Lecture #1.2 Superposition and Interference of Mechanical Waves 1. Mechanical Waves (Review of the last lecture from the previous semester) At the end of the last semester we have discussed mechanical waves. Here are the main results of our discussion. In contrast to simple harmonic motion, where position velocity and acceleration are changing as periodic functions of time, but both position and energy of the oscillating object remain in the same local region of space without traveling anywhere, waves give us an example of how motion of energy (or information) can be conducted through the space without actual motion of matter. We have limited out attention to mechanical waves. This is the most familiar for everyday life type of waves, because we are actually using them almost every day in the form of sound. We can see them as waves on the water surface and even sometimes can feel them as seismic waves. All these waves are governed by Newton's laws and they can only exist in material medium, such as gas, liquid or solid. A simple one-dimensional example of the mechanical wave is the wave sent along the stretched taut string. This becomes possible because the string is under tension. So, if the string is pulled up and down at one end, it begins to pull up and down the adjacent section of the string and then the next section and so on. As a result the pulse will travel along the string with some velocity v . If a person who pulls the string will continue to do that on periodic basis the continuous wave will travel along this string. If the external force causing this motion has the form of a simple harmonic motion, then this wave will have the shape of sinusoidal function and will be called harmonic wave. If we consider the motion of some element of this string we will see that it moves up and down in the direction perpendicular to the direction of propagation of the wave. This is why we called that type of wave transverse wave. Alternatively we can consider a wave produced by a piston in a long air-filled pipe. In a same way as the person was pulling on the string, he/she can move the piston rightward and leftward. This motion of the piston can be a simple harmonic motion. At first it will cause the increase of air pressure right next to the piston then this pressure increase will move to the next section of the pipe and so on. When the piston moves back, the pressure will decrease, this decrease will also travel along the pipe. As a result we have a sound wave in this pipe. However, this wave is different from the one we considered before, because now different elements of air in the pipe are moving in the same direction as the direction of wave’s travel. We shall call such a wave to be longitudinal wave. Both transverse wave and longitudinal wave are said to be traveling waves, because they both travel from one point in space to another point in space. It is the wave that moves but not the material. In both cases elements of the string or elements of the air in the pipe do not travel anywhere. They just oscillate near the same positions. If we consider a transverse wave in the string, this is an example of the plane wave, which propagates in the direction perpendicular to the plane surface. We called this direction to be x-direction. Since it is transverse wave, the elements of the string are moving in the direction perpendicular to the x-direction. We called that direction to be ydirection. This means that positions of the elements of the string changes with time and it will be different for different values of x. To describe this wave we need to know the b g function y y x, t for the displacement of the elements in the string. We only considered sinusoidal waves, behaving according to y x, t A sin kx t . (1.2.1) In this equation A is called the wave amplitude, k is called the wave number and is wave angular frequency. The wave described by equation 1.2.1 is moving in positive x direction. The phase of the wave is the argument of the sin-function kx t . If we fix x in this argument, we can watch how the position of the string changes at certain location in space. According to equation 1.2.1 it oscillates in a simple harmonic motion. If we fix time t, we can see the snapshot of this wave in space. It will look like a sin-function, which changes along x direction. It is periodic function which will reproduce its shape along axis x. The smallest distance between repetitions of the wave shape along axis x is called a wavelength . We have shown that the wave number k and the wavelength are related according to k 2 . (1.2.2) We have also shown that the time period of the simple harmonic wave is related to its angular frequency according to 2 . T (1.2.3) If the wave pattern moves in space for distance x during time t , so we can talk about wave’s speed x t . This speed is also known as a phase speed, because the wave's phase remains constant, as the wave moves in positive x direction. We have shown that the wave’s speed is v k T f . (1.2.4) This means that the wave moves for the distance of one wavelength during the time interval equal to the wave's period. We have also shown that the speed of the wave in the string depends on elastic properties of the string (tension force F) and linear mass density of the string ( is mass per unit of length) as v F . (1.2.5) The other common example of mechanical wave is the sound wave. The sound wave from the point like source in air is longitudinal spherical wave. When we discussed kinematics, we introduced the idea of the point-like or particle-like object. The size of this object is much smaller compared to the distance of its travel. Using the same idea, we can introduce the point-like source of sound. This is different compared to situation of the string, where transverse wave was going in one direction of x-axis only. In the case of the string a wavefront, the surface where oscillations of matter have the same phase is a planar surface. In the case of the sound wave propagating in all directions along so called rays in the air, the wavefronts are spherical. Those wavefronts are perpendicular to the rays, showing the direction of the wave’s propagation. In the case of the longitudinal wave the oscillations of air are also taking place in the direction of those rays perpendicular to wavefronts, while for transverse wave they take place in the direction of the wavefront perpendicular to the rays. If, however, we consider a spherical wave at very large distance from the source, the wavefront's curvature is almost negligible