PHY4324/Fall 09: EM II HOMEWORK ASSIGNMENT #6: SOLUTIONS Instructor: D. L. Maslov

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PHY4324/Fall 09: EM II

HOMEWORK ASSIGNMENT #6: SOLUTIONS due by 11:45 p.m. Wednesday 10/15

Instructor: D. L. Maslov maslov@phys.ufl.edu 392-0513 Rm. 2114

Please help your instructor by doing your work neatly.

Every (algebraic) final result must be supplemented by a check of units. Without such a check, no more than 75% of the credit will be given even for an otherwise correct solution.

1. G9.10 [We did this problem in class but the problem is so good that it’s worth doing it again. Here is a link to the original 1901 paper by P. N. Lebedev describing his experiments on measuring the light pressure http://web.ihep.su/dbserv/compas/src/lebedev01/eng.pdf] [20 points]

Solution: The momentum density of the electromagnetic wave is P = I/c 2 .

Consider a slab of area A and height cdt.

Over time dt, all the momentum in this slab will fall on the surface. For a perfectly absorbing surface, the change in the momentum is P cdtA = ( I/c ) dtA.

Pressure is the force per unit are

P = I/c =

1 .

3 × 10 3

3 × 10 8

= 4 .

3 × 10

− 6

N/m

2

.

Atmospheric pressure is about 10 5 N/m 2 , so the pressure of light is about 4 .

3 × 10 − 11 reflecting surface, the pressure is twice bigger=8 .

6 × 10 − 6 N/m 2 atm. For a perfectly

2. G9.14 [25 points]

Solution: Let

E i

E r

E t

= E

0 i

= E

0 r

(cos α ˆ + sin α y )

= E

0 t

(cos β ˆ + sin β y ) .

From Faraday’s law, ∇ × E = − ∂ B /∂t → B = ( k × E ) /ω →

B

B i r

E t

=

= − ( k

1

× E ) /ω = −

E

0 r v

1

= (

E v

1 k

0 i

2

× E ) /ω =

E

0 t v

2

( −

( − cos β cos

ˆ

α ˆ + sin

+ sin β x ) .

α x )

The boundary conditions E 1

||

= E 2

|| coefficients of ˆ in the B field gives and B 1

||

1

= B 2

||

2

.

Equating the coefficients of ˆ in the E field and the

E

0 r sin α = E

0 t sin β

E

0 r

µ

1 sin v

1

α

= −

E

0 t

µ

2 sin β v

2

→ E

0 r sin α = −

µ

1

µ

2 v

1 v

2

E

0 t sin β.

These two equations are compatible only if α = β = 0 .

Q. E.D.

3. G9.33 [30 points]

Solution a)

1. Gauss’s law

∇ · E =

1 r sin θ

∂E

φ

∂φ

= 0 .

X

2. Use the Faraday’s law to find the magnetic field.

∂ B

∂t

= ∇ × E =

1 r sin θ

∂θ

(sin θE

φ

) ˆ −

1 r

∂r

( rE

φ

Denote u ≡ kr − ωt and observe that

∂r

∂ cos u = − k sin

∂r sin u = k cos u.

u

Then,

∂ B

∂t

=

1 r sin θ

E

0 r

2 sin θ cos θ cos u −

1 kr

× ( − k sin u + sin u kr 2

− cos u r sin u ˆ −

1 r

E

0 sin θ

Integrate over t using R dt cos u = − 1

ω sin u and R dt sin u = 1

ω cos u

B =

2 E

0 cos

ωr 2

θ 1 sin u + kr cos u ˆ +

E

0 sin θ

ωr

− k cos u + cos u kr 2

+ sin u r

3. Having found B , we can now check if the ”no monopoles” law is satisfied.

∇ · B = 0

∇ · B = r

1

2

= r

1

2

∂r

∂r

= r

2

B r

+

2 E

0 cos θ

1 r 2

2 E

0 cos θ

ω

ω k

∂ r sin θ ∂θ cos

1 sin u u

+

(sin θB

θ

)

1 kr cos u kr 2 cos u +

− sin r u

+

1

2 cos θE

0 r 2 ω

∂ r sin θ ∂θ

E

0 sin

2

θ

ωr

− k cos u + cos u kr 2

+ sin u r

− k cos u + cos u kr 2

+ sin u r

= 0 .

