Waves in air, fluids and solids

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Notas de aula

Wave Basics

  • Waves transfer energy and information without transferring matter.
  • Waves are oscillations or vibrations about a fixed point.
  • Ripples on water cause particles to oscillate up and down; sound waves cause air particles to vibrate back and forth.
  • Objects floating on water (like a duck) bob up and down but do not travel with the wave, showing that matter is not transferred.

Describing Wave Motion

  • Amplitude is the distance from the undisturbed position to the peak or trough of a wave, measured in metres (m).
  • Wavelength is the distance from one point on a wave to the same point on the next wave, measured in metres (m).
  • Frequency is the number of waves passing a point each second, measured in hertz (Hz).
  • Time period is the time taken for one complete wave to pass a point, measured in seconds (s).
  • Frequency and period are related by: f = 1/T.
  • Wave speed is the speed at which energy is transferred through a medium.
  • Wavefronts are lines representing each wave; the distance between them is the wavelength.

Transverse wave motion in a rope: the vibration is at 90 degrees to the direction of wave motion and energy transfer, with the crest and trough labelled.

Transverse wave motion in a rope: the vibration is at 90 degrees to the direction of wave motion and energy transfer, with the crest and trough labelled.

Transverse and Longitudinal Waves

  • Transverse waves vibrate at 90° (perpendicular) to the direction of energy transfer.
  • Examples of transverse waves: ripples on water, vibrations in a guitar string, S-waves, electromagnetic waves.
  • Longitudinal waves vibrate parallel to the direction of energy transfer.
  • Longitudinal waves consist of compressions (regions of higher density) and rarefactions (regions of lower density).
  • Examples of longitudinal waves: sound waves, P-waves, pressure waves in liquids or gases.
  • Transverse waves can travel in solids and on the surfaces of liquids; longitudinal waves can travel in solids, liquids and gases.
  • Only electromagnetic waves (transverse) can travel through a vacuum; longitudinal waves cannot.

Longitudinal and transverse waves.

Longitudinal and transverse waves.

The Wave Equation

  • Wave speed can be calculated using: v = f × λ (wave speed = frequency × wavelength).
  • v is wave speed in metres per second (m/s), f is frequency in hertz (Hz), λ is wavelength in metres (m).
  • Wave speed can also be calculated using: v = x / t (speed = distance / time).
  • The wave equation can be rearranged to find frequency (f = v/λ) or wavelength (λ = v/f).
  • All waves obey the wave equation.

Measuring Wave Speed

  • Speed of sound in air can be measured between two points: measure distance with a trundle wheel, time the sound with a stopwatch.
  • Using echoes: clap blocks in rhythm with echoes, measure distance to wall, time 20 claps, total distance = 20 × 2 × distance.
  • Using an oscilloscope: two microphones connected to an oscilloscope, measure time difference for sound to travel between them.
  • Speed of ripples on water: measure distance between two points, time how long a ripple takes to travel, repeat and average.
  • The oscilloscope method is most accurate because timing is automatic; the two-point method is least accurate due to short time intervals.

Measuring the speed of sound between two points

Measuring the speed of sound between two points

Reflection, Absorption and Transmission

  • When waves meet a boundary between two materials, they can be reflected, absorbed or transmitted.
  • A reflected sound wave is called an echo.
  • Reflection occurs at the boundary between two different materials.
  • Transmission is when a wave passes through a material; absorption is when a wave's energy is taken in by a material.
  • Ray diagrams can be used to illustrate the reflection of a wave at a surface.

Sound Waves

  • Sound waves are longitudinal waves consisting of compressions and rarefactions.
  • Sound waves cause pressure variations in the air, so they are pressure waves.
  • When sound waves hit a solid, the pressure variations cause the solid to vibrate in sync with the wave.
  • Sound travels fastest in solids, slower in liquids, and slowest in gases because molecules are closer together in solids.
  • The human ear detects sound when sound waves cause the eardrum and small bones to vibrate, which creates electrical impulses sent to the brain.
  • The range of human hearing is 20 Hz to 20 000 Hz (20 kHz).

Ultrasound and Infrasound

  • Ultrasound is sound with a frequency above 20 000 Hz (above the human hearing range).
  • Infrasound is sound with a frequency below 20 Hz (below the human hearing range).
  • Ultrasound is used in sonar, foetal scanning, and industrial imaging.
  • Infrasound is produced by earthquakes (P-waves) and can be used to study the Earth's core.
  • Ultrasound waves are partially reflected at boundaries between different media; the time for reflections to return can determine distance.

Frequencies of ultrasound

Frequencies of ultrasound

Seismic Waves and Earth's Structure

  • Earthquakes produce P-waves (longitudinal) and S-waves (transverse).
  • P-waves travel faster than S-waves, so P-waves are felt first.
  • P-waves can travel through solids and liquids; S-waves can only travel through solids.
  • S-waves cannot pass through the Earth's liquid outer core, which is why they are not detected on the opposite side of the Earth from an earthquake.
  • P-waves refract as they pass through different layers, creating shadow zones that provide evidence about the Earth's internal structure.
  • Seismic waves provide evidence that the mantle is solid, the outer core is liquid, and the inner core is solid.

Calculating Depth and Distance

  • If wave speed is known, distance can be calculated using: distance = speed × time (x = v × t).
  • Echo sounding uses ultrasound to detect objects underwater and measure water depth.
  • The sound wave travels to the ocean bottom and back, so total distance = 2 × depth.
  • The time for the echo to return is used to calculate depth: depth = (speed × time) / 2.
  • For example, a thunderclap heard 4 s after lightning: distance = 330 m/s × 4 s = 1320 m.

Slides

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Questões de prática

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  1. 1.Which type of wave is a sound wave travelling through air?

    Easy
    • ATransverse
    • BLongitudinal
    • CElectromagnetic
    • DStationary
  2. 2.In a longitudinal wave, the particles vibrate at right angles to the direction in which the wave transfers energy.

    Easy

    True or false?

  3. 3.Which row correctly names the two features labelled on a longitudinal wave?

    Easy
    • ACompression = region of lower density; rarefaction = region of higher density
    • BCompression = region of higher density; rarefaction = region of lower density
    • CCompression = highest point; rarefaction = lowest point
    • DCompression = region of constant density; rarefaction = region of changing pressure
  4. 4.Which statement about the movement of particles in a sound wave travelling through air is correct?

    Medium
    • AAir particles travel along with the wave from the source to the listener.
    • BAir particles vibrate about fixed positions and do not travel with the wave.
    • CAir particles move at right angles to the direction of energy transfer.
    • DAir particles are permanently pushed away from the source.
  5. 5.Sound waves travel fastest in solids and slowest in gases.

    Easy

    True or false?

  6. 6.What is the normal range of frequencies that a healthy human ear can hear?

    Easy
    • A2 Hz to 2000 Hz
    • B20 Hz to 20 000 Hz
    • C200 Hz to 200 000 Hz
    • D20 Hz to 2000 Hz
  7. 7.What name is given to a sound wave that is reflected from a surface?

    Easy
    • AAn echo
    • BA refraction
    • CA rarefaction
    • DAn ultrasound
  8. 8.Which of the following statements about sound waves are correct? (select all that apply)

    Medium
    • AThey are longitudinal waves.
    • BThey consist of compressions and rarefactions.
    • CThey can travel through a vacuum.
    • DThey cause pressure variations in the air.
    • EThey travel faster in gases than in solids.

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