and we can treat it as a planar wave. In the case of the sound wave moving in 3-dimensional medium, the elastic properties of the medium are related to periodic compressions and expansions of its small volume elements. The so-called bulk modules B p V V (1.2.6) is responsible for these changes. In this equation p is the change of pressure (force acting per unit of area) and V V is the fractional change of volume. The equation for speed of sound is then v B , (1.2.7) where is the density of the medium. The speed of sound, as we can see from equation 1.2.7 depends on a substance, since different substances have different densities as well as on temperature, since density also depends on temperature. In the air under the normal atmospheric pressure and temperature, the speed of sound is v 343 m s 770 mi h . Table 16.1 in the book shows values of speed of sound for some other substances at different conditions. If we consider a traveling sound wave in the tube filled by air, this wave appears due to the motion of the piston at the end of the tube from the left to the right and backward in the sinusoidal pattern. This motion causes the air elements at the end closer to the piston change their density according to the same sinusoidal law as a result of compression and then those changes of density will travel along the tube. Each element of air with thickness x in the tube will oscillate according to the same sinusoidal law as the piston does. In the longitudinal wave, those oscillations take place in the same direction x as this wave propagates. To avoid confusions we used letter s to show this displacement. If this wave has a form of the cos-function then s x, t A cos kx t , (1.2.8) where A is the amplitude. All other characteristics of the wave, such as k , , f , , T are defined in a same way as they were in the case of transverse wave. Another important characteristic of sound is its intensity, which actually shows how strong the sound is at a particular point in space. Intensity of sound I at certain surface is the average power per unit area transferred by this wave trough or onto the surface I P . A (1.2.9) If we consider a point-like source of sound, which emits sound waves isotropically (with equal intensity in all directions) and if the sound wave's energy is conserved, so it is not dissipated in space, then we can write that I Ps . 4r 2 (1.2.10) Here Ps is the power of the source and r is the distance from the source. As you can see, the sound intensity gets smaller with distance, not even because of the reflections and scattering from different objects, but because the same energy spreads over larger and larger areas of the spheres 4r 2 surrounding this point-like source. We have also introduced the intensity level or sound level, which was defined as b g 10dB log I . I0 (1.2.11) Here dB is abbreviation for decibel, the unit of sound level, I 0 1012 W m2 stands for the standard reference intensity, chosen because it is near the low limit of the human range of hearing. This standard reference level corresponds to zero decibels. 2. Superposition of Waves Now we will consider a case, when there are several waves coming to the same point in space from different sources. This could be the case of the sound waves coming from different objects or the waves on the surface of water coming from different disturbances. Since we were discussing transverse waves in the string, let us continue with this example and consider two waves traveling along the string simultaneously. In this case the net displacement of the string's element will be an algebraic sum of the two displacements due to each of the waves b g b g b g y x, t y1 x, t y2 x, t . (1.2.12) This is known as the principle of superposition of mechanical waves. The overlapping waves do not in any way alter each other. The net wave depends on the extent to which the waves are in phase. If these two waves are exactly in phase, the net wave is just a doubled wave. However, the case, when there is a finite phase difference between the waves, is different. We have y1 x, t A sin kx t and y2 x, t A sin kx t These two waves have the same frequency and the same wave number. They both travel in the positive x direction and have the same amplitude. They are only different by the phase constant . In this case the net wave is going to be y x, t y1 x, t y2 x, t A sin kx t A sin kx t 2 A cos sin kx t 2 2 So, the resultant wave is again a sinusoidal wave traveling in the same positive x direction. However, this wave has different phase constant 2 and different amplitude 2 A cos . In the case if the phase difference between the two original waves is zero the 2 amplitude of the resultant wave achieves its maximum possible value 2A, which is called fully constructive interference. If the original phase difference was equal then the amplitude of the resultant wave is zero and it is a case of fully destructive interference, like no wave goes along the string at all. In all other cases we have intermediate interference. Now let us consider the case, when the two waves are traveling along the string in the opposite directions. Let these waves be of the same angular frequency and the same wave number. In that situation there are places on the string called nodes, where the string never moves. Half way between the adjacent nodes there are antinodes, where the amplitude of the resultant wave has its maximum. The pattern like this is called a standing wave, because this wave does not move in space, but just oscillate with time. Let us analyze this standing wave combined from y1 x, t A sin kx t and y2 x, t A sin kx t , which gives y x, t y1 x, t y2 x, t A sin kx t A sin kx t 2 A sin kx cos t This equation does not describe a traveling wave. Instead it describes a standing wave. The absolute value of the first term in this equation 2 A sin kx gives the amplitude of oscillations at point x. As you can see this amplitude varies with position. At nodes it is equal zero b g sin kx 0, kx n, n 0,1... n x n . k 2 The last equation shows positions of the nodes along the x-axis. They are separated by distances equal to the half of wavelength. The position of antinodes, where the amplitude has its maximum, can be found from the condition b g F 1I kx G n J , n 0,1... H 2K F 1I F 1I x Gn J Gn J . H K H k 2 2K 2 sin kx 1, They are also separated by the half of wavelengths. The standing wave can be obtained as a result of the reflection of the traveling wave in the string from the boundary. Indeed, the reflected wave has the same frequency and wavelength, but travels in the opposite direction. If the end of the string is fixed (attached to the wall), then the standing wave will have a node at this point. If the end of the string is fasten to a light ring on a vertical rod, so it can move freely, then this point is going to be an anti-node for the resultant standing wave. In the case if both ends of the string are fixed (the guitar string for instance) we can obtain a series of the standing waves at certain frequencies. Such standing waves are said to be produced at resonance and the string is resonating at these resonate frequencies. Since both ends of the string are fixed, they produce nodes for the resultant standing wave. This is only possible if the distance L between the ends of the string is equal the integer number of the half wavelengths, which is 2L , n 1,2... n So this wave has frequencies f v n v , n = 1,2... 