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Standing Waves
  • 00:07Overview
  • 01:15Principles of Standing Waves and Simple Harmonics
  • 04:15Observing the Superposition of Wave Pulses
  • 05:39Measuring Frequency of Standing Waves
  • 06:37Data Analysis and Results
  • 07:50Applications
  • 09:05Summary

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Overview

출처: 아리아나 브라운, 아산타 쿠레이, 박사, 물리학 및 천문학학과, 물리 과학 대학, 캘리포니아 대학, 어바인, 캘리포니아

서 있는 파도 또는 고정된 파도는 전파하지 않는 것처럼 보이며 동일한 주파수와 진폭으로 반대 방향으로 이동하는 두 파도의 간섭에 의해 생성됩니다. 이 파도는 선형 움직임없이 위아래로 진동하는 것처럼 보이며 뽑은 기타 문자열, 호수의 물 또는 방에있는 공기와 같은 유한 한 매체에서 가장 쉽게 식별됩니다. 예를 들어, 문자열이 양쪽 끝에 고정되고 길이를 따라 이동하는 두 개의 동일한 파도가 전송되면 첫 번째 파도가 끝 장벽에 부딪히고 반대 방향으로 반사되고 두 파도가 겹쳐서 서있는 파도를 생성합니다. 이 동작은 매체의 길이에 의해 정의된 주파수로 주기적으로 되며 간단한 고조파 모션의 시각적 예입니다. 간단한 고조파 운동은 복원력이 변위에 비례하는 진동 또는 주기적인 동작으로, 더 멀리 무언가가 밀려나기 어렵게 밀어 붙입니다.

이 실험의 목적은 서 있는 파도를 만드는 파도 중첩과 반사의 역할을 이해하고, 이러한 개념을 활용하여 처음 몇 개의 공진 주파수 또는 고조파를 계산하는 것입니다. 물체가 생성하는 각 주파수에는 가능한 빈도가 가장 낮은 웨이브가 기본 주파수라고 하는 자체 서파 패턴이 있습니다. 고조파는 전체 정수 수에 의해 기본 주파수에 비례하는 주파수를 가진 파도입니다.

Principles

Procedure

1. 슬링키 펄스의 중첩과 반사 관찰 한 학생이 한쪽 끝을 들고 다른 학생을 안고 바닥이나 복도를 가로질러 길게 늘어서 있거나 강철 스프링을 길게 늘라. 테이프를 사용하여 양쪽에 슬링키 의 중간에서 떨어진 발에 대해 두 개의 길이 ‘장벽’을 표시합니다. 양쪽의 중간에서 2피트 떨어진 장벽으로 반복합니다. 표시된 장벽 내에 머무르는 진폭으로 펄스를 발사합니다(작은 거리를 수?…

Results

Harmonic (n) # Cycles Total Time (s) Frequency (Hz) f/f0 Period (s) Wavelength (m)
1 10 19.2 0.521 (f0) 1 1.210 16 m
2 10 9.75 1.026 1.97 0.975 8 m
3 10 6.21 1.601 3.07 0.625 5.33 m

Table 1: Section 2 – Stretched Spring Length = 8 m

In Section 1, principles of wave superposition and reflection in a finite medium are demonstrated and confirmed as pulses were sent down the length of the slinky. Specifically, we see that when two waves with identical amplitudes and phase meet, they undergo constructive interference and their amplitudes add. Similarly, we see that when two waves with opposite polarity (180 ° phase shift) and identical amplitudes meet, they undergo destructive interference and their amplitudes cancel. The latter of these principles is key in understanding standing wave patterns.

