Frequency of tuning fork v(Hz)
Resonance
No. of observations
Position of water level at resonance
Mean length (mean of three observations in column 4c) l (cm)
Water level falling (cm)
Water level rising (cm)
Mean (cm)
512
First
1.
2.
3.
l₁’ = 16.1
Second
1.
2.
3.
l₂’ = 50.3
480
First
1.
2.
3.
l₁’’ = 17.3
Second
1.
2.
3.
l₂’’ = 53.9
( Note. The ideal observations are as samples.)
Sound experiments.
May 13, 2019 English Posts 10,935 Views
The most obvious use for a sound card interfaced with a computer, along with a microphone and speakers, is to explore the physics of sound and the propagation of acoustic waves. The sound card and its use we have already described in the following post: Sound Card Applications . We now want to describe a series of simple experiences of sound waves physics that can be completed with a sound card, open software and a few other “low cost” components.
With a sound card and two microphones it is relatively easy to measure the speed of sound. Recall that the speed of sound is the speed of a sound wave which propagates in an environment, called medium . The speed of sound varies depending on the medium (for example, the sound propagates faster in water than in air), and also varies with the properties of the medium, especially with its temperature.
This is a very important physical property, because it is also the speed of mechanical perturbations in a given substance.
In the air, the sound speed is 331 m/s at 0°C and 343.8 m/s at 20°C (and in linear approximation it varies according to the law a (T) = (331.45 + (0, 62 * T)) m/s with T the temperature measured in °C).
The measure consists in arranging the two microphones separated from each other by a known distance (which we will then vary) and in producing a sound of short duration (for example a snap) in a place in front of the microphones. The arrangement of the microphones is shown in the image below, the “lab jack” on the right is where the sound is produced by dropping a metal ball on the plate.
Obviously the acoustic waves will reach first the microphone 1 and then the microphone 2. Through the sound card and the two connected microphones (one on the left channel and the other on the right channel) and using the audacity software it is possible to acquire and display the two audio tracks, shown in the graphic below. We can see how the instant of arrival of the acoustic wave is temporally displaced for the two microphones. By measuring the time difference and knowing the distance between the two microphones it is possible to calculate the speed of the acoustic wave.
To better evaluate the time difference of arrival of the acoustic wave, samples can be exported and data can be acquired and displayed on Excel . Knowing the sampling frequency ( f = 44.1 KHz, T = 22.67 μs ) it is immediate to find the time difference.
By measuring for different distance values of the two microphones we can more accurately evaluate the speed of the acoustic wave by tracing the regression line, as shown in the graph below. We get the value of 347 m/s , very close to the real value of 344 m/s.
The theory of sound tubes states that inside a tube of length L and diameter D , closed at one end, stationary resonance acoustic waves of frequency fn are formed and the frequency can be determined by the formula :
fn = (2n-1) * v/4L where n = 1,2,3,… v = sound speed
For a tube open at both ends, the formula for determining stationary frequencies is:
fn = n * v/2L where n = 1,2,3,… v = sound speed
To derive these formulas it is sufficient to consider the “boundary conditions” so that a stationary wave can be established inside the tube : for example at the point corresponding to the cap the variation of air displacement is set to zero, while at the point corresponding to the the tube open, the pressure variation is set to zero because the air is at atmospheric pressure. To obtain more precise results, however, it is necessary to take into account the “on-board effects” of the air near the pipe openings: in practice instead of length L the “effective length” must be used, which also takes into account the diameter D :
Lef = L + 0,8*D for an open tube
Lef = L + 0,4*D for a tube open on only one side
After this theoretical premise we briefly describe this simple experiment. A plastic tube about 1m long was used, at one end a microphone connected to the sound card was placed. The air in the tube was placed in “resonance” simply by blowing at the open end. Measurements were made both with the open tube and with the tube closed. The image below shows the experimental setup.
With audacity the audio track is recorded, image below as an example, and from this audio track the frequency spectrum of the sound emission is calculated.
The diagram below shows the aspect of the frequencies that are produced in the case of a tube open at both ends. In the following graph instead is shown the spectrum produced by a tube closed on one side. The peaks corresponding to the various harmonics that extend, with ever smaller amplitude, up to quite high frequencies, are very noticeable.