2L The oscillation mode with the lowest frequency f=v/2L is called the fundamental mode or the first harmonic. The collection of all possible modes for n=1,2… is called the harmonic series and n is called the harmonic number. Let us now consider more general (not necessarily in one dimension) case of interference. This may happen with sound waves. It, for instance, takes place, when you hear sounds coming from different speakers. For simplicity we shall consider the interference between the two identical sound waves traveling in almost the same L1 P direction. S1 L2 S2 This situation is shown in the picture, where two waves are traveling from the two pointlike sources S1 and S2 to the same point in space P. Both waves are in phase and of identical wave length. We can also assume that distances from the sources to point P are much larger than the distance between the sources themselves, so we can say that waves are traveling in the same direction. Since distance L1 traveled from the first source is slightly different from the distance L2 traveled from the second source, the answer for the question, whether or not these waves are in phase at point P, depends strongly on the path length difference L L2 L1 . The phase difference between the two waves is equal L 2 . (1.2.13) The fully constructive interference occurs if the phase difference is equal to the integer number of 2 , so L 0,1,2... Fully destructive interference occurs when the phase difference between the waves is equal the odd multiple of , so L 1 3 5 , , ,... 2 2 2 One of the most interesting types of sound is the musical sound. In the most part of cases musical sound is obtained as a result of oscillations of some part of a musical instrument. For instance, it could be oscillating string of the string instrument such as a guitar or a violin. Actually, in this case it is even more complicated, because not only strings but also the bodies of these musical instruments are oscillating. In the case of the percussion like drums or plates, the oscillating parts are different membranes of the instruments. In the case of winds, the oscillating parts are not instruments themselves, but the air columns inside of those instruments. We have already discussed oscillations of strings. They can occur as a result of the standing transverse wave in those strings. The wavelength required for such a standing wave is the one, which has frequency corresponding to the resonant frequency of the string. In the case of the standing wave, the string will oscillate with a large enough amplitude to produce a strong hearable sound wave in the air. In a same way as we can set up the standing wave in a string, we can do it in a pipe of some wind instrument (for instance organ pipe) filled with air. In this case it is a longitudinal sound wave, but again it can be obtained as a result of the reflection from the end of the pipe. This reflection will take place for the pipe with the open end as well as for the pipe with the closed end. In order to have this standing wave, the wavelength should be in certain relation to the length of the pipe. These wavelengths correspond to the resonant frequencies of the pipe. The standing wave in the pipe is very similar to the standing wave in a string. The nodes of the standing wave correspond to the closed end of the pipe and antinodes correspond to the open end of the pipe. In the case of the pipe with two open ends, there are two antinodes at those ends. The simplest standing wave, which one can set up in such a pipe, is a wave, which only has one node in between the ends. This is fundamental mode or the first harmonic of that pipe. It is easy to see that its wavelength 2L , where L is the length of the pipe. More generally for the pipe with two open ends the resonant frequencies occur, when 2L , n 1,2,3... , n where n is called harmonic number. The resonant frequencies in this case are f v nv , n 1,2,3... 2L If one has a pipe with only one end opened (which will be the case in your laboratory experiment next time), it will be slightly different, since it should be a node at one end and antinode at the other. In the simplest case a wavelength should be 4L which is fundamental mode for this pipe. In general 4L , n 1,3,5... n In this case harmonic number n is an odd number and frequencies are given by f v nv , n 1,3,5... 4L So, the length of musical instrument reflects the possible values of frequencies it can generate. The larger the length, the lower frequency it can play. If one listens to sounds coming from two different sources, but those sources have very close frequencies, it will be almost impossible to distinguish between the two sounds. Instead the person will hear a sound which has a frequency equal to the average of the two combed frequencies. Intensity of this combined sound will change slightly with time wavering beats with frequency equal to the difference between the two combined frequencies. Let us consider this beat phenomenon at some point in space, where waves coming from the two sources have the form of s1 A cos 1t , s2 A cos 2t , where 1 2 . The superposition principle of two waves gives s s1 s2 A cos 1t cos 2t 2 2 2 A cos 1 t cos 1 t , 2 2 so we have s t 2 A cos t cos t , where 1 2 2 and 1 2 2 . Since frequencies of the two waves are very close, this means that and we can treat the first cosine function in the last equation as the slowly changing wave's amplitude. The angular frequency at which beats occur is beat 2 1 2 . This beat-phenomenon is used by musicians to turn their instruments on the standard frequency until beats disappear.
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