X

4. Check the Amp`ere’s law

(

∇ × B =

∇ × B =

∇ ×

1 c 2

B

)

E

∂t

φ

=

=

=

=

=

1 c 2

1 r

∂ E

∂t

∂r

( rB

θ

) −

∂B r

∂θ

1 r

∂r

1 r

∂θ

E

0 sin θ

ω

2 E

0 cos θ

ωr 2

− k cos u + cos u kr 2

+ sin u r sin u + cos kr u

1 E

0 sin θ r ω

+

2 E

0 sin θ

ωr 3 kE

0 sin θ

ωr k 2 sin u −

2 sin u r 2 k sin u + cos u sin u +

1 r kr cos u

− 2 cos u kr 3

+ k cos u r

1 c 2

E

0 sin θ r k 2

ω 2

ωE

0 sin θ kr

ω sin u +

ω kr k sin u + cos u =

1 r cos u =

1 c 2

ωE

0 sin θ kr kE

0 sin

ωr

θ k sin u +

1 r cos u k sin u +

1 r cos u = ( ∇ × B )

φ

.

X

2

3 b) Poynting vector

Recall that

S =

1

µ

0

E × B =

E

0 sin θ

µ

0 r

×

2 E

0 cos θ

ωr 2 sin u + cos u − sin kr u

1 kr cos u ˆ +

E

0 sin θ

ωr

− k cos u + cos u kr 2

+ sin u r

ˆ

ˆ form a right-handed triad so that ˆ ×

ˆ

= ˆ and ˆ × r = ˆ Then,

S =

=

E 2

0 sin 2

µ

0

ωr 2

θ

E 2

0 sin

µ

0

ωr

2

2

θ cos u − sin u kr sin u +

1 kr cos u cos u − sin u

− k cos u + kr cos u kr 2

+ sin u r

E 2

0 sin 2

µ

0

ωr 2

θ cos u sin u 1 −

1

( kr )

2

!

+

1 kr cos

2 u − sin

2 u

E 2

0 sin

µ

0

ωr

2

2

θ

!

− k cos 2 u +

1 r sin u cos u + cos 2 u kr 2

− sin u cos u k 2 r 3

+ cos u sin u

− r sin

2 u kr 2

.

Average over the period using h cos u sin u i = 0 , h cos

2 the ˆ component becomes equal to u i = h sin

2 u i = 1 / 2 .

The ˆ component of S vanishes while h S i = kE 2

0

2 µ

0 sin

2

ωr 2

θ

ˆ =

E 2

0 sin

2

2 µ

0 cr 2

θ c) Power

Z h S i· d a =

=

=

E 2

0

2 µ

0 c

πE

µ

0 c

2

0

Z

Z

1

− 1

Z Z sin

2

θ r 2 sin θdrdθdφ = r 2

Z

1

1 − x

2 dx =

2 πE 2

0

µ

0 c

0

πE

µ

0 c

2

0

1 − x

2

2 πE 2

0

µ

0 c

1 −

1

3

=

4 πE 2

0

.

X

3 µ

0 c

Z

π sin

3

θdθ

0 dx

4. G9.36 [25 points]

Solution

Substituting numbers into Eq. (9.199),

5.

T

− 1

=

=

1

4 (4 / 3) (1)

(

4

3

+ 1

2

+

49

48

+

85

(48) (36) sin

2

3 ωd

2 c

16

9

9

4

1 −

9

4

9

4

.

sin

2

3 ωd

2 c

)

Obviously, if T − 1 sin

2 3 ωd

2 c

= 1 .

