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Project Summary

Difficulty  7 
Time required Very Short (a day or less)
Prerequisites To do this project, you'll need a piano which is in tune. You'll also need to know enough about the piano to find notes by their letter names.
Material Availability Readily available
Cost Very Low (under $20)
Safety No issues


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Abstract

The renowned pianist Vladimir Horowitz once said, "The most important thing is to transform the piano from a percussive instrument into a singing instrument." Check out this project to learn about sympathetic vibrations, one way to make piano strings sing.

Objective

The goal of this project is to understand which notes can induce sympathetic vibrations on an "open" string on the piano.

Introduction

How can you make a piano string sing? What are sympathetic vibrations? This project will show you what and how. You'll need a quiet room with a piano, and some knowledge of sound waves and how they are produced.

This is a fairly simple project that explores the science of musical sounds. What exactly do we mean by musical sounds? It will help if we think about it step-by-step. First, we need to understand the basics of sound: how it is produced and how it is perceived. Then we can consider what makes a sound musical.

You'll also need to understand some basic properties of waves to get the most out of this project. We'll provide a quick introduction here, but for a more complete understanding we recommend some background research on your own. The Bibliography section, below, has some good starting points for researching this project.

What is sound? Sound is a wave, a pattern—simple or complex, depending on the sound—of changing air pressure. Sound is produced by vibrations of objects. The vibrations push and pull on air molecules. The pushes cause a local compression of the air (increase in pressure), and the pulls cause a local rarefaction of the air (decrease in pressure). Since the air molecules are already in constant motion, the compressions and rarefactions starting at the original source are rapidly transmitted through the air as an expanding wave. When you throw a stone into a still pond, you see a pattern of waves rippling out in circles on the surface of the water, centered about the place where the stone went in. Sound waves travel through the air in a similar manner, but in all three dimensions. If you could see them, the pattern of sound waves from the stone hitting the water would resemble an expanding hemisphere. The sound waves from the stone also travel much faster than the rippling water waves from the stone (you hear the sound long before the ripples reach you). The exact speed depends on the number of air molecules and their intrinsic (existing) motion, which are reflected in the air pressure and temperature. At sea level (one atmosphere of pressure) and room temperature (20°C), the speed of sound is about 344 m/s.

Perception of a sound begins when sound pressure waves reach the tympanic membrane (eardrum), a thin, flexible membrane in the middle ear. The pressure waves cause the tympanic membrane to vibrate. The vibrations are amplified by a series of three tiny bones and transmitted to the cochlea. Curled up inside the fluid-filled, snail-shaped cochlea is the organ of Corti, where the vibrations are transduced into nerve impulses by cells called hair cells. Moving along the length of the organ of Corti, each region is sensitive to vibrations of decreasing frequency (i.e., higher pitch). The nerve impulses from the hair cells are conducted to the brain, where they are further processed, leading ultimately to the perception of sound. (Chudler, 2006; Kelly, J.P., 1991)

You've seen that one way to describe a wave is by its speed. In addition to speed, we will also find it useful to describe waves by their frequency, period, and wavelength. Let's start with frequency (f). The top part of Figure 1, below, represents the compressions (darker areas) and rarefactions (lighter areas) of a pure-tone (i.e., single frequency) sound wave traveling in air (Henderson, 2004). If we were to measure the changes in pressure with a detector, and graph the results, we could see how the pressure changes over time, as shown in the bottom part of Figure 1. The peaks in the graph correspond to the compressions (increase in pressure) and the troughs in the graph correspond to the rarefactions (decrease in pressure).

Illustration of a sound wave as compression and rarefaction of air, and as a graph of pressure vs. time.
Figure 1. Illustration of a sound wave as compression and rarefaction of air, and as a graph of pressure vs. time (Henderson, 2004).

Notice how the pressure rises and falls in a regular cycle. The frequency of a wave describes how many cycles of the wave occur per unit time. Frequency is measured in Hertz (Hz), which is the number of cycles per second. Figure 2, below, shows examples of sound waves of two different frequencies (Henderson, 2004).

Graphs of high and low frequency waves.
Figure 2. Graphs of high (top) and low (bottom) frequency waves (Henderson, 2004).