In Section 2, the nodes and antinodes of the slinky were easily visible at various frequencies. As the number of nodes increased, so did the frequency. The wavelength is inversely proportional to frequency, so there is naturally a decrease in wavelength. The frequencies of the harmonics are positive integer multiples of the fundamental frequency that correspond to n. For example, using the n = 2 harmonic, the frequency is measured and defined as the number of cycles per unit time:

Equation 4

The period is defined as the inverse of the frequency (Equation 2) and is equal to:

Equation 5

The wavelength is defined in Equation 1 as:

Equation 6

Finally, we can see the integer-proportional relationship between the harmonics and the fundamental frequency by calculating:

Equation 7

Applications and Summary

In this experiment, the concepts of wave superposition and standing waves were explored in two demonstrations. Wave reflection and constructive versus destructive interference were visualized in the first demonstration. In the second, the changes in frequency and period were measured and higher harmonic frequencies were found to be integer multiples of the fundamental frequency.

A famous example of standing waves in the real world are the strings on a guitar, or any string instrument. In these instruments, a plucked string emits a particular frequency depending on how taut and dense the string is and the string length. Each string only makes certain notes because only certain standing waves, or harmonics, can form on that string. The musician can use their fingers to shorten the string length, creating a new node and new set of harmonics that are proportional to the fundamental frequency. Vibrations that are not at the right frequency, say fingers pinning the strings down onto a fret that doesn't allow for a standing wave at that string length, will sound odd and eventually cancel themselves out.

Standing waves also occur in nature, often in bounded bodies of water like lakes and harbors. Sometimes, they can form on a river bed allowing river surfers to ride this wave for an extended period of time without actually moving. Typically, they form when a large amount of water is flowing over an obstruction, like a big rock, at a rapid pace. As the water flows over the rock and crashes behind it, it creates a large wave in the opposite direction of the river's current that interferes with the incident wave of water. Thus, a standing wave is formed and river surfers can ride it for as long as their balance will allow them since the wave likely will not end in a matter of seconds.

Transcript

Standing waves, or stationary waves, are waves that appear to not propagate and they are most evident in a vibration. For example, when a taut string is plucked, the resulting waves appear to vibrate up and down, with no linear movement. These are actually produced by the interference of two waves traveling in opposite directions, with the same frequency and amplitude.

This oscillating motion with periodic frequency is an example of simple harmonic motion. The motion happens because the string has a restoring force that is proportional to the initial displacement. This relationship between restoring force and displacement is given by Hooke’s Law — explained in detail in another JoVE Science Education video. This essentially means that the harder something is pulled, like this sling shot, the harder it pushes back.

In this video, we will create standing waves using a slinky, and explore the physics behind simple harmonic motion and its applications.

Before we start the demonstration in the laboratory, let’s learn a bit more about standing waves and simple harmonic motion. A wave is defined by its wavelength, lambda — the distance between two crests, and its frequency, f — the number of occurrences of crests in unit time, The amplitude is the distance from crest to trough. When two waves arrive at the same point in a path, at the same time, they interfere. The amplitude of the resulting wave is the sum of the amplitudes of the two waves.

Constructive interference occurs when the amplitudes of the waves are in phase, and add. Destructive interference occurs when the waves are out of phase, and the amplitudes subtract.

Take for example, a pulse on a finite string. Ideally, when the traveling pulse meets a boundary, it is reflected. Now let’s send a wave down the string, and let it reflect back and forth for an extended period of time. This action creates a stationary pattern, or standing wave.

The points of minimum amplitude, called nodes, are where the waves have opposite phases and cancel each other out. The points of maximum amplitude, or antinodes, are points where the waves have the same phase and their amplitudes combine. The simplest standing wave occurs when the wavelength is twice the length of the string.

The next possible standing wave has a node in the center, and the wavelength equals the length of the string. If we continue to add nodes, we create waves with shorter and shorter wavelengths. These patterns are called harmonics, where the number of antinodes, denoted by letter n, gives the wave of nth harmonic. So if the wave has four antinodes, the wave is the fourth harmonic.

Based on the relationship between the wavelength and the length of the string of each harmonic, we can derive a formula relating these three terms and say that lambda of an nth harmonic standing wave equals two times the length of the string divided by n.

