29
W. Sautter 2007

W. Sautter 2007. These are also called Compressional Waves

Embed Size (px)

Citation preview

Page 1: W. Sautter 2007. These are also called Compressional Waves

W. Sautter 2007

Page 2: W. Sautter 2007. These are also called Compressional Waves

These are also calledCompressional Waves

Page 3: W. Sautter 2007. These are also called Compressional Waves

Crest

Trough

Compression Rarefaction Compression CompressionRarefaction Rarefaction

Trough

Crest

Rarefaction = low PressureCompression = high Pressure

Page 4: W. Sautter 2007. These are also called Compressional Waves

Wavelength

Frequency

Velocity Wavelength

Frequency

Velocity

vx =

Page 5: W. Sautter 2007. These are also called Compressional Waves

Wave A

Wave A

Wave A

Wave B

Wave B

Wave B

Constructive interference

Destructive interference

Partially Constructive interference

Page 6: W. Sautter 2007. These are also called Compressional Waves

Intensity = Power / Area

SoundSource

Sound radiates out from a source as concentric spheresand follows an Inverse Square function

Page 7: W. Sautter 2007. These are also called Compressional Waves

Inverse Square means as distance from the source doubles,the intensity 1/4 the original. If distance triples, the intensity

is 1/9 the original and so on.

The surface area of a sphere is given by 4 r2

Power is measured in watts ( 1 joule / second)

Intensity = Power / Area = watts/ 4 r2

Or Watts / meter2

Page 8: W. Sautter 2007. These are also called Compressional Waves

dB = 10 log ( I / I0 )

I = the intensity of the sound to be evaluatedI0 = intensity of lowest sound that can be heard

(1 x 10-12 watts / meter2)

Page 9: W. Sautter 2007. These are also called Compressional Waves

•SINCE LOGS ARE POWERS OF 10 THEY ARE USED JUST LIKE THE POWERS OF 10 ASSOCIATED WITH SCIENTIFIC NUMBERS.

•WHEN LOG VALUES ARE ADDED, THE NUMBERS THEY REPRESENT ARE MULTIPLIED.

•WHEN LOG VALUES ARE SUBTRACTED, THE NUMBERS THEY REPRESENT ARE DIVIDED

•WHEN LOGS ARE MULTIPLIED, THE NUMBERS THEY REPRESENT ARE RAISED TO POWERS

•WHEN LOGS ARE DIVIDED, THE ROOTS OF NUMBERS THEY REPRESENT ARE TAKEN.

Decibels are logarithmic functions

Page 10: W. Sautter 2007. These are also called Compressional Waves

• A LOGARITHM (LOG) IS A POWER OF 10. IF A NUMBER IS WRITTEN AS 10X THEN ITS LOG IS X.

• FOR EXAMPLE 100 COULD BE WRITTEN AS 102 THEREFORE THE LOG OF 100 IS 2.

• IN PHYSICS CALCULATIONS OFTEN SMALL NUMBERS ARE USED LIKE .0001 OR 10-4. THE LOG OF .0001 IS THEREFORE –4.

• FOR NUMBERS THAT ARE NOT NICE EVEN POWERS OF 10 A CALCULATOR IS USED TO FIND THE LOG VALUE. FOR EXAMPLE THE LOG OF .00345 IS –2.46 AS DETERMINED BY THE CALCULATOR.

Decibels are logarithmic functions

Page 11: W. Sautter 2007. These are also called Compressional Waves

Whisper 20 decibels Plane 120 decibels

Conversation 60 decibels Siren 100 decibels

Page 12: W. Sautter 2007. These are also called Compressional Waves

The frequency of a string depends on the Tension (N)and string Linear Density in kilograms per meter (Kg/m).

Light strings under high tension yield high frequencies.Heavy strings under low tension yield low frequencies.

Page 13: W. Sautter 2007. These are also called Compressional Waves

V (air) = 341 m/s at 20 oC

If observer is moving towards the source, V(observer) = +If observer is moving towards the source, V (observer) = -If source is moving towards the observer, V (source) = - If source is moving towards the observer, V (source) = +

Page 14: W. Sautter 2007. These are also called Compressional Waves

Slower at low temp

Faster at high temp

Page 15: W. Sautter 2007. These are also called Compressional Waves

0C

Page 16: W. Sautter 2007. These are also called Compressional Waves

Moving Towardsource

Moving Towardobserver Observed Frequency

Is higher

Page 17: W. Sautter 2007. These are also called Compressional Waves

Moving Away from

observer

Moving Away from

sourceObserved FrequencyIs lower

Page 18: W. Sautter 2007. These are also called Compressional Waves

Moving Away from

observerObserver

At restObserved FrequencyIs lower

Page 19: W. Sautter 2007. These are also called Compressional Waves

Moving Towardobserver

ObserverAt restObserved Frequency

Is higher

Page 20: W. Sautter 2007. These are also called Compressional Waves

1/2 1 3/2

Fundamental = 2 L Second Harmonic = L Third Harmonic = 2/3 L

Page 21: W. Sautter 2007. These are also called Compressional Waves

fundamental

fundamental

d = diameter of tubeL = length of tube at first resonant point

If d is small compared to L(which is often true) then:

Page 22: W. Sautter 2007. These are also called Compressional Waves

Since V = f

If velocity is constant thenas decreases, f increases

In the same ratio

Second Harmonic = L

Fundamental = 2 L

Third Harmonic = 2/3 L Third Harmonic =3 ffund

Fundamental f = ffund

Second Harmonic f = 2 ffund

Page 23: W. Sautter 2007. These are also called Compressional Waves

1/4 3/4 5/4

Fundamental = 4 L Second Harmonic = 4/3 L Third Harmonic = 4/5 L

Page 24: W. Sautter 2007. These are also called Compressional Waves

fundamental

fundamental

d = diameter of tubeL = length of tube at first resonant point

If d is small compared to L(which is often true) then:

Page 25: W. Sautter 2007. These are also called Compressional Waves

Since V = f

If velocity is constant thenas decreases, f increases

In the same ratio

Second Harmonic = 4/3 L

Fundamental = 4 L

Third Harmonic = 4/5 L Third Harmonic = 5 ffund

Fundamental f = ffund

Second Harmonic f = 3 ffund

Page 26: W. Sautter 2007. These are also called Compressional Waves

Fundamental = 2 L

Second Harmonic = L

Third Harmonic = 2/3 L

Fourth Harmonic = ½ LNode

Node

VIBRATIONAL MODES

Page 27: W. Sautter 2007. These are also called Compressional Waves

Since V = f

If velocity is constant thenas decreases, f increases

In the same ratio

Second Harmonic = L

Fundamental = 2 L

Third Harmonic = 2/3 L Third Harmonic = 3 ffund

Fundamental f = ffund

Second Harmonic f = 2 ffund

Page 28: W. Sautter 2007. These are also called Compressional Waves

Waves from aDistant source = crest

= trough

Barrier withTwo slits

In phase wavesEmerge from slits

Constructive interference

Destructiveinterference

Page 29: W. Sautter 2007. These are also called Compressional Waves