With our sound card and audacity software we can also easily make a qualitative demonstration of the doppler effect in acoustics. The Doppler effect is a physical phenomenon which consists in the apparent change, with respect to the original value, of the frequency or wavelength perceived by an observer reached by a wave emitted by a source that is in movement with respect to the observer himself . As we all know The Doppler effect can be seen by listening to the difference in the sound emitted by the siren of a rescue vehicle when it approaches and when it moves away, or that in the whistle of a train approaching before and then moving away.
For the theoretical explanation we refer to the numerous texts and websites that describe the phenomenon.
The experiment consists in using a simple buzzer with a battery attached to a rod and rotating this rod in front of the microphone connected to the sound card : in this way the buzzer will alternatively be approaching and moving away from the microphone.
For audio recording we use the audacity spectrogram function: this feature allows you to record and display the trend over time of the sound frequency spectrum, where the intensity is represented by the color. The image below shows the spectrogram of the sound emitted by the buzzer when it is stopped with respect to the microphone. The lines correspond to the various frequencies and we see how these are constant over time.
The following graphs show instead the spectrograms that are obtained when the buzzer is rotated. We see how the frequency of the harmonics, as they are recorded by the microphone, varies cyclically between a maximum and a minimum around the value that one has when stopped. This variation corresponds to the moments in which the buzzer approaches / moves away from the microphone.
The graph below shows the magnified spectrogram of a high frequency harmonic in which the frequency shift of the sound emission is more evident.
Our sound card allows us to easily explore another interesting phenomenon: beats . In music theory, in physics and particularly in acoustics, beat is the frequency resulting from the superposition of periodic quantities, usually sinusoidal oscillations of different and near frequency. It is based on the properties of the superposition principle .
The phenomenon can easily be understood if we consider the mathematical sum of two sinusoidal functions (which represent two overlapping sounds):
The experiment is performed by placing two loudspeakers horizontally on supports, driven by an amplifier and function generator. The microphone connected to the sound card is placed in the intermediate space between the speakers. By varying the frequency of the sound emitted by the two speakers, the audio track is acquired, always with audacity software.
The graph below shows the beat produced by two sounds, in the left part the two sounds have very close frequencies, while in the right part of the graph the frequencies are more distanced and in fact the envelope function has a greater frequency.
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Abstract: in this article, we continue the presentation of the new KC761B device. In the previous post, we described the apparatus in general terms. Now we mainly focus on the gamma spectrometer functionality.
Learning objectives.
By the end of this section, you will be able to:
Sound, like all waves, travels at a certain speed and has the properties of frequency and wavelength. You can observe direct evidence of the speed of sound while watching a fireworks display ( Figure 17.4 ). You see the flash of an explosion well before you hear its sound and possibly feel the pressure wave, implying both that sound travels at a finite speed and that it is much slower than light.
The difference between the speed of light and the speed of sound can also be experienced during an electrical storm. The flash of lighting is often seen before the clap of thunder. You may have heard that if you count the number of seconds between the flash and the sound, you can estimate the distance to the source. Every five seconds converts to about one mile. The velocity of any wave is related to its frequency and wavelength by
where v is the speed of the wave, f is its frequency, and λ λ is its wavelength. Recall from Waves that the wavelength is the length of the wave as measured between sequential identical points. For example, for a surface water wave or sinusoidal wave on a string, the wavelength can be measured between any two convenient sequential points with the same height and slope, such as between two sequential crests or two sequential troughs. Similarly, the wavelength of a sound wave is the distance between sequential identical parts of a wave—for example, between sequential compressions ( Figure 17.5 ). The frequency is the same as that of the source and is the number of waves that pass a point per unit time.
