670 likes | 1.5k Views
Topic 4 Oscillations and Waves. Waves. Waves can transfer energy and information without a net motion of the medium through which they travel. They involve vibrations (oscillations) of some sort. Wave fronts. Wave fronts highlight the part of a wave that is moving together.
E N D
Waves Waves can transfer energy and information without a net motion of the medium through which they travel. They involve vibrations (oscillations) of some sort.
Wave fronts Wave fronts highlight the part of a wave that is moving together. = wavefront Ripples formed by a stone falling in water
Rays Rays highlight the direction of energy transfer.
Transverse waves The oscillations are perpendicular to the direction of energy transfer. Direction of energy transfer oscillation
Transverse waves peak trough
Transverse waves • Water ripples • Light • On a rope/slinky • Earthquake
Longitudinal waves The oscillations are parallel to the direction of energy transfer. Direction of energy transfer oscillation
Longitudianl waves compression rarefraction
Longitudinal waves • Sound • Slinky • Earthquake
Displacement - x This measures the change that has taken place as a result of a wave passing a particular point. Zero displacement refers to the average position. = displacement
Amplitude - A The maximum displacement from the mean position. amplitude
Period - T The time taken (in seconds) for one complete oscillation. It is also the time taken for a complete wave to pass a given point. One complete wave
Frequency - f The number of oscillations in one second. Measured in Hertz (s-1) 50 Hz = 50 vibrations/waves/oscillations in one second.
Wavelength - λ The shortest distance between points that are in phase (points moving together or “in step”). wavelength
Wave speed - v The speed at which the wave fronts pass a stationary observer. 330 m.s-1
Period and frequency Period and frequency are reciprocals of each other f = 1/T T = 1/f
The Wave Equation The time taken for one complete oscillation is the period T. In this time, the wave will have moved one wavelength λ. The speed of the wave therefore is distance/time v =λ/T = fλ
displacement cm Time s 0.1 0.2 0.3 0.4 -1 -2 Displacement/time graph This looks at the movement of one point of the wave over a period of time IMPORTANT NOTE: This wave could be either transverse or longitudnal 1 PERIOD
Displacement/distance graph This is a “snapshot” of the wave at a particular moment IMPORTANT NOTE: This wave could also be either transverse or longitudnal displacement cm 1 WAVELENGTH Distance cm 0.4 0.8 1.2 1.6 -1 -2
Wave intensity This is defined as the amount of energy per unit time flowing through unit area It is normally measured in W.m-2
Wave intensity For example, imagine a window with an area of 1m2. If one joule of light energy flows through that window every second we say the light intensity is 1 W.m-2.
Intensity and amplitude The intensity of a wave is proportional to the square of its amplitude I α a2 (or I = ka2)
Intensity and amplitude This means if you double the amplitude of a wave, its intensityquadruples! I = ka2 If amplitude = 2a, new intensity = k(2a)2 new intensity = 4ka2
Electromagnetic spectrum λ ≈ 700 - 420 nm λ ≈ 10-4 - 10-6 m λ ≈ 10-7 - 10-8 m λ ≈ 10-9 - 10-11 m λ ≈ 10-2 - 10-3 m λ ≈ 10-1 - 103 m λ ≈ 10-12 - 10-14 m
What do they all have in common? • They can travel in a vacuum • They travel at 3 x 108m.s-1 in a vacuum (the speed of light) • They are transverse • They are electromagnetic waves (electric and magnetic fields at right angles to each oscillating perpendicularly to the direction of energy transfer)
Refraction When a wave changes speed (normally when entering another medium) it may refract (change direction)
Snell’s law speed in substance 1 sinθ1 speed in substance 2 sinθ2 =
Snell’s law In the case of light only, we usually define a quantity called the index of refraction for a given medium as n = c cm where c is the speed of light in a vacuum and cm is the speed of light in the medium c vacuum cm
Snell’s law Thus for two different media sinθ1/sinθ2 = c1/c2 = n2/n1
Refraction – a few notes The wavelength changes, the speed changes, but the frequency stays the same
Diffraction Waves spread as they pass an obstacle or through an opening
Diffraction Diffraction is most when the opening or obstacle is similar in size to the wavelength of the wave
Diffraction Diffraction is most when the opening or obstacle is similar in size to the wavelength of the wave
Principle of superposition When two or more waves meet, the resultant displacement is the sum of the individual displacements
Constructive and destructive interference When two waves of the same frequency superimpose, we can get constructive interference or destructive interference. + = = +
If we pass a wave through a pair of slits, an interference pattern is produced
Path difference Whether there is constructive or destructive interference observed at a particular point depends on the path difference of the two waves
Constructiveinterference if path difference is a whole number of wavelengths antinode
Destructive interference if path difference is a half number of wavelengths node
Phase difference • is the time difference or phase angle by which one wave/oscillation leads or lags another. 180° or π radians
Phase difference • is the time difference or phase angle by which one wave/oscillation leads or lags another. 90° or π/2 radians
Simple harmonic motion (SHM) • periodic motion in which the restoring force is proportional and in the opposite direction to the displacement
displacement Time Graph of motion Amplitude x0 Period T x = x0sinωt where ω = 2π/T = 2πf = (angular frequency in rad.s-1)
When x = x0 at t = 0 Amplitude x0 Period T x = x0cosωt displacement Time where ω = 2π/T = 2πf = (angular frequency in rad.s-1)
displacement Time When x = 0 at t = 0 x = x0sinωt v = v0cosωt Amplitude x0 Period T where ω = 2π/T = 2πf = (angular frequency in rad.s-1)
When x = x0 at t = 0 x = x0cosωt v = -v0sinωt Amplitude x0 Period T displacement Time where ω = 2π/T = 2πf = (angular frequency in rad.s-1)
To summarise! • When x = 0 at t = 0 x = x0sinωtand v = v0cosωt • When x = x0 at t = 0 x = x0cosωt andv = -v0sinωt It can also be shown thatv = ±ω√(x02 – x2) and a = -ω2x where ω = 2π/T = 2πf = (angular frequency in rad.s-1)
Maximum velocity? • When x = 0 • At this point the acceleration is zero (no resultant force at the equilibrium position).
Maximum acceleration? • When x = +/– x0 • Here the velocity is zero