GCSE Physics - Intro to Waves - Longitudinal and Transverse Waves #61

Cognito
15 Jan 202006:21

Summary

TLDRThis educational video delves into the fundamentals of wave physics, explaining how waves transfer energy without matter. It covers wave labeling, including amplitude, wavelength, crest, and trough, and introduces the concepts of time period and frequency. The video also demonstrates how to calculate wave speed using wavelength and frequency, and distinguishes between transverse and longitudinal waves, providing examples of each. The content is designed to clarify complex wave dynamics in an accessible manner.

Takeaways

  • 🌊 Waves are energy transfer phenomena that do not move matter from one place to another.
  • πŸ‘€ Our brain interprets energy from light and sound waves as meaningful information, allowing us to see images and hear sounds.
  • πŸ“Š The displacement distance graph shows how far a wave has traveled and oscillated from its equilibrium point.
  • πŸ”Ό Amplitude is the maximum displacement of a wave from its equilibrium position.
  • πŸŒ€ Wavelength is the distance of one complete oscillation of a wave, from crest to crest or trough to trough.
  • πŸ•’ Time period is the duration of one complete oscillation, measured when time is on the x-axis of a graph.
  • πŸ”’ Frequency, measured in hertz, is the number of complete oscillations per second and can be calculated using the time period.
  • πŸš€ Wave speed is calculated by multiplying the wavelength by the frequency, giving the total distance waves travel per second.
  • πŸ“ For a given example, a sound wave with a frequency of 400 Hz and a wavelength of 70 cm (0.7 m) has a speed of 280 m/s.
  • ↕️ Transverse waves oscillate perpendicular to the direction of energy transfer, like light and water waves.
  • πŸ”„ Longitudinal waves oscillate parallel to the direction of energy transfer, with regions of compression and rarefaction, such as sound waves.

Q & A

  • What is the primary function of waves?

    -Waves transfer energy from one place to another without transferring matter.

  • Can waves transfer information? If so, how?

    -Yes, waves can transfer information. For example, light waves from a phone screen or sound waves from speakers can be interpreted by the brain as images or sounds.

  • What are the key parts of a wave?

    -The key parts of a wave include the crest (the highest point), trough (the lowest point), wavelength (the distance of one complete oscillation), and amplitude (the maximum displacement from the equilibrium point).

  • How do displacement-distance and displacement-time graphs differ?

    -In a displacement-distance graph, the x-axis represents distance, while in a displacement-time graph, the x-axis represents time. The wavelength corresponds to distance in the former, while the time period corresponds to time in the latter.

  • What is the time period of a wave, and how is it related to frequency?

    -The time period is the time it takes for one complete oscillation. It is inversely related to frequency, which is the number of oscillations per second. The relationship is given by the formula: Time Period = 1 / Frequency.

  • How can you calculate the frequency if you know the time period?

    -Frequency can be calculated using the formula: Frequency = 1 / Time Period.

  • What equation is used to calculate wave speed, and how does it work?

    -Wave speed is calculated using the equation: Wave Speed = Wavelength Γ— Frequency. This equation multiplies the length of one wavelength by the number of wavelengths per second, giving the total distance the wave travels per second.

  • What is the wave speed of a sound wave with a frequency of 400 Hz and a wavelength of 70 cm?

    -First, convert 70 cm to meters, which is 0.7 meters. Then, multiply by the frequency of 400 Hz. The wave speed is 280 meters per second.

  • What is the difference between transverse and longitudinal waves?

    -In transverse waves, the oscillations are perpendicular to the direction of energy transfer (e.g., light waves). In longitudinal waves, the oscillations are parallel to the direction of energy transfer (e.g., sound waves).

  • Can you provide examples of transverse and longitudinal waves?

    -Examples of transverse waves include electromagnetic waves (like light and radio waves) and water ripples. Examples of longitudinal waves include sound waves and seismic P-waves.

Outlines

00:00

🌊 Basics of Waves and Energy Transfer

This paragraph introduces the fundamental concepts of waves, emphasizing their role in transferring energy without matter. It explains how waves, such as light and sound, carry energy and can convey meaningful information to our brain, allowing us to perceive images and sounds. The paragraph delves into the terminology of waves, including amplitude, wavelength, crest, and trough, and introduces the concept of displacement and distance graphs to illustrate wave behavior. It also explains the time period and frequency, highlighting their relationship and how they can be calculated using specific equations.

05:01

πŸ“ Understanding Wave Speed and Types

The second paragraph focuses on calculating wave speed and distinguishing between transverse and longitudinal waves. It teaches how to determine wave speed by multiplying wavelength by frequency, using an example of a sound wave to illustrate the calculation. The paragraph also contrasts transverse waves, where oscillations are perpendicular to the direction of energy transfer, with longitudinal waves, where oscillations occur parallel to the energy transfer. Examples of each type of wave are provided, such as electromagnetic waves for transverse and sound waves for longitudinal, concluding with a brief mention of shock waves like seismic P-waves.