Figure 2 also shows the period (T) of the wave, which is the time that elapses during a single cycle of the wave. The period is simply the reciprocal of the frequency (T = 1/f). For a sound wave, the frequency corresponds to the perception of the pitch of the sound. The higher the frequency, the higher the perceived pitch. On average, the frequency range for human hearing is from 20 Hz at the low end to 20,000 Hz at the high end.

The wavelength is the distance (in space) between corresponding points on a single cycle of a wave (e.g., the distance from one compression maximum (crest) to the next). The wavelength (λ), frequency (f), and speed (v) of a wave are related by a simple equation: v = fλ. So if we know any two of these variables (wavelength, frequency, speed), we can calculate the third.

Now it is time to take a look at how sound waves are produced by a musical instrument. For a scientist, it is always a good idea to know as much as you can about your experimental apparatus! Figure 3, below, is a top-down view of an open grand piano.

Top view of an open grand piano.
Figure 3. Top view of an open grand piano.

The piano has many tightly-stretched strings which are struck by felt-covered, wooden hammers when a piano key is pressed (more on this later). The diagonal layout of the bass strings provides for maximum length. The strings are stretched over a bridge (above the sinuous green line in the diagram), which transmits their vibrations to the soundboard. The soundboard, with its large area, amplifies the sound of the strings. (One way to see this for yourself is with the mechanism from a music box. First try playing it while holding it in the air. Then, place it in contact with a wood surface, like solid wood table top, and play it again. The music box mechanism causes the table to vibrate. The table has a much larger surface area in contact with the air. The sound is greatly amplified by the wood.) The cast iron frame of the piano bears the load of the strings, whose combined tension can total 20 tons.

The mechanism that transmits the force of the pianists fingers on the keys to the hammers that strike the strings is called the action. It is a complicated mechanism (see the Bibliography for references that show how the action works in detail) but, basically, here's how it works. A piano key is a long lever. Inside the piano, when you press on a key, the other end of the lever initiates two actions: 1) a damper (small felt pad that silences the string) is lifted from the string and 2) the hammer is set in motion. The hammer is not directly connected to the key, so at a certain point, it is carried forward by its own momentum, and bounces off of the string. This way, the hammer does not remain in contact with the string, which would act to dampen the vibration and silence the string. As long as you hold the key down, the damper is remains raised and the string can continue to vibrate. When you let go of the key, the damper re-contacts the string and silences it. A final detail: although the description above refers to a singular "string," only the lowest piano notes are played by single strings. In the treble range, there are three strings for each note (the hammer hits all three at once), and in the lower midrange, there are two strings for each note. We will continue to refer to a single string, but keep in mind that, for most of the piano's notes, there is more than one string.

The string vibrates between two fixed points: where it is stretched over the bridge and the opposite end of the string, where it is attached to the frame. The vibration results in a standing wave on the string. The fixed points of the string don't move (nodes), while other points on the string oscillate back and forth maximally (antinodes). Figure 5, below, shows some of the standing wave patterns that can occur on a vibrating string (Nave, 2006a).

Standing waves on a vibrating string.
Figure 4. Standing waves on a vibrating string, showing the fundamental (top), first harmonic (middle), and second harmonic (bottom) vibrational modes. (Nave, 2006a)

The string can vibrate at several different natural modes (harmonics). Each of these vibrational modes has nodes at the fixed ends of the string. The fundamental mode (Figure 5, top) has a single antinode halfway along the string. Thus, the wavelength of the fundamental vibration is twice the length (L) of the string. The second harmonic has a node halfway along the string. Thus, the wavelength of the second harmonic is equal to the length of the string. Remember that the relationship between wavelength and frequency depends on the speed of the wave. We can rewrite the equation presented earlier as f = v/λ. If we take the ratio between the frequency, f2, of the second harmonic and the frequency, f1, of the first harmonic, the velocity term cancels out:

f2
f1
 =   v/L 
v/2L
 =   1 
1/2
 =  2

You can continue the calculations for the higher harmonics yourself. What is the frequency of the third harmonic, relative to the fundamental?

