WAVES Definition • What is Wave? Wave is a method of propagation of energy For example: when we drop a pebble into a pond of still water, a few circular ripples move outwards, on the surface of the water. As these circular ripples spread out, energy is being carried with them • From definition above then waves carry energy. For Example: during an earthquake, the seismic waves produced can cause great damage to buildings and the surroundings Source of waves • The source of any wave is a vibration or oscillation • Wave motion provides a mechanism for the transfer of energy from one point to another without the physical transfer of the medium between the two points. Type of waves • Remind: wave is method of propagation of energy • Transverse wave: Energy propagate in a direction perpendicular to the direction of vibration Example: Rope waves, Water waves, Light waves, Radio waves, Electromagnetic waves. • Longitudinal wave: propagate in a direction parallel to the direction of vibration. Example: Sound waves and waves produced in a vertical oscillating spring under tension. Describing Waves • Crest and troughs • High point and low point that characterize transverse waves only. For longitudinal wave, compression and rarefaction are used. • Amplitude: The value of the maximum displacement from the rest of central position in either direction. • Wavelength: (λ) The shortest distance between any 2 points on a wave that are in phase. The two easiest points to choose for a distance of one wavelength are 2 successive crests or troughs. • Frequency: (f : Hz) Number of completed waves produced per second. For example: if the figure shows 2 completed waves and if they are produced in one second then the frequency of this wave is 2Hz • Period: (T : s) Time taken to product one completed wave. • Wave speed: the distance travelled by wave in one second. • Wave front: An imaginary line on a wave that join all points which are in phase of vibration. • Phase: 2 point are said to be in phase because that are moving in the same direction with same speed and having same displacement from rest point. Any 2 crests or troughs are in phases. • Phase difference: is the difference, expressed in degrees or radians, between two waves having the same frequency and referenced to the same point in time The wave equation and principle • Speed = distance / time • Wavelength is distance moved by the wave in one cycle i.e distance • Time = period = 1/frequency • So speed = wavelength / period Wave speed on stretched string Big wave rules: • The speed of a wave is determined by the type of wave and the characteristics of the medium, not by the frequency. • When a wave passes into another medium, its speed changes, but its frequency does not. • What is medium? Medium is environment that wave travel in. Superposition principle • Occurs when there is more than one wave in a medium at a given time. • At any instant, the resultant displacement is simply the sum of the displacements of the individual waves. • Constructive and destructive interference are obvious examples of this idea. • Constructive Interference: Resultant amplitude is larger than either individual wave. • Destructive Interference: Resultant amplitude is less than either individual wave. Examples Constructive Interference: Destructive Interference: Constructive Interference Standing Waves …a wave in which the amplitude at a given location does not vary with time. Standing Wave Features: • Amplitude is zero at fixed ends • Nodes (other places with zero amplitude) • Anti-nodes (places with maximum amplitude) Standing Wave: Both Ends Fixed Standing Wave: One End Fixed, One End Free Reflection of Waves – Fixed End • Whenever a traveling wave reaches a boundary, some or all of the wave is reflected • When it is reflected from a fixed end, the wave is inverted • The shape remains the same Reflected Wave – Free End • When a traveling wave reaches a boundary, all or part of it is reflected • When reflected from a free end, the pulse is not inverted Mathematical Description of the Travelling waves Or Where: - A : amplitude - ω: angular frequency. - λ: wavelength y = A sin (ωt + 2πx/λ) y = A sin (ωt - 2πx/ λ) Sound wave The speed of a sound wave depends on the medium through which it travels. In particular, it depends on the density (ρ ) and on the bulk modulus (B), a measure of the medium’s response to compression. • Sound level: • Intensity: the rate at which they transmit energy, per unit area. (W/ 𝑚2 ) • Intensity is proportional with 𝐴2 => Intensity depends on the wave’s amplitude: The greater the amplitude (A), the greater the intensity (and, therefore, the louder the sound) • Loudness: how soft or how intense the sound is as perceived by the ear and interpreted by the brain. (Unit: decibels dB) Where: 𝐼0 is threshold of hearing. • Pitch : is perceived as how "low" or "high" a sound is and represents the cyclic, repetitive nature of the vibrations that make up sound (frequency) • Duration: is perceived as how "long" or "short" a sound is and relates to onset and offset signals created by nerve responses to sounds • Beat: When two sound waves of different frequency approach your ear, the alternating constructive and destructive interference causes the sound to be alternatively soft and loud - a phenomenon which is called "beating" or producing beats. The Doppler effect is the way a wave seems to increase or decrease in frequency when there is relative motion between the observer and the source of the wave. Have you ever stopped at a railroad crossing to let a train pass by? Did you notice that the sound of the train's whistle is higher pitched when the train was approaching and lower when it was receeding? Then you have witnessed the Doppler effect. Doppler Acapella (Link) When a source of waves and an observer are moving towards each other: 1. A higher frequency is heard 2. A shorter wavelength is observed. When a source of waves and an observer are moving apart: 1. A lower frequency is heard 2. A longer wavelength is observed. Doppler’s effect Weather radars send out radio waves. Objects in the air, such as rain drops, snow crystals, hail stones or even insects and dust, scatter or reflect some of the radio waves back to the antenna. Weather radars electronically convert the reflected radio waves into pictures showing the location and intensity of precipitation. Doppler radars also measure the frequency change in returning radio waves. Waves reflected by something moving away from the antenna change to a lower frequency. Waves from an object moving toward the antenna change to a higher frequency. Summary • Type of waves: W AVES M echanical w aves Transversewaves Electrom agneticw aves Longitudinal waves Transversewaves Wave Properties - A wave is described in terms of the following characteristics: Amplitude Wavelength ( ) Frequency (f ) Period (T) Wave velocity (v) Crest Trough Compression Rarefaction Nodes Speed of wave Constructive & Destructive Interference Section 13.10