler effect also occurs when the observer moves while the source remains stationary.
In this case, the wavelength in the medium is not changed by the observer's motion.
Instead, the observer moves through the existing wavefronts at a different rate.
If the observer moves toward the source:
more wavefronts encountered each second → higher observed frequency
If the observer moves away:
fewer wavefronts encountered each second → lower observed frequency
Moving Observer Equation
For a stationary source and an observer moving toward it:
f_observed = f_source × (v + v_observer)/v
For an observer moving away:
f_observed = f_source × (v − v_observer)/v
The observer's motion changes the rate at which wavefronts are encountered.
Moving Source vs Moving Observer
The two situations produce similar frequency changes, but the physical mechanisms are different.
| Moving Source | Moving Observer |
|---|---|
| Changes wavefront spacing | Does not change wavefront spacing in the medium |
| Changes wavelength | Wavelength in the medium remains unchanged |
| Source moves between emissions | Observer moves through existing wavefronts |
| Approach compresses wavelength | Approach increases encounter rate |
| Recession stretches wavelength | Recession decreases encounter rate |
This distinction is especially important for sound, because sound travels through a medium.
Both Source and Observer Moving
If both move, both effects can be included.
A useful general form for sound is:
f_observed = f_source × (v ± v_observer)/(v ∓ v_source)
The signs depend on the directions of motion.
A reliable way to choose them is to think physically:
- motion toward each other should increase observed frequency
- motion apart should decrease observed frequency
It is better to understand the physical situation than simply memorize signs.
Worked Example: Moving Source and Observer
A horn emits:
f_source = 500 Hz
An observer moves toward the source at:
v_observer = 10 m/s
The source also moves toward the observer at:
v_source = 20 m/s
Using:
v = 340 m/s
f_observed = 500 × (340 + 10)/(340 − 20)
f_observed = 500 × 350/320
f_observed ≈ 547 Hz
Because both motions bring the source and observer together, the observed frequency is significantly higher.
Frequency Is Not Loudness
A Doppler shift changes observed frequency.
It does not directly mean the sound has become more intense.
As an approaching vehicle gets closer, its sound may also become louder, but this is mainly because the distance to the source decreases.
Therefore:
frequency → pitch
intensity → loudness
These effects should not be confused.
Frequency Is Not Wave Speed
Another common misconception is that the approaching waves travel faster.
For sound in the same stationary medium:
wave speed remains approximately constant
The moving source changes the wavelength, not the propagation speed.
Since:
v = fλ
a shorter wavelength corresponds to a higher frequency detected by the stationary observer.
Doppler Shift
The difference between the observed and emitted frequency is called the Doppler shift.
It can be written:
Δf = f_observed − f_source
For an approaching source:
Δf > 0
For a receding source:
Δf < 0
Sometimes only the magnitude of the shift is required:
|Δf| = |f_observed − f_source|
Radar
Radar uses electromagnetic waves, often in the radio or microwave region, to detect objects and measure properties such as:
- distance
- direction
- speed
- motion
A radar system transmits an electromagnetic signal toward an object.
The signal reflects from the object and returns to the detector.
If the object is moving, the reflected signal can have a different frequency.
This Doppler shift can be used to determine the object's radial velocity.
Doppler Radar
Consider a vehicle moving toward a radar system.
The returning signal experiences a frequency shift.
The radar electronics compare:
transmitted frequency
with:
received frequency
The difference provides information about the vehicle's motion.
A larger Doppler shift generally corresponds to a greater component of velocity toward or away from the radar.
Radial Velocity
The Doppler effect measures motion along the line between the detector and the object.
This is called radial velocity.
An object moving directly toward the detector produces a strong Doppler shift for its speed.
An object moving perpendicular to the detector's line of sight may have little or no radial Doppler shift at that instant.
Therefore, Doppler systems do not automatically measure the object's complete velocity vector.
Doppler Radar Approximation
For reflected electromagnetic waves when the target speed is much smaller than the speed of light, the magnitude of the Doppler shift is approximately:
|Δf| ≈ 2f₀v_r/c
where:
- Δf = Doppler frequency shift
- f₀ = transmitted frequency
- v_r = radial speed
- c = speed of light
The factor of 2 occurs because the wave experiences Doppler effects on the trip to the moving target and again when the reflected wave returns.