Mindmap

Keywords

πŸ’‘Waves

Waves are disturbances that transfer energy through a medium or space, as described in the video. They are central to the theme as they form the basis for discussing various concepts like energy transfer, wave speed, and types of waves. The script mentions light and sound waves as examples of how waves carry energy without matter.

πŸ’‘Energy Transfer

Energy transfer refers to the movement of energy from one point to another, which is a fundamental concept in the video. It is exemplified by the script's explanation of how light waves transfer energy from a phone screen to the eye, and sound waves from speakers to the ear.

πŸ’‘Displacement

Displacement in the context of waves is the distance a point on the wave has moved from its equilibrium position. It is key to understanding wave behavior, as the script describes it in relation to amplitude and wavelength, using a graph to illustrate the concept.

πŸ’‘Amplitude

Amplitude is the maximum displacement of a wave from its equilibrium position. It is a measure of the wave's energy and is crucial for understanding wave characteristics. The script mentions amplitude when explaining the distance of one complete oscillation.

πŸ’‘Wavelength

Wavelength is the distance of one complete oscillation of a wave, which could be from peak to trough or from one crest to the next. It is a fundamental property of waves and is used in the script to explain how waves travel and their speed.

πŸ’‘Crest

The crest is the highest point of a wave, as mentioned in the script when describing the distance of one oscillation. It is an important part of the wave's structure and is used to help understand the concept of wavelength.

πŸ’‘Trough

The trough is the lowest point of a wave, opposite to the crest. It is used in the script to contrast with the crest and to illustrate the concept of a complete oscillation, which is vital for understanding wavelength.

πŸ’‘Time Period

The time period is the duration of one complete oscillation of a wave, measured in seconds. It is related to frequency and is used in the script to explain how to calculate frequency and vice versa, providing a way to quantify wave behavior over time.

πŸ’‘Frequency

Frequency is the number of complete oscillations a wave makes per second, measured in hertz. It is a key concept in the video, as it helps to understand how often a wave oscillates and is used in the script to demonstrate the relationship between time period and wave speed.

πŸ’‘Wave Speed

Wave speed is the distance a wave travels per second, calculated by multiplying the wavelength by the frequency. It is a central concept in the video, as it quantifies how fast waves propagate and is illustrated with an example of a sound wave in the script.

πŸ’‘Transverse Waves

Transverse waves are waves where the oscillations are perpendicular to the direction of energy transfer. They are a key type of wave discussed in the video, with examples including light and radio waves, and are contrasted with longitudinal waves.

πŸ’‘Longitudinal Waves

Longitudinal waves have oscillations that are parallel to the direction of energy transfer, creating regions of compression and rarefaction. They are a type of wave explained in the video, with sound waves and seismic waves as examples, to contrast with transverse waves.

Highlights

Waves transfer energy without transferring matter.

Waves can carry meaningful information that our brain interprets as images or sounds.

A displacement distance graph illustrates the wave's travel and oscillation from the equilibrium point.

Amplitude is the maximum displacement of a wave from its equilibrium position.

Wavelength is the distance of one complete oscillation, from crest to crest or trough to trough.

Crest is the highest point of a wave, while the trough is the lowest.

A displacement time graph shows the wave's oscillation over time.

Time period is the duration of one complete oscillation.

Frequency, measured in hertz, is the number of complete oscillations per second.

The relationship between time period and frequency is reciprocal, calculated as 1/frequency.

Wave speed is calculated by multiplying wavelength by frequency.

An example calculation shows how to find the speed of a sound wave given its frequency and wavelength.

Transverse waves have oscillations perpendicular to the direction of energy transfer.

Examples of transverse waves include light, radio waves, water ripples, and string vibrations.

Longitudinal waves have oscillations parallel to the direction of energy transfer, causing regions of compression and rarefaction.

Sound waves and seismic P-waves are examples of longitudinal waves.

The video concludes with a summary of the key concepts covered.

