24
Physics for Scientists and Engineers II , Summer Semester 2009 1 Lecture 22: July 15 th 2009 Physics for Scientists and Engineers II

Lecture 22: July 15 th 2009

  • Upload
    saskia

  • View
    19

  • Download
    0

Embed Size (px)

DESCRIPTION

Lecture 22: July 15 th 2009. Physics for Scientists and Engineers II. Momentum and Radiation Pressure. + + + +. Antennas. The Half Wave Antenna. Source of alternating voltage having frequency f = c / l. Conducting rods. - - - -. + + + +. - - - -. - PowerPoint PPT Presentation

Citation preview

Page 1: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

1

Lecture 22: July 15th 2009

Physics for Scientists and Engineers II

Page 2: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

2

Momentum and Radiation Pressure

c

2I

c

2SP and

2p :reflection completeFor

power)not pressure, is here P :(Note

)absorption (completec

I

c

S

c

1

A

1

A

1

A

FP

)pressure"radiation ("radiation by the surface on the exerted is P pressureA

)absorption (completep

:magnitude a has surface the todtransporte

p momentum the,S lar toperpendicu surface aby absorbed totally is T If

unit time.per p momentum and Tenergy carriesradiation neticElectromag

avg

avg

ER

ER

c

T

A

dtdT

c

T

dt

d

dt

dp

c

T

ER

ER

ER

ER

Page 3: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

3

Antennas

.radiation) (emenergy radiatesit s,accelerate particle charged aWhenever

fields. varying- timeproduce toneeded charges dAccelerate

radiation. neticelectromag produce to

fields varying- timeneed that weus tellequations sMaxwell'

fields magneticconstant Produce :currentsConstant

fields electricconstant Produce :charges Stationary

++

+

+

-

-

--

4

4

The Half Wave Antenna

Source of alternating voltage having frequency f = c /

Conducting rods

Page 4: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

4

Driving the resonance frequency of the antenna ----???

current).greater fields, electric(greater amplitudeshigher with occurs Resonance

).2L

c(f antenna theoffrequency n oscillatio-self the toequalfrequency a

with voltagegalternatinan applyingby n oscillatiodriven a createcan You

++

+

+

-

-

--

E

I

I

BS

E

BS

Snapshot in time:

Separation of charges creates an electricfield like that of a dipole: Given the name “Dipole antenna”

time.and spacein points allat EB

Page 5: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

5

Driving the resonance frequency of the antenna

++

+

+

-

-

--

E

I

I

B

flows)energy in which

direction theg(indicatin S

E

BS

Snapshot in time:

maximum). aat are rods theof endsouter at the

charges the0,I when (e.g., phase ofout 90 are and

time.and spacein points allat

BE

EB

Page 6: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

6

Voltage and Current Distribution

IV IV

IV IV

Page 7: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

7

Driving the resonance frequency of the antenna

IV

Page 8: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

8

The “near field” (dipole field) behavior

++

+

+

-

-

--

E

I

I

B

E

BS

++

+

+

-

-

--

E

I

I

B

E

BS

S

ant.insignific becomesquickly and r

1 toalproportion of falls

field)(near field dipole The No! ???energy of flownet no

inward flowingEnergy

direction reverses vector Poynting

:reversescurrent theereafter,Shortly th

3

Page 9: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

9

The “far field” behavior

2

0000

r

1 toalproportionintensity loosesradiation

r

1 toalproportion are B and E

phase.in aremanner in this produced fields electric and magnetic The

law Maxwell-Ampere B

law sFaraday'sdE

toaccording versa viceand field magnetic varying

- timeinduce fields electric varying- timedistanceslarger At

dt

dIIIsd

dt

d

Ed

B

Page 10: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

10

Angular dependence of radiation intensity

S

2

2sin :Radiation ofIntensity

rSI avg

equally. mattersn orientatioradiation, receive toantennaan using when Similarly,

S

Page 11: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

11

Angular dependence of radiation intensity

equally. mattersn orientatioradiation, receive toantennaan using when Similarly,

SSender

SenderS

E

reception Good

reception No

SSender

B

reception No

B

E

antenna toparallel be should E

Page 12: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

12

Electromagnetic Spectrum

Page 13: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

13

The Nature of Light

Newton: Light = Stream of Particles (can explain reflection and refraction)