Table 17.1 shows that the speed of sound varies greatly in different media. The speed of sound in a medium depends on how quickly vibrational energy can be transferred through the medium. For this reason, the derivation of the speed of sound in a medium depends on the medium and on the state of the medium. In general, the equation for the speed of a mechanical wave in a medium depends on the square root of the restoring force, or the elastic property , divided by the inertial property ,
Also, sound waves satisfy the wave equation derived in Waves ,
Recall from Waves that the speed of a wave on a string is equal to v = F T μ , v = F T μ , where the restoring force is the tension in the string F T F T and the linear density μ μ is the inertial property. In a fluid, the speed of sound depends on the bulk modulus and the density,
The speed of sound in a solid depends on the Young’s modulus of the medium and the density,
In an ideal gas (see The Kinetic Theory of Gases ), the equation for the speed of sound is
where γ γ is the adiabatic index, R = 8.31 J/mol · K R = 8.31 J/mol · K is the gas constant, T K T K is the absolute temperature in kelvins, and M is the molar mass. In general, the more rigid (or less compressible) the medium, the faster the speed of sound. This observation is analogous to the fact that the frequency of simple harmonic motion is directly proportional to the stiffness of the oscillating object as measured by k , the spring constant. The greater the density of a medium, the slower the speed of sound. This observation is analogous to the fact that the frequency of a simple harmonic motion is inversely proportional to m , the mass of the oscillating object. The speed of sound in air is low, because air is easily compressible. Because liquids and solids are relatively rigid and very difficult to compress, the speed of sound in such media is generally greater than in gases.
Medium | (m/s) |
---|---|
Air | 331 |
Carbon dioxide | 259 |
Oxygen | 316 |
Helium | 965 |
Hydrogen | 1290 |
Ethanol | 1160 |
Mercury | 1450 |
Water, fresh | 1480 |
Sea Water | 1540 |
Human tissue | 1540 |
Vulcanized rubber | 54 |
Polyethylene | 920 |
Marble | 3810 |
Glass, Pyrex | 5640 |
Lead | 1960 |
Aluminum | 5120 |
Steel | 5960 |
Because the speed of sound depends on the density of the material, and the density depends on the temperature, there is a relationship between the temperature in a given medium and the speed of sound in the medium. For air at sea level, the speed of sound is given by
where the temperature in the first equation (denoted as T C T C ) is in degrees Celsius and the temperature in the second equation (denoted as T K T K ) is in kelvins. The speed of sound in gases is related to the average speed of particles in the gas, v rms = 3 k B T m , v rms = 3 k B T m , where k B k B is the Boltzmann constant ( 1.38 × 10 −23 J/K ) ( 1.38 × 10 −23 J/K ) and m is the mass of each (identical) particle in the gas. Note that v refers to the speed of the coherent propagation of a disturbance (the wave), whereas v rms v rms describes the speeds of particles in random directions. Thus, it is reasonable that the speed of sound in air and other gases should depend on the square root of temperature. While not negligible, this is not a strong dependence. At 0 °C 0 °C , the speed of sound is 331 m/s, whereas at 20.0 °C 20.0 °C , it is 343 m/s, less than a 4 % 4 % increase. Figure 17.6 shows how a bat uses the speed of sound to sense distances.
As stated earlier, the speed of sound in a medium depends on the medium and the state of the medium. The derivation of the equation for the speed of sound in air starts with the mass flow rate and continuity equation discussed in Fluid Mechanics .
Consider fluid flow through a pipe with cross-sectional area A ( Figure 17.7 ). The mass in a small volume of length x of the pipe is equal to the density times the volume, or m = ρ V = ρ A x . m = ρ V = ρ A x . The mass flow rate is
The continuity equation from Fluid Mechanics states that the mass flow rate into a volume has to equal the mass flow rate out of the volume, ρ in A in v in = ρ out A out v out . ρ in A in v in = ρ out A out v out .
Now consider a sound wave moving through a parcel of air. A parcel of air is a small volume of air with imaginary boundaries ( Figure 17.8 ). The density, temperature, and velocity on one side of the volume of the fluid are given as ρ , T , v , ρ , T , v , and on the other side are ρ + d ρ , T + d T , v + d v . ρ + d ρ , T + d T , v + d v .