At last, you have enough of an introduction to sound waves and pianos so that you can understand how one string can make another "sing." Playing a key to strike the string with the hammer is one way to start the string vibrating, but the strings can also be set in motion by sound. If you lift up the damper on a string (if you press the key very slowly and gently, you can do this without sounding the string with the hammer), you leave the string "open" to vibrate. If you then play and release another note, e.g., one octave higher, you will hear the open string sound. It sings!

How does this work? The fundamental vibration of the string for the note one octave higher is at the same frequency as the second harmonic of the open string. The vibration of the higher string, transmitted through the air and (via the soundboard) through the bridge, sets excites this vibrational mode of the open string. This phenomenon is called sympathetic vibration. Besides octaves, what other intervals can excite an open string? The Experimental Procedure section, below, shows you how to find out.

Terms, Concepts and Questions to Start Background Research

To do this project, you should do research that enables you to understand the following terms and concepts:

Bibliography

Materials and Equipment

To do this experiment you will need the following materials and equipment:

Experimental Procedure

  1. Start by holding the C2 (two octaves below middle C) string open. Depress the key very slowly so that the damper is lifted up, but the hammer does not cause the string to vibrate. There should be no sound. If you do hear sound, let go of the key, wait a second or two (the damper will contact the string and silence it), and try again.
  2. While still holding C2 open, firmly play and quickly release C3 (one octave below middle C). If you're familiar with music terminology, you want to play a forte stacatto note. If you're familiar with physics terminology, you are trying to produce an impulse response with the hammer on the C3 string.
  3. The tone from the C3 string will die away quickly when the damper re-contacts the string after you let go of the key. However, since you are holding the C2 string open, you should still hear a sound. If you let go of the C2 key, the sound should die away quickly as the damper re-contacts the C2 string. Let go of the C2 key and prove to yourself that it is the source of the continued sound.
  4. Next you will time the duration of the sympathetic vibration induced in the open C2 string by each of the notes between C3 and C4, inclusive (the test notes). Make a data table in your lab notebook, with at least three spaces for each of the thirteen notes.
  5. Start by holding the C2 (two octaves below middle C) string open. Depress the key very slowly so that the damper is lifted up, but the hammer does not cause the string to vibrate. There should be no sound. If you do hear sound, let go of the key, wait a second or two (the damper will contact the string and silence it), and try again.
  6. Have your helper count down (3-2-1-go!) and start the stopwatch on "Go!" At the same moment, firmly play and release the note you are testing. Try to use the same motion (same amount of force, same acceleration) for each test note you play.
  7. Listen carefully to the sound of the C2 string, and at the first moment you can no longer hear it, say "Stop!" Your helper should immediately stop the stopwatch. Write down the duration in your data table.
  8. Repeat the duration measurement at least three times for each test key. Depending on how consistent you are in striking the test note, you may need more trials to get consistent results.
  9. Average the duration results for each test note.
  10. Graph your results (a bar graph aligned with a graphic of the piano keys corresponding to the test notes would be one idea). The duration of the sound on the C2 string is a measure of the strength of the vibrational excitation from the test note. Which test notes excite C2 most strongly? Do you see any patterns in the duration data?
  11. Figure 5, below, shows the fundamental frequencies for each of the piano strings. Compute harmonics 1–6 for C2. How do these compare to the fundamental frequencies of the test notes? To their harmonics? Which modes of C2 are excited by which test notes?
  12. Make calculations for the octave between C2 and C3 (or between C4 and C5). Predict which test notes will produce the longest-duration symapathetic vibrations. Repeat your test with the new test octave and test your hypothesis. What did you learn?

Fundamental frequencies of the 88 notes on the piano keyboard.
Figure 5. Fundamental frequencies of the 88 notes on the piano (Irvine, 2000).

Variations

Credits

Andrew Olson, Ph.D., Science Buddies

Sources


Last edit date: 2006-04-20 00:20:02


Career Focus

If you like this project, you might enjoy exploring careers in Music.

Sound Engineering Technician
Any time you hear music at a concert, a live speech, the police sirens in a TV show, or the six o'clock news you're hearing the work of a sound engineering technician. Sound engineering technicians operate machines and equipment to record, synchronize, mix, or reproduce music, voices, or sound effects in recording studios, sporting arenas, theater productions, or movie and video productions.
 



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