Since 2L is the wavelength of the first harmonic, the wavelength of each harmonic is Λ1 divided by n. Now, we know that Λ and f have inverse relationship. Hence, we can deduce that the frequency of each harmonic would be the nth multiple of the first harmonic, or the ratio of the frequency to the frequency of first harmonic yields n. Note that the first harmonic is also known as the fundamental frequency of that string.

Now that we’ve discussed the basics of simple harmonics, let’s take a look at how to make standing waves using a slinky, and how to measure the frequency of standing waves.

First, stretch a slinky or steel spring lengthwise across the floor with one person holding each end. Use tape to mark two lengthwise barriers, each about a foot away from the middle of the slinky, on each side.

Also, add lengthwise barriers that are two feet away from the middle of the slinky on each side.

Take turns for launching wave pulses by jerking the slinky a small distance horizontally, and then immediately snapping it back to the starting point. Ensure that the amplitudes stay within the marked barriers.

Next, simultaneously launch identical pulses with the same polarity, and observe what happens when the pulses meet. The superimposed wave should double in amplitude, cross the first taped barriers and hit the second taped barriers.

Now, simultaneously launch identical pulses with opposite polarity. The pulses should cancel one another out as they superimpose and continue traveling. They should never reach the barriers.

Finally, fix one end by holding it tightly in position. Send a single pulse down to the fixed position, and observe the waves amplitude as it is reflected. It will reflect back with opposite polarity.

Now let’s take a look at how to measure the frequency of standing waves. Stretch the slinky across the room again, and measure the stretched length.

With one end fixed, gently begin sliding the other end horizontally until you find the first harmonic. For this harmonic, there should be only one wave’s crest with one amplitude moving back and forth.

Use a stopwatch to record the time it takes for each wave cycle. One complete cycle starts when an antinode forms on one side, slides through the center to form an antinode on the other side, and then returns to the original position.

Now, increase the speed of the sliding until you reach the next harmonic. For the second harmonic, there should be two wave crests on opposite sides moving in opposite directions. Measure the time for one wave cycle.

Repeat these steps for the third harmonic.

Now that we have discussed the experiment, let’s learn how the analyze the data collected in order to obtain the frequencies of different harmonics. Recall, the wavelength is equal to two times the length of the slinky divided by n. Thus, for the second harmonic, the wavelength is the length of the slinky, or 8 m.

Frequency is defined as the number of cycles per unit time. Thus, frequency can be calculated for each harmonic by dividing the number of cycles by the total time. It is evident that, as n increases, the frequency of the wave also increases.

This was noticeable during the experiment as well. Now let’s verify the relationship between the frequencies and n. If we divide the frequency of each harmonic with the fundamental frequency, then we obtain these values. These values demonstrate that the second harmonic is approximately twice the frequency of the fundamental frequency and the third harmonic is thrice the fundamental frequency. Together, these results validate the harmonics formulae.

Standing waves can be found in many real world examples in science and nature.

A plucked guitar string is a simple example of a standing wave. A plucked string emits a particular sound frequency depending on the string length and how taut or dense the string is.

Each string only makes certain notes because only certain standing waves are able to form on that string. These standing waves are all integer multiples of the string’s fundamental frequency. The musician can shorten the string length, creating a new set of harmonics.

Acoustophoresis, which means migration with sound, is a technique in biomedical engineering that uses standing waves to displace particles in a microscale channel of flowing liquid. This is typically performed in a microfluidic device, which has micrometer scale fluid channels.

When a standing wave with specific frequency is formed within the channel, which focuses the particles into a controlled stream. Using this method, a researcher can rapidly focus or separate microscopic entities.

You’ve just watched JoVE’s introduction to standing waves and simple harmonic motion. You should now understand the properties of standing waves, and where they are present in every day applications. Thanks for watching!

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JoVE Science Education Database. JoVE Science Education. Standing Waves. JoVE, Cambridge, MA, (2023).