Waves Waves - disturbance that propagates through space & time - - - PowerPoint PPT Presentation

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Waves Waves - disturbance that propagates through space & time - - - PowerPoint PPT Presentation

Waves Waves - disturbance that propagates through space & time - usually with transfer of energy - Mechanical requires a medium - Electromagnetic no medium required Mechanical waves: sound, water, seismic . the wave


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Waves

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Waves

  • disturbance that propagates through space & time
  • usually with transfer of energy
  • Mechanical

requires a medium

  • Electromagnetic

no medium required Mechanical waves: sound, water, seismic …. ‘the wave’ Electromagnetic waves: all light - radio, microwave, infrared, visible ...

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SLIDE 3

Waves travel & transfer energy from place to place need not be permanent displacement e.g., oscillation about fixed point Mechanical waves require a medium it must be an elastic medium cannot be perfectly stiff or perfectly pliable … no wave!

everything moves in unison

  • nly translation

all particles move independently no propagation

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SLIDE 4

Most waves are of two sorts: “String” type : particles oscillating perpendicular to propagation “Density” type : particles oscillating parallel to propagation … so far as we are concerned, at least

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Describing waves example: mass on a spring; oscillation perp. to wave direction

y time y0

2A A wavelength λ

time y0

crest node trough A = amplitude = intensity λ = wavelength = char. size f = frequency, full periods/sec wave propagation

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SLIDE 6

y time y0

2A A wavelength λ T = Period = how long per cycle T = 1/f or f = 1/T frequency - wavelength - velocity: λf = v = velocity of wave propagation

  • r vT = λ …. travel one wavelength per period

simplest wave:

f(x, t) = A sin

  • 2πft − 2π

λ x

  • λ characterizes

SPATIAL variation f characterizes TIME variation circular motion had no spatial dependence

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SLIDE 7

Characteristics of waves they have Crests & Troughs

  • intensity varies periodically. “vibration”

Longitudinal Transverse vibrations are PERPENDICULAR to propagation vibrations are PARALLEL to propagation string, EM waves sound

time

vibration propagation

amplitude

propagation vibration

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SLIDE 8
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SLIDE 9
  • f course, there are in between cases

mixed transverse & longitudinal e.g., objects bobbing up & down on a water wave

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Under some conditions, all waves can: reflect: change direction after hitting a reflecting surface refract: change direction after hitting a refracting surface diffract: bend as they interact with objects (when object’s size is near wavelength) interfere: superposition of colliding waves disperse: split up by frequency move in a straight line: propagation (standing waves)

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Reflection pulse on a string density wave

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Refraction (mainly PH102) light & heavy string density wave at a boundary

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Refraction of sound If the air above the earth is warmer than that at the surface, sound will be bent back downward toward the surface by refraction.

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Normally, only the direct sound is received. Refraction can add some additional sound Effectively amplifies the sound. Natural amplifiers can occur over cool lakes. (sound faster in warm air over lake)

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SLIDE 15

Superposition similarly with density waves!

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SLIDE 16
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Dispersion (mainly PH102) speed of wave depends on wavelength blue light waves are slower in glass take a longer path water: longer wavelengths travel faster!

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SLIDE 18

Diffraction (mainly PH102) depends on wavelength of light/water/ etc can use it to measure wavelengths

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This happens with sound too!

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Straight line propagation waves *can* travel in a straight line but they need not - standing waves

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SLIDE 24

Standing waves must meet special conditions geometry ...

L

for end points to be fixed:

nλ 2 = L

Position varies in time we will come back to this ...

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SLIDE 25

Doppler Effect: moving relative to waves

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in one period T, you move closer to the source by vsT the waves appear squashed together the apparent frequency (1/T) is still velocity / wavelength approaching the source

vs v

f = v λ − vsT = v v/f − vsT = v v/f − vs/f =

  • v

v − vs

  • f
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SLIDE 27

Approaching the source: pitch (freq) seems higher Moving away from source: pitch (freq) seems lower Only has to do with RELATIVE motion! e.g., ambulance - driver hears no change similarly: doesn’t matter who is moving

f =

  • v

v − vs

  • f

f =

  • v

v + vs

  • f

happens for light too - receding galaxies have “red shift” (lower freq)

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SLIDE 28

!"#$%&'#()*+,-#'$&./,-#&'#(0),1 23)4-,#5-&6&78#$33#"9'$:

Via relativity, it works with light too ... why ?