Transcripts

play00:04

in today's video we're going to look at

play00:06

the basics of waves

play00:08

including how to label the different

play00:10

parts

play00:11

how to calculate the wave speed

play00:14

and the differences between transverse

play00:17

and longitudinal waves

play00:22

the first thing to understand about

play00:24

waves is that they transfer energy from

play00:27

one place to another but they don't

play00:30

transfer any matter

play00:33

so when light waves pass from a phone

play00:36

screen to your eye

play00:38

or sound waves pass from the speakers to

play00:40

your ear

play00:42

only energy is being transferred

play00:45

sometimes though we can interpret that

play00:47

energy as meaningful information

play00:49

which is why our brain is able to build

play00:52

up images and tunes from the light and

play00:55

sounds that it receives

play00:59

to travel from one place to another

play01:02

the waves vibrate or oscillate

play01:05

as we can see in this displacement

play01:07

distance graph

play01:10

the distance is how far the wave has

play01:12

traveled from the starting point

play01:15

while the displacement is how far from

play01:18

the equilibrium point the wave has

play01:20

oscillated

play01:22

so how far it's gone up or down

play01:25

the maximum displacement is known as the

play01:28

amplitude

play01:29

while the distance of one entire

play01:32

oscillation is called the wavelength

play01:35

so that could be from equilibrium

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up down and back up

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or it could be from the very top of a

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wave which we call the crest

play01:45

down and back up to the next crust

play01:48

it just has to be one entire oscillation

play01:52

and the opposite of the crest is called

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the trough

play01:59

now sometimes you might see a

play02:01

displacement time graph instead

play02:04

which looks pretty much the same

play02:06

but because we have time on the x-axis

play02:09

instead of distance

play02:11

the length of one complete oscillation

play02:13

would be the time period instead of the

play02:16

wavelength

play02:18

and the time period is just the time it

play02:20

takes for one complete oscillation

play02:24

the benefit of knowing the time period

play02:26

is that we can then use this equation

play02:28

here to work out frequency

play02:32

which is measured in hertz

play02:34

and is a number of complete oscillations

play02:36

per second

play02:40

to see how it works imagine that each

play02:42

oscillation takes 0.5 seconds

play02:46

or in other words the time period is 0.5

play02:50

seconds

play02:52

this means that there must be a total of

play02:54

two oscillations per second

play02:57

so the frequency is two

play03:00

which is what we'd get if we did one

play03:02

divided by the time period of 0.5

play03:08

we can also use the equation the other

play03:10

way around

play03:12

so time period equals 1 over frequency

play03:16

so if we were told that the frequency of

play03:19

a wave was four hertz

play03:21

which means four oscillations per second

play03:25

then to find the time period we'd just

play03:27

do one divided by four

play03:30

which tells us that each oscillation

play03:32

must be 0.25 seconds

play03:39

the next equation to know is that we can

play03:41

find the speed of the wave

play03:43

so the wave speed

play03:45

by multiplying the wavelength by the

play03:48

frequency

play03:50

so basically we multiply how long each

play03:53

wavelength is

play03:54

by how many there are per second

play03:58

and that will give us the total distance

play03:59

they travel per second

play04:02

to see how this works let's imagine we

play04:04

had a sound wave that had a frequency of

play04:07

400 hertz

play04:09

and a wavelength of 70 centimeters

play04:13

what is its wave speed

play04:17

well in this case all we'd have to do is

play04:19

convert the 70 centimeters to 0.7 meters

play04:23

because we always want our wavelength in

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meters

play04:26

and then multiply it by the frequency of

play04:29

400 hertz

play04:32

which gives us 280 meters per second as

play04:35

our wave speed

play04:40

the last thing we need to look at are

play04:42

the differences between transverse and

play04:44

longitudinal waves

play04:47

in transverse waves the oscillations are

play04:51

perpendicular to the direction of energy

play04:53

transfer

play04:55

or the direction in which the wave is

play04:57

moving

play04:59

which is why on our drawing the

play05:01

vibrations are going up and down

play05:04

whilst the overall wave is traveling

play05:06

from left to right

play05:10

most waves we can think of are

play05:11

transverse

play05:13

including all electromagnetic waves

play05:15

like light and radio waves

play05:19

ripples and waves in water

play05:21

and the waves of strings like on a

play05:23

guitar

play05:27

longitudinal waves on the other hand

play05:29

have oscillations that are parallel to

play05:32

the direction of energy transfer

play05:35

this one's a bit trickier to get your

play05:37

head around but basically it leads to

play05:39

some regions that are more spread out

play05:42

and other regions that are more

play05:44

compressed

play05:45

because the waves vibrating back and

play05:47

forth

play05:49

in motion it would look as if this area

play05:51

of compression is moving from the left

play05:54

to the right within the wave

play05:57

examples of longitudinal waves include

play05:59

sound waves

play06:01

and some types of shock waves like

play06:03

seismic p waves

play06:10

anyway that's everything for this video

play06:12

so hope you found it useful

play06:14

and i'll see you again soon

play06:20

you

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Related Tags
Wave BasicsEnergy TransferWave SpeedTransverse WavesLongitudinal WavesLight WavesSound WavesWavelengthFrequencyAmplitudeOscillation