Applications of Doppler Radar
Doppler radar is used in:
- vehicle speed measurement
- weather monitoring
- aviation
- navigation
- motion sensors
- sports measurement
- satellite tracking
Its ability to detect motion without direct physical contact makes it extremely useful.
Weather Radar
Weather radar can detect motion within storms.
Radar signals reflect from:
- raindrops
- snow
- ice particles
- other precipitation
Doppler shifts reveal motion toward or away from the radar.
Meteorologists can use this information to study:
- wind motion
- storm rotation
- precipitation movement
- severe weather development
Sonar
Sonar uses sound waves rather than electromagnetic waves.
A sonar system can transmit sound through water and detect reflected echoes.
Sonar can be used to determine:
- distance
- depth
- position
- motion
- speed
If the reflecting object moves relative to the sonar system, the reflected sound experiences a Doppler shift.
Doppler Sonar
Suppose a submarine sends a sound wave toward another moving object.
The reflected frequency can differ from the transmitted frequency.
By analyzing this shift, the system can estimate the object's radial motion.
Applications include:
- underwater navigation
- submarine detection
- ocean-current measurements
- ship-speed measurements
- underwater research
Radar vs Sonar
| Radar | Sonar |
|---|---|
| Uses electromagnetic waves | Uses sound waves |
| Commonly used in air and space | Commonly used underwater |
| Waves can travel through vacuum | Sound requires a medium |
| Can measure Doppler shifts | Can measure Doppler shifts |
| Used for aircraft, weather and vehicles | Used for ships, submarines and ocean measurements |
Both can use the Doppler effect to obtain information about motion.
Doppler Ultrasound
The Doppler effect has important medical applications.
Doppler ultrasound sends high-frequency sound waves into the body.
The waves can reflect from moving structures, especially blood cells.
Motion of the blood produces a Doppler shift in the reflected ultrasound.
Doctors can use this shift to estimate blood-flow velocity.
Measuring Blood Flow
Consider ultrasound reflecting from blood moving toward the probe.
The reflected frequency is shifted upward.
Blood moving away produces a lower returned frequency.
By analyzing the frequency shift, medical equipment can determine information about:
- direction of blood flow
- speed of blood flow
- patterns of circulation
Doppler Ultrasound Equation
A commonly used simplified relationship is:
Δf = 2f₀v cos θ / c
where:
- Δf = measured frequency shift
- f₀ = transmitted ultrasound frequency
- v = blood-flow speed
- θ = angle between the ultrasound beam and blood-flow direction
- c = speed of sound in the tissue
The angle is important.
If the beam is parallel to the flow:
θ = 0°
and:
cos 0° = 1
The Doppler shift is greatest.
Why the Ultrasound Angle Matters
If the ultrasound beam is perpendicular to blood flow:
θ = 90°
Since:
cos 90° = 0
the ideal Doppler shift is:
Δf = 0
even though the blood is moving.
Therefore, Doppler measurements depend on the component of velocity along the ultrasound beam.
This is another example of radial motion being important.
Medical Applications
Doppler ultrasound can help investigate:
- blood flow through arteries
- blood flow through veins
- heart function
- circulation
- fetal blood flow
- narrowing of blood vessels
It provides information without requiring direct measurement inside the blood vessel.
Doppler Effect and Light
The Doppler effect also applies to electromagnetic waves such as light.
When a light source and observer move relative to each other, the observed frequency and wavelength can change.
For visible light:
approaching source → higher observed frequency → shorter wavelength
receding source → lower observed frequency → longer wavelength
These changes are called blueshift and redshift.
Blueshift
A source moving toward the observer produces a shift toward shorter wavelengths.
This is called blueshift.
It does not necessarily mean the object literally appears blue.
Instead, its entire spectrum is shifted toward shorter wavelengths.
Therefore:
approaching → shorter λ → higher f → blueshift
Redshift
A source moving away produces a shift toward longer wavelengths.
This is called redshift.
Again, the object does not necessarily appear red to the eye.
Its spectral features move toward longer wavelengths.
Therefore:
receding → longer λ → lower f → redshift
Spectral Lines
Stars and galaxies produce spectra containing identifiable spectral lines.
Laboratory measurements tell scientists the normal wavelengths of these lines.