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Sound in air most sound = waves produced by vibrations of a material e.g., guitar string, saxophone reed, column of air

  • riginal vibration stimulates a larger one

sounding board sound = compression / rarefaction waves in a medium Density Waves

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MAX pressure = MIN velocity

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Sound carries ENERGY in density waves = pressure modulation P = F/ A = (F*d)/(A*d) = W/V = (energy)/(volume) variation of pressure = variation of energy density sound power = (energy)/(time) sound intensity = (power)/(unit area)

intensity ∼ 1 (dist)2 ∼ (pressure)2

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SLIDE 33
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sound intensity covers a huge range … use a log scale

dB = 10 log power reference

  • = 20 log

pressure reference

  • (power goes as pressure squared)

reference pressure = 20 μPa (tiny! atmosphere = 101,325 Pa) 1 Pa = 1 N/m2 pressure difference would be 94 dB !!

  • ur hearing: max & min pressures differ by a MILLION times

max/min power differs by a million times

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N S

Speaker cone forces surrounding air to compress/rarefy cone pushes nearby air molecules, which hit others ... learn about how it moves in PH102 (can use the opposite for a microphone …)

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How to transmit sound in a medium? must have a degree of ELASTITCITY i.e., a restoring force Solids bonds are like springs atoms respond to each other’s motions speed of sound <-> crystal structure bonding bond strength <-> speed of sound Liquids also true … but less so

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Gasses, like air? “restoring force”? creation of partial vacuum / lower pressure region air moves in to fill void Horribly inefficient Depends on PRESSURE of gas Depends on WHAT GAS vacuum (e.g., space) - nothing there to compress/ expand (solid in vacuum … still OK)

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Result: sound is really slow in air faster in : Warm air (0.6 m/s per oC) Humid air (slightly) about one MILLIONTH light speed e.g.., golf ball struck 500m away light: sound:

δtlight = δx c ≈ 1.6 µsec δtsound = δx 340 m/s ≈ 1.5 sec

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Sound can be REFLECTED like other waves Reverberation different paths from source to observer are possible slight difference in path length = time lag Yuck.

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For good sound, this effect must be optimized walls too reflective: reverb problems walls too reflective: “ dead” sound, low level reflected sound = “lively” & “full” … like in the shower Best: parabolic or elliptical reflector

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a.k.a. “whispering gallery” parabolic or elliptical room

  • St. Paul’s cathedral

London can hear a whisper across the room

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Natural (resonance) frequencies

  • bjects have characteristic vibration modes - unique sounds

composition shape density elasticity e.g., string <- depends on all these

nλ 2 = L

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geometry dictates allowed frequencies fundamental + overtones (harmonics)

L = nλ 2 and λf = v =⇒ L = nv 2f =⇒ f = nv 2L

guitar strings: frets change L what is the velocity v ???

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Velocity is related to: T = Tension (force) μ = mass per unit length (weight)

v =

  • T

µ f = n 2L

  • T

µ

string fixed at both ends change L via FRETS shorter = higher pitch tune via TENSION tighter = higher pitch range via MASS thinner = higher pitch (same deal for a piano, less the frets)

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SLIDE 48

fundamental (n=1) 1st overtone / 2nd harmonic (n=2) 3rd harmonic (n=3) 4th harmonic (n=4) ... ... it is different if ends are not fixed!

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example: air columns (pipe organ) we can set up resonance in a fixed tube of air pipe open at both ends STANDING WAVES set up in tube need nodes at the ends max velocity zero pressure difference math? same as for the string

f = nv 2L

v = 340 m/s for air at RT

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Things are different when we close one end of the pipe! air velocity is ZERO at one end! effectively, twice as long pitch is twice as low

f = nv 4L

(now n must be ODD for waves to fit)

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OPEN - OPEN pipes : like strings, all harmonics present OPEN - CLOSED pipes : only ODD harmonics, 2x lower pitch presence (or absence) of harmonics changes “tone” waveform = sum of fundamental + harmonics!

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A clarinet is CLOSED on one end

  • nly odd harmonics

“warm” & “ dark” compared to saxophone - all harmonics

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Pitch and frequency

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What about a tuning fork? (or any 3D solid) fit wavelengths in each dimension Lx Ly Lz

f = v 2 l L x

  • +

m L y

  • +

n L z

  • l, m, n are integers

Aluminum : v = 4900m/s say, 1 x 1 x 0.5cm block f = 3500 Hz = A7 (3 octaves above middle C)

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Interference two sound waves of different frequencies alternating constructive and destructive interference causes the sound to “beat” beat frequency = difference in frequency of the two waves.

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beats

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sweep

  • ne

generator