1678 Christian Huygens : Showed that a wave model of light can also explain reflection and refraction.

1801 Thomas Young: Experimental demonstration of the wave nature of light (Double slit experiment “Interference” effects)

Maxwell: Light = high frequency electromagnetic wave

Hertz: Confirms existence of electromagnetic waves …..but also discovers the photoelectric effect (contradicts the wave model, which predicts: more light intensity = more energy transferred to electrons)

Einstein 1905: Proposes that energy of light wave is present in particles called photons. E=hf is the energy of a photon (explains photoelectric

effect).

Page 14: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

14

Measuring the speed of light

Galileo: Using lanterns between mountains didn’t work. The light is too fast.

1675: Ole Roemer found that the period of revolution of the moon Io around Jupiter depends on whether the earth is receding from or moving towards Jupiter (longer period when earth is receding). From these data Huygens calculated c > 2.3 x 108 m/s

1849: Fizeau’s method (toothed wheel): c = 3.1 x 108 m/s

Currently accepted value: c = 2.997 9 x 108 m/s

Page 15: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

15

Eclipse Time Delay of Io in the shadow of Jupiter

Roemer’s method

Sun

Iobeingeclipsedby Jupiter

Jupiter

In this position, the time of the eclipseis delayed by many minutescompared to the opposite positionof the earth.

delay

earthsun

t

Rc

2

Page 16: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

16

Ray Approximation in Geometric Optics

Geometrical Optics The study of the propagation of light under these assumptions:1) In a uniform medium light travels in a straight line. 2) Light changes direction in a medium with non-uniform optical properties, or at the interface between two media.

The “Ray approximation”:Wave moving through a mediumtravels in a straight line in thedirection of it’s rays.

Rays

Wave fronts

Page 17: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

17

Ray Approximation in Geometric Optics

Encountering barriers (like an opening in a wall):

The ray approximation is valid if << d, where d is the size of the opening.

d

Wave continues in a straight line

d Diffraction occurs

Opening acts like a point source of a wave.

Page 18: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

18

Reflection of Light/Wave

NormalIncident Ray Reflected Ray

1 '1

incidence of Angle reflection of Angle1

'1

Page 19: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

19

Specular and Diffuse Reflection

Specular reflection“Smooth surface”

Diffuse reflection

surfacein Variations

Page 20: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

20

The Wave under Refraction

NormalIncident Ray Reflected Ray

21 '1

2Refracted Ray

Air

Glass

Angle of Refraction

12 vv

1v

Page 21: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

21

The Wave under Refraction

Incident Ray, Reflected Ray, and Refracted ray are all in one plane.

1 mediumin light of Speed

2 mediumin light of Speed

sin

sin

1

2

1

2 v

v

Page 22: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

22

The Wave under Refraction

NormalIncident Ray Reflected Ray

1 '1

12 Refracted Ray

Air

Glass

Angle of Refraction

12 vv

1v

Page 23: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

23

Index of Refraction – not yet covered in class but needed for HW 16

v

c

medium ain light of speed

in vacuumlight of speedn: Refraction ofIndex

1n :mediaother All

1n :For vacuum vacuum

n

n

nnn

n

nc

nc

v

v

fv

fv

fvfvfff

22111

2

2

1

2

1

2

1

2

1

221121

changes.ngth but wavele constant, remainsfrequency

:medium a enterslight When

Wavelength in vacuum

Wavelength in medium

n

Page 24: Lecture 22: July 15 th   2009

Physics for Scientists and Engineers II , Summer Semester 2009

24

Snell’s Law of Refraction – not yet covered in class but needed for HW 16.

2211

2

1

1

2

1

2

sinnsinn

n

n

sin

sin

v

v

Snell’s Law of Refraction