The continuity equation states that the mass flow rate entering the volume is equal to the mass flow rate leaving the volume, so
This equation can be simplified, noting that the area cancels and considering that the multiplication of two infinitesimals is approximately equal to zero: d ρ ( d v ) ≈ 0 , d ρ ( d v ) ≈ 0 ,
The net force on the volume of fluid ( Figure 17.9 ) equals the sum of the forces on the left face and the right face:
The acceleration is the force divided by the mass and the mass is equal to the density times the volume, m = ρ V = ρ d x d y d z . m = ρ V = ρ d x d y d z . We have
From the continuity equation ρ d v = − v d ρ ρ d v = − v d ρ , we obtain
Consider a sound wave moving through air. During the process of compression and expansion of the gas, no heat is added or removed from the system. A process where heat is not added or removed from the system is known as an adiabatic system. Adiabatic processes are covered in detail in The First Law of Thermodynamics , but for now it is sufficient to say that for an adiabatic process, p V γ = constant, p V γ = constant, where p is the pressure, V is the volume, and gamma ( γ ) ( γ ) is a constant that depends on the gas. For air, γ = 1.40 γ = 1.40 . The density equals the number of moles times the molar mass divided by the volume, so the volume is equal to V = n M ρ . V = n M ρ . The number of moles and the molar mass are constant and can be absorbed into the constant p ( 1 ρ ) γ = constant . p ( 1 ρ ) γ = constant . Taking the natural logarithm of both sides yields ln p − γ ln ρ = constant . ln p − γ ln ρ = constant . Differentiating with respect to the density, the equation becomes
If the air can be considered an ideal gas, we can use the ideal gas law:
Here M is the molar mass of air:
Since the speed of sound is equal to v = d p d ρ v = d p d ρ , the speed is equal to
Note that the velocity is faster at higher temperatures and slower for heavier gases. For air, γ = 1.4 , γ = 1.4 , M = 0.02897 kg mol , M = 0.02897 kg mol , and R = 8.31 J mol · K . R = 8.31 J mol · K . If the temperature is T C = 20 ° C ( T = 293 K ) , T C = 20 ° C ( T = 293 K ) , the speed of sound is v = 343 m/s . v = 343 m/s .
The equation for the speed of sound in air v = γ R T M v = γ R T M can be simplified to give the equation for the speed of sound in air as a function of absolute temperature:
One of the more important properties of sound is that its speed is nearly independent of the frequency. This independence is certainly true in open air for sounds in the audible range. If this independence were not true, you would certainly notice it for music played by a marching band in a football stadium, for example. Suppose that high-frequency sounds traveled faster—then the farther you were from the band, the more the sound from the low-pitch instruments would lag that from the high-pitch ones. But the music from all instruments arrives in cadence independent of distance, so all frequencies must travel at nearly the same speed. Recall that
In a given medium under fixed conditions, v is constant, so there is a relationship between f and λ ; λ ; the higher the frequency, the smaller the wavelength ( Figure 17.10 ).
Calculating wavelengths.
The speed of sound can change when sound travels from one medium to another, but the frequency usually remains the same. This is similar to the frequency of a wave on a string being equal to the frequency of the force oscillating the string. If v changes and f remains the same, then the wavelength λ λ must change. That is, because v = f λ v = f λ , the higher the speed of a sound, the greater its wavelength for a given frequency.
Imagine you observe two firework shells explode. You hear the explosion of one as soon as you see it. However, you see the other shell for several milliseconds before you hear the explosion. Explain why this is so.
Although sound waves in a fluid are longitudinal, sound waves in a solid travel both as longitudinal waves and transverse waves. Seismic waves , which are essentially sound waves in Earth’s crust produced by earthquakes, are an interesting example of how the speed of sound depends on the rigidity of the medium. Earthquakes produce both longitudinal and transverse waves, and these travel at different speeds. The bulk modulus of granite is greater than its shear modulus. For that reason, the speed of longitudinal or pressure waves (P-waves) in earthquakes in granite is significantly higher than the speed of transverse or shear waves (S-waves). Both types of earthquake waves travel slower in less rigid material, such as sediments. P-waves have speeds of 4 to 7 km/s, and S-waves range in speed from 2 to 5 km/s, both being faster in more rigid material. The P-wave gets progressively farther ahead of the S-wave as they travel through Earth’s crust. The time between the P- and S-waves is routinely used to determine the distance to their source, the epicenter of the earthquake. Because S-waves do not pass through the liquid core, two shadow regions are produced ( Figure 17.11 ).