Astronomers compare:
rest wavelength
with:
observed wavelength
If the observed lines shift toward longer wavelengths:
redshift
If they shift toward shorter wavelengths:
blueshift
The shift can reveal motion along our line of sight.
Measuring Wavelength Shift
The wavelength shift can be written:
Δλ = λ_observed − λ_rest
For relatively low speeds compared with the speed of light:
v_r/c ≈ Δλ/λ_rest
where:
- v_r = radial velocity
- c = speed of light
- Δλ = wavelength shift
- λ_rest = original wavelength
This approximation is useful when:
v << c
At speeds approaching the speed of light, relativistic Doppler equations are required.
Worked Example: Stellar Redshift
A spectral line normally occurs at:
λ_rest = 500 nm
It is observed at:
λ_observed = 500.5 nm
Shift:
Δλ = 500.5 − 500
Δλ = 0.5 nm
Using:
v_r/c ≈ Δλ/λ_rest
v_r/c ≈ 0.5/500
v_r/c ≈ 0.001
Using:
c = 3.0 × 10⁸ m/s
v_r ≈ 0.001(3.0 × 10⁸)
v_r ≈ 3.0 × 10⁵ m/s
or:
v_r ≈ 300 km/s
Because the wavelength increased, the source is receding.
Stars and the Doppler Effect
Astronomers use Doppler shifts to study stellar motion.
They can determine whether a star is moving:
- toward Earth
- away from Earth
They can also measure how quickly the star is moving along our line of sight.
This information helps astronomers investigate:
- binary stars
- stellar motion
- galactic rotation
- exoplanets
Detecting Exoplanets
A planet and its star both orbit their common center of mass.
Although the star moves much less than the planet, it can undergo a small periodic motion.
As the star moves:
toward Earth → slight blueshift
then:
away from Earth → slight redshift
Repeated shifts in the star's spectrum can provide evidence for an orbiting planet.
This technique is called the radial velocity method.
Binary Stars
Two stars orbiting each other can also produce periodic Doppler shifts.
As one star moves toward Earth, its spectral lines become blueshifted.
As it moves away, they become redshifted.
These patterns can reveal:
- orbital speeds
- orbital periods
- properties of the stellar system
The stars may therefore reveal their motion even when their orbital movement cannot be directly seen.
Galaxies and Redshift
Many distant galaxies show redshifted spectra.
Their spectral features appear at wavelengths longer than their laboratory values.
This provides evidence that many galaxies are receding from us.
Observations of galactic redshift played a major role in developing our understanding of the expanding universe.
For very distant galaxies, however, cosmological redshift is best understood through the expansion of space, rather than simply treating it as an ordinary sound-like Doppler effect.
Doppler Shift vs Cosmological Redshift
For nearby objects moving through space, Doppler shift provides a useful description of wavelength changes caused by relative motion.
For very distant galaxies, expansion of the universe stretches the wavelength of travelling light.
Therefore, although both effects can produce redshift:
Doppler redshift → relative motion
cosmological redshift → expansion of space during light travel
At introductory levels they are often discussed together, but the distinction is important.
Navigation
Doppler measurements can contribute to navigation systems.
If a vehicle measures frequency shifts from known signals or reflected waves, it can obtain information about relative motion.
Applications can include:
- aircraft navigation
- spacecraft navigation
- marine navigation
- satellite tracking
- autonomous systems
Doppler measurements are especially useful because they provide information about velocity, not just position.
Satellites
Radio signals transmitted between satellites and ground stations can experience Doppler shifts.
As a satellite approaches a receiver:
observed frequency increases
As it moves away:
observed frequency decreases
Tracking these changes can provide information about:
- orbital motion
- relative velocity
- satellite position and trajectory
Spacecraft Navigation
Space agencies can monitor radio signals exchanged with spacecraft.
Precise measurements of Doppler shift can reveal extremely small changes in radial velocity.
This helps engineers determine:
- spacecraft speed
- trajectory
- orbital changes
- effects of gravitational encounters
Doppler measurements are therefore important far beyond everyday sound.
Motion Sensors
Some motion sensors transmit electromagnetic waves and analyze returning signals.
If an object moves, the reflected signal can experience a Doppler shift.
