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Waves
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Menu Describing Waves Ultrasound Refraction of water waves
Seismic Waves
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Longitudinal Waves SOUND IS A LONGITUDINAL WAVE
Direction of wave Travel Vibrations In Longitudinal waves the VIBRATIONS are along the SAME DIRECTION as the Wave is Travelling SOUND IS A LONGITUDINAL WAVE
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Transverse Waves Most Waves are Transverse. LIGHT IS A TRANSVERSE WAVE
Direction of Wave Travel Most Waves are Transverse. LIGHT IS A TRANSVERSE WAVE Vibrations are at right Angles to Direction of Travel
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Describing Waves Vertical displacement Amplitude Horizontal Displacement Amplitude THE AMPLITUDE shows the displacement of the particles. It is related to energy
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Describing Waves THE WAVELENGTH is a full cycle of the wave Wavelength
Vertical displacement Wavelength Horizontal Displacement THE WAVELENGTH is a full cycle of the wave
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Describing Waves Vertical displacement Time THE PERIOD is the time taken for 1 complete cycle. (Notice the change in the horizontal axis)
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Frequency The frequency is the number of waves that pass a set point each second It is measured in hertz (Hz)
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The Wave Equation Speed Frequency & Wavelength are all linked together using the following equation:- SPEED = FREQUENCY x WAVELENGTH m/s Hz m
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Our Ears can only hear a certain range of ‘frequencies’
The ‘NORMAL’ range of human hearing is:- 20 Hz to ,000Hz A wasp moves its wings more than 20 times a second because we can hear it This means that we can only hear objects that vibrate over 20 times per second
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The upper limit decreases with age
The upper limit decreases with age. Sounds above 20,000Hz can’t be heard by humans. They can however be heard by dogs, bats etc Sounds above 20,000Hz are called ULTRASOUND
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Ultrasound is useful to us
We can use ultrasound to:- Clean delicate mechanisms (electronics, teeth & jewellery) Check for ‘cracks’ in aeroplane wings Sonar and Pre- natal Scanning
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Foetal Scanning Can you see the baby sucking its thumb? Menu
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When sound is reflected we call it an ECHO
We can use sound echoes to detect: shoals of fish Oil reserves how a foetus is developing inside the mothers womb cracks on aeroplane wings/ bridges Return to Menu
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Refraction of water waves
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Deep Water - Fast Waves Shallow Water - Slow Waves
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Waves are bent towards the normal
Wavelength decreases Frequency stays the same Deep Water - Fast Waves Shallow Water - Slow Waves
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Refraction – of plane waves
Deep water Boundary Shallow water
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Deep Deep Shallow
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Deep Deep Shallow If the waves arrive perpendicular to the boundary they do not bend Menu
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The Structure of the Earth
Seismic Waves & The Structure of the Earth
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The Earth’s Crust Is Made up of ‘Plates’ That Constantly Move
Which way have the ‘plates’ moved?
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An Earthquake Occurs When There Is Movement in the Plates
There are 2 types of waves P WAVES are Push and Pull Longitudinal Waves S WAVES are Shear or Shake Transverse Waves
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The Structure of the Earth
Crust Mantle Outer Core Inner Core
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The Structure of the Earth
The paths of the waves are curved because of Refraction (changes in density) If the wave travels along the ‘normal’ it does not deviate from its position
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The Structure of the Earth
P waves travel through both solids & liquids P waves travel faster than s waves NO WAVES pass through the Shadow Zone No S Waves reach here as they can’t pass through the core
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What does the seismograph tell us about the structure of the Earth?
1) About halfway through the Earth there is an abrupt change in direction of both types of waves, indicating a sudden change in density at that point – THE CORE
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What Does the Seismograph Tell Us About the Structure of the Earth?
2) The fact that S waves are NOT detected in the shadow of the core tells us that the CORE IS LIQUID
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What Does the Seismograph Tell Us About the Structure of the Earth?
3) P Waves travel slightly faster through the middle of the core. This strongly suggests there is a SOLID INNER CORE
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What damage can earthquakes do?
Damage to buildings Fires caused by ruptured power lines Death Disease can spread rapidly due to disrupted water & food supplies Return to Menu
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