Seismologists and geophysicists use properties and velocities of earthquake waves to study the Earth's interior, which due to it's depth and pressure is not observable through many other means. In fact, the discoveries of the structure of the Earth, illustrated in the figure above, resulted from earthquake observations. In 1914, Beno Gutenberg used differences in wave speeds to determine that there must be a liquid core within the mantle. In 1936, Inge Lehmann began investigating P-waves from a New Zealand earthquake that had unexpectedly reached Europe, which should have been in the shadow region. Up until that point, seismologists had explained such shadow waves as being caused by some type of diffraction (as Gutenberg himself assumed) or a result of faulty seismometers. However, Lehmann had installed the European instruments herself, and so trusted their accuracy. She calculated that the amplitude of the waves must be caused by the existence of a solid inner core within the liquid core. This model has been accepted and reinforced by decades of subsequent calculations, including those from nuclear test explosions, which can be measured very precisely.
As sound waves move away from a speaker, or away from the epicenter of an earthquake, their power per unit area decreases. This is why the sound is very loud near a speaker and becomes less loud as you move away from the speaker. This also explains why there can be an extreme amount of damage at the epicenter of an earthquake but only tremors are felt in areas far from the epicenter. The power per unit area is known as the intensity, and in the next section, we will discuss how the intensity depends on the distance from the source.
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Speed of sound.
Experiment #28 from Physics Explorations and Projects
The goal of this activity is for students to devise an experiment that allows them to determine the speed of sound through air.
In the Preliminary Observations, students will observe sound waves that are “delayed” in their arrival, such as seeing a gun flash before hearing it. Students will then estimate how fast sound waves travel through air and devise a method for measuring it. Since groups may choose different methods, you will need to have a class discussion after the investigations to summarize the class’s findings.
This experiment features the following sensors and equipment. Additional equipment may be required.
Ask an expert.
Get answers to your questions about how to teach this experiment with our support team.
This experiment is #28 of Physics Explorations and Projects . The experiment in the book includes student instructions as well as instructor information for set up, helpful hints, and sample graphs and data.
IMAGES
VIDEO
COMMENTS
7. Calculate avg. 8. Calculate the speed of sound using avg for this tuning fork. 9. Repeat the above procedure for the other tuning fork. 10. Calculate an average value for the speed of sound. 11. Calculate a theoretical value for the speed of sound using: v = (331.50+0.61T)m/s (Eq. 7-3) where T is the temperature in degrees Celsius.
Measurement of the speed of sound propagation in air inside a {large} room is an approximation to this ideal situation. This experimental setup is shown in the pix below. The apparatus consists of using a narrow voltage pulse output from an Agilent 3320A Function Generator to excite a piezo-electric horn mounted at the LHS end of an optical ...
Past Papers. Edexcel. Religious Studies. Past Papers. OCR. Religious Studies. Past Papers. Revision notes on 4.9.10 Determining the Speed of Sound in Air in a Resonance Tube for the OCR A Level Physics syllabus, written by the Physics experts at Save My Exams.
A sound wave is a mechanical vibration that propagates through a medium, such as air or a liquid. The speed of sound is the speed at which this wave propagates in this m edium, it depends on the temperature, the pressure and the density of the medium through which it propagates. In air, if we assimilate it to a perfect diatomic gas, we can calculate the speed of sound by the equation: c = sqrt ...
1. Measure the length of the resonance tube. Record the length on the datasheet. 2. With the speaker placed a few centimeters from one end of the tube, as shown in Fig. 1 Connect the speaker to the "Low Ω" outputs of the frequency generator, as shown in Fig. 2 and connect the "High Ω" outputs to "CH1" of the oscilloscope.
