Wave Lecture (narrows bridge: wave lecture intro: ( bill nye: waves.

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Wave Lecture (narrows bridge: http://www.youtube.com/watch? v=xox9BVSu7Ok) wave lecture intro: (http://www.youtube.com/watch? v=jAXx0018QCc) bill nye: waves (http://www.youtube.com/watch? v=OGyRe_SGnck)

Transcript of Wave Lecture (narrows bridge: wave lecture intro: ( bill nye: waves.

Page 1: Wave Lecture (narrows bridge:  wave lecture intro: ( bill nye: waves.

Wave Lecture(narrows bridge: http://www.youtube.com/watch?

v=xox9BVSu7Ok)wave lecture intro: (http://www.youtube.com/watch?

v=jAXx0018QCc)bill nye: waves

(http://www.youtube.com/watch?v=OGyRe_SGnck)

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1. Wave properties

A. waves are the transfer of kinetic energy through a medium or vacuum:

-sound though air,

-light through space: vacuum

-heat through a metal pan: solid

B. when waves travel through matter:

1. it transfers kinetic energy

2. but medium/matter remains in place:

-grass blades waving in the wind,

-sound through walls

- ocean waves

3. the energy in motion carries information: sound, pictures and numbers

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matter remains in place: net circular motion

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C. waves have a repeating cycle (back-and- forth), called an oscillator,

-like a person on a swing (pendulum) or

-a vibrating string on a guitar

1. repeating motion is also called harmonic:

heartbeat,

solar seasons,

singing in

harmony

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Harmonic wave motion

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2. one full revolution is called a cycle,

known as one unit of harmonic motion

3. waves move around a point of equilibrium: where the system is at “rest”, with a net force of zero

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D. energy/inertia pulls the wave away from equilibrium and the restoring force brings the wave back to the point of equilibrium:

= restoring force

= equilibrium

Demo Newton’s cradle:Newton’s first law

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E. wave part/labels

1. crest: top of the wave

2. trough: bottom of the wave

3. equilibrium: half way between crest and trough

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F. wavelength: distance from crest to crest,

(or trough to trough)

- Greek symbol lambda, = upside down y:

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G. amplitude: size of a wave (cycle)

1. wave height from point of equilibrium to top of crest (or half wave height from

trough to crest)

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2. amplitude will reduce (dampen) toward equilibrium with less wave energy

-direct relationship

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H. frequency: how often vibrations (wave cycles) occur

1. number waves per time:

-usually the number of wave crests per second

2. unit is the Hertz (Hz) = # waves

second

low frequency

high frequency

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I. radio waves:

-AM radio: alters amplitude of waves (height)

-FM radio: alters frequency of waves (how often)

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J. period: amount of time for a cycle: crest to crest (how much time for a class period?)

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K. frequency and period are inverse relationships:

period = 1

frequency

frequency = 1

period

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L. wave speed

1. within same medium = same speed

2. different densities of matter cause different wave speeds:

more dense =

more inertia =

slower wave speed

- an inverse relationship

3. greater the elasticity of the medium (ability to bounce back to original position), the faster the wave speed

- ie: steel faster than air: tap on a steel wall vs talking through air

- direct relationship

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4. wave speed =

-distance/time or

-frequency x wavelength =

(# waves/sec x distance crest to crest)

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2. Wave types

A. transverse waves (sine waves)

1. medium motion (oscillation) is perpendicular to the wave motion (up/down)

- as a water wave moves toward the shore, the crests/troughs move up

and down

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-examples of transverse waves:

light, heat, ocean/water, earthquake, Tacoma Narrows bridge

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B. longitudinal waves

1. medium motion in same direction (parallel) as wave motion (oscillation)

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2. waves of alternating regions of matter crowded together (compressions)

and matter spread apart: rarefactions

3. sound waves are longitudinal waves

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3. Wave interactions

- when energy waves move they are influenced by the boundaries they collide with and influence other waves they run into

A. reflection (as in a mirror image)

- wave/energy is not absorbed but bounced, how much depends the surfaces’ degree of absorption

- example: mirrors, barrier reefs, sound walls

- incoming wave angle (incident wave) =

outgoing wave angle (reflected)

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reflected wave: incident = reflected

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reflected waves: wavelength and frequency remain unchanged, usually (if energy is not absorbed)

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B. refraction

- bending of wave due to a change in speed- due to changing one medium to another

medium, thus changing density of the medium

-pencil in water:

- how would a pencil in oil look?

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light refraction from air to glass mediums (what album cover?):

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C. diffraction

-waves bending around or through an obstacle: sound traveling around a corner

-waves passing through a hole: changes to circular waves

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diffraction waves: circular waves produced: explains why sound can be heard through small opening.

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D. absorption

-waves can get smaller as they transfer energy into the medium they travel through:

ie: light passing through sunglasses, sound passing through sound boards in a recording studio

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E. wave to wave interference

- when two or more waves collide at the same point in space and time

1. constructive

a. wave crests meet and combine

b. form a single wave

c. amplitude is increased: additive of two original waves

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d. resonance

- when the natural frequency of an object matches the input wave frequency

- causes a dramatic increase of energy and thus an increase in amplitude of the generated wave:

-musical instruments

-Tacoma narrows bridge

-Calvary troops across marching across a footbridge in Manchester,England (1831)

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constructive interference

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2. destructive

a.when the crest of one wave meets the trough of a second wave

b. forms a single wave

c. amplitude is decreased: energy is subtracted

d. ie: anti-noise technology for earphones

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and so, the sun’s waves set yet again at the ocean waves, groovy!

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