This principle can be used in:
- automatic doors
- security systems
- occupancy sensors
- traffic monitoring
- industrial automation
Sports Technology
Radar systems can use Doppler shifts to measure the speeds of moving objects such as:
- baseballs
- tennis serves
- golf balls
- vehicles
- other sports equipment
The measurement can be made without attaching a sensor directly to the moving object.
Speed Cameras
Some traffic-speed systems use radar.
A signal is transmitted toward a moving vehicle.
The reflected signal returns with a Doppler shift.
The system uses this frequency difference to determine the vehicle's radial speed.
The underlying sequence is:
transmitted wave → reflection from moving vehicle → frequency shift → speed calculation
Sonic Booms Are Different
The Doppler effect should not be confused with a sonic boom.
As a source approaches the speed of sound, wavefronts become strongly compressed.
If the source moves faster than sound, it produces a shock-wave pattern.
A sonic boom results from these shock waves.
The Doppler effect occurs at ordinary subsonic speeds as well and does not require the source to exceed the speed of sound.
Mach Number
The speed of an object relative to the speed of sound can be described using the Mach number:
Mach number = object speed / speed of sound
For example, if:
v_object = 170 m/s
and:
v_sound = 340 m/s
then:
Mach = 170/340
Mach = 0.50
An object travelling at Mach 1 is travelling approximately at the local speed of sound.
Everyday Examples
Doppler shifts can be observed or applied in:
- ambulance sirens
- train horns
- race cars
- aircraft
- radar
- sonar
- weather monitoring
- ultrasound
- astronomy
- satellite tracking
- speed measurement
The same wave principle connects an enormous range of technologies.
A Complete Sound Problem
A train horn produces:
f_source = 600 Hz
The train approaches a stationary observer at:
v_source = 30 m/s
Take:
v = 340 m/s
Approaching frequency:
f_observed = 600 × 340/(340 − 30)
f_observed = 600 × 340/310
f_observed ≈ 658 Hz
After passing:
f_observed = 600 × 340/(340 + 30)
f_observed = 600 × 340/370
f_observed ≈ 551 Hz
The observer therefore hears a clear decrease in pitch as the train passes.
A Complete Astronomy Problem
A spectral line has a laboratory wavelength of:
λ_rest = 600 nm
A star's spectrum shows the line at:
λ_observed = 599.4 nm
Change:
Δλ = 599.4 − 600
Δλ = −0.6 nm
Because the wavelength decreased, this is a blueshift.
Using the magnitude:
|v_r|/c ≈ 0.6/600
|v_r|/c ≈ 0.001
Therefore:
|v_r| ≈ 0.001(3.0 × 10⁸)
|v_r| ≈ 3.0 × 10⁵ m/s
or:
300 km/s
The negative wavelength shift indicates that the star is approaching.
Choosing the Correct Doppler Relationship
Before calculating, identify the situation.
Ask:
What type of wave is involved?
Sound and electromagnetic waves require somewhat different treatments.
What is moving?
Is it:
- the source
- the observer
- both
- a reflecting target?
Are they approaching or separating?
Approaching should increase observed frequency.
Separating should decrease observed frequency.
Is only radial motion relevant?
Many Doppler technologies measure the velocity component along the line of sight.
Checking these points helps prevent sign errors.
Common Mistakes
Thinking an approaching sound source makes sound travel faster
The speed of sound through the same stationary medium remains approximately unchanged. The wavelength changes.
Confusing frequency with loudness
Frequency affects pitch. Intensity is more closely related to loudness.
Thinking the source's actual emitted frequency changes
The Doppler effect concerns the frequency observed because of relative motion.
Treating a moving source and moving observer as physically identical
A moving sound source changes wavelength in the medium. A moving observer changes how quickly existing wavefronts are encountered.
Assuming all motion produces the same Doppler shift
Only the velocity component along the line of sight directly contributes to the radial Doppler shift.
Thinking redshift means an object actually turns red
Its spectral wavelengths shift toward longer wavelengths.
Thinking blueshift always means blue visible light
It means wavelengths shift toward shorter values.
Treating every astronomical redshift as a simple Doppler shift
Large-scale cosmological redshift involves expansion of space.
Forgetting the factor of 2 in simple reflected-wave Doppler measurements
Radar and Doppler ultrasound can involve a wave travelling to a moving target and then returning.