A variable piston adjusts the length of a resonance air column, which is a glass tube. The two subsequent resonances seen at room temperature are at 20 cm and 85 cm in column length. Calculate the sound velocity in the air at room temperature if the length's frequency is 256 Hz.
of the sound wave. In this experiment, you will be using different frequencies produced by a frequency generator interface to determine the velocity of sound in air. Since the frequencies used will be known, to calculate the velocity of sound you need to find the wavelength corresponding to that sound. By
EXPERIMENT 11 Velocity of Waves 2. Purpose To determine the speed of sound in air, and to find the relationship between the velocity of a wave in a string, the linear density, and the tension. You will do this by performing two different experiments: Part 1: Speed of Sound in Air IPart 2: Sonometer- Waves in a Stretched String
the speed of sound in air. Preliminaries. This experiment investigates the resonance conditions of a simple system consisting of a column of air closed at one end and driven at the other by an external speaker. Figure 1. Schematic for Standing Sound Waves Experiment . Any vibrating object that can compress and rarify a gas can produce traveling ...
temperature. The speed of sound is not a constant value! To calculate today's speed of sound, v,wewilldeter-mine the wavelength, (lambda), of the sound pro-duced by a tuning fork of known frequency, f: v = f (12.1) A vibrating tuning fork generates a sound wave that travels outward in all directions. When held above a sound tube, a portion of ...
Measurement of Sound Speed in Air. With a sound card and two microphones it is relatively easy to measure the speed of sound. Recall that the speed of sound is the speed of a sound wave which propagates in an environment, called medium. The speed of sound varies depending on the medium (for example, the sound propagates faster in water than in ...
Sound 8.1 Purpose In this experiment we will be using resonance points of a sound wave traveling through an open tube to measure the speed of sound in air. In order to understand how this can be done, we must discuss some properties of wave motion. 8.2 Introduction The type of waves that we will be concerned with in this experiment are what are ...
Speed of Sound in Various Media. Table 17.1 shows that the speed of sound varies greatly in different media. The speed of sound in a medium depends on how quickly vibrational energy can be transferred through the medium. For this reason, the derivation of the speed of sound in a medium depends on the medium and on the state of the medium.
9. Calculate the average speed of sound for a given frequency using the speeds of sound calculated in the previous step. Also determine the standard deviations. Finally, compare the average speeds of sound from part B to the speed of sound determined in part A of the experiment. Data
The goal of this activity is for students to devise an experiment that allows them to determine the speed of sound through air. In the Preliminary Observations, students will observe sound waves that are "delayed" in their arrival, such as seeing a gun flash before hearing it. Students will then estimate how fast sound waves travel through air and devise a method for measuring it. Since groups ...
Strike the tuning fork with the rubber hammer and hold above the top of the tube. 5. Adjust the height of the tube until the sound is loudest. Hold the tube still and measure and record the distance from the water to the top of the tube. 6. Hold a thermometer in the middle of the tube and record the air temperature. Part B. 1.
Measure the speed of sound in air using a tube that is closed at one end. Use a Sound Sensor to record the initial pulse of sound and its echo. ... Calculate the speed of sound based on the overall distance traveled and the round-trip time. Providing educators worldwide with innovative solutions for teaching science. ... Toll Free: 1-800-772 ...
Speed of Sound in Physics. This entry was posted on June 17, 2023 by Anne Helmenstine (updated on June 22, 2023) The speed of sound in dry air at room temperature is 343 m/s or 1125 ft/s. In physics, the speed of sound is the distance traveled per unit of time by a sound wave through a medium. It is highest for stiff solids and lowest for gases.
Students will first predict the speed of sound in the air of their classroom using a simple relationship accounting for temperature. Students will measure the time it takes a short pulse of sound to travel the length of a tube, reflect off the closed end, and return. Using this measurement, they will calculate the speed of sound and compare it to their prediction.
In this experiment, we are going to use a tuning forkfor other experiments such as measuring the resistivity of a wire https://www.youtube.com/watch?v=sGhGR...
The first method is based on simply measuring the time it takes a pulse of light or sound to traverse a known distance; dividing the distance by the transit time then gives the speed. The second ...
Learn how to use a starting pistol, a stopwatch and a trundle wheel to estimate the speed of sound in air. The web page explains the method, the assumptions and the formula involved in this simple experiment.