Key Terms
Doppler effect — change in observed frequency caused by relative motion between a source and an observer.
Doppler shift — difference between observed and emitted frequency.
Observed frequency — frequency measured by an observer.
Source frequency — frequency produced by the wave source.
Radial velocity — component of velocity toward or away from an observer.
Wavefront — surface connecting points of a wave in the same phase.
Redshift — shift of electromagnetic radiation toward longer wavelengths.
Blueshift — shift toward shorter wavelengths.
Spectral line — characteristic wavelength in a spectrum associated with particular atomic or molecular processes.
Radar — system using electromagnetic waves to detect and measure objects.
Doppler radar — radar that uses frequency shifts to determine motion.
Sonar — system using sound waves to detect or investigate objects, commonly underwater.
Doppler ultrasound — medical technique using frequency shifts in reflected ultrasound to investigate motion such as blood flow.
Radial velocity method — astronomical method that detects periodic Doppler shifts in a star's spectrum, often used to identify exoplanets.
Cosmological redshift — increase in wavelength associated with the expansion of the universe.
Mach number — ratio of an object's speed to the local speed of sound.
Key Takeaways
- The Doppler effect is a change in observed frequency caused by relative motion.
- Approaching motion generally produces a higher observed frequency.
- Receding motion generally produces a lower observed frequency.
- For a moving sound source, wavefronts are compressed ahead of the source and spread out behind it.
- A moving sound source changes the wavelength in the medium.
- A moving observer does not change the wavelength already travelling through the medium but encounters wavefronts at a different rate.
- The speed of sound is determined mainly by the medium rather than the speed of the source.
- Doppler shift measures the component of motion along the line of sight.
- Radar uses electromagnetic waves and Doppler shifts to measure motion.
- Sonar can use sound-wave Doppler shifts to investigate underwater motion.
- Doppler weather radar measures motion of precipitation and can help reveal storm movement.
- Doppler ultrasound uses frequency shifts to investigate blood flow.
- Redshift corresponds to increasing wavelength and usually indicates recession in a simple Doppler interpretation.
- Blueshift corresponds to decreasing wavelength and usually indicates approach.
- Astronomers use spectral shifts to measure stellar and galactic motion.
- Periodic Doppler shifts in a star can provide evidence for an orbiting exoplanet.
- Cosmological redshift must be distinguished from a simple local Doppler shift.
- Doppler measurements are used in navigation, satellites, spacecraft, medicine, astronomy, transportation, weather forecasting, and sports.
- Frequency, wavelength, wave speed, and relative motion must be carefully distinguished when analyzing Doppler problems.
- The Doppler effect demonstrates how one fundamental wave principle can be applied across sound, medicine, transportation, astronomy, and modern technology.
Check Your Understanding
- Define the Doppler effect.
- Explain why an approaching ambulance sounds higher in pitch than the same ambulance moving away.
- Describe what happens to the wavelength in front of and behind a moving sound source.
- Explain the difference between the Doppler effect produced by a moving sound source and that produced by a moving observer.
- A siren emits 800 Hz while approaching a stationary observer at 20 m/s. Using a sound speed of 340 m/s, calculate the observed frequency.
- The same 800 Hz siren moves away at 20 m/s. Calculate the observed frequency.
- Explain why the speed of the source should not simply be added to the speed of sound when analyzing an approaching sound source.
- What is radial velocity, and why is it important in radar and astronomical Doppler measurements?
- Explain how Doppler radar can determine the speed of a moving vehicle.
- Compare the use of the Doppler effect in radar and sonar.
- Explain how Doppler ultrasound can be used to determine the direction and speed of blood flow.
- A spectral line normally occurs at 500 nm but is observed at 501 nm. Identify whether this is redshift or blueshift and calculate the approximate radial speed using c = 3.0 × 10⁸ m/s.
- Explain how periodic redshifts and blueshifts in a star's spectrum can provide evidence for an orbiting planet.
- Distinguish between ordinary Doppler redshift and cosmological redshift.
- Choose two applications from astronomy, medicine, navigation, weather monitoring, traffic measurement, or space exploration. Explain how each uses the Doppler effect and identify what information can be obtained from the measured frequency or wavelength shift.