So, is maximal, then T is minimal. The maximum of T − 1

T min

=

49

48

+

1

85

(48)(36)

≈ 0 .

935 .

is at

3 ωd

2 c

= π

2

(2 n + 1) , where

Likewise, when sin

2 3 ωd

2 c

= 0 , T − 1 reaches its minimum and T reaches its maximum

T max

=

48

49

≈ 0 .

980 .

Since Eq. (9.199) is unchanged if n

1 is replaced by n

3 and n

3 is replaced by the reverse direction is the same and the fish sees you as well as you see it.

n

1

, the transmission coefficient in

4

6.

Bonus: G9.34 [25 points]

Let r

12

= n

1

− n

2 n

1

+ n

2 be the (amplitude) reflection coefficient for the wave coming from medium 1 to medium 2. Similarly r

21

= − r

12

= n

2

− n

1 n

1

+ n

2 is the reflection coefficient for the wave coming from medium 2 to medium 1, and r

23

= n

2

− n

3 n

2

+ n

3 is the same for the wave coming from medium 2 to medium 3. Also, t

12

= n

1

2 n

1

+ n

2 is the (amplitude) transmission coefficient for a wave coming from medium 2 to medium 3, and t

23

= n

2

2 n

2

+ n

3 is the same for the wave coming from medium 2 to medium 3. Choose the amplitude of the incident wave to be equal E

0

.

Follow the ”trajectory” of the wave after a couple of reflections. The first transmitted wave has the amplitude t

12 t

23 and it has traveled through glass once, so it accumulated the phase factor e ik

2 d , where k

2

= ωn

2

/c.

The wave reflected from the right inner surface of the glass has an amplitude t a phase factor e ik

2 d

12 r

23 and

.

After reflection from the inner left surface of glass, the amplitude of the wave changes to t

12

P r

23

.

The net amplitude of the second wave coming from glass is t

12 is t

12 t e 5 ik

2 d

.

The next transmitted wave

, etc. Summing up transmitted waves with the help of the formula for geometric series n =0 r

21

, and one more passage through the right inner glass surface adds a factor of t

23 t

23 r

21 r

23 and a phase factor of e 3 ik

2 d

23 x n r 2

21 r 2

23

= 1 / (1 − x ), we get

E t

= E

0 t

12 t

23 e ik

2 d

= E

0 t

12 t

23 e ik

2 d

+ t

12 t

23 r

21 r

23 e

3 ik

2 d

+ t

12 t

23 r

2

21 r

2

23 e

5 ik

2 d

1 + r

21 r

23 e 2 ik

2 d + r 2

21 r 2

23 e 4 ik

2 d + . . .

+ . . .

t

12 t

23 e ik

2 d

= E

0

1 − r

21 r

23 e 2 ik

2 d

.

The intensity of the wave is | E | 2 /vµ

0

, so the energy transmission coefficient is

T =

| E t

| 2 v

3

:

| E

1

|

2 v

1

= n

3 n

1 t

12 t

23 e ik

2 d

1 − r

21 r

23 e 2 ik

2 d

2

= n

3 n

1

1 + r 2

21 r 2

23 t 2

12 t 2

23

− 2 r

21 r

23 cos (2 k

2 d )

.

The rest is just some algebra.

T = 16 n n

3

1 n 2

1 n 2

2

( n

1

+ n

2

)

2

( n

2

+ n

3

)

2

1 + n

2 n

1

− n

1

+ n

2

2 n

2

− n

3 n

2

+ n

3

1

2

− 2 n

2 n

1

− n

1

+ n

2 n

2

− n

3 n

2

+ n

3 cos (2 k

2 d )

= 16 n

=

1 n

3 n

2

2

( n

1

+ n

2

)

2

( n

2

+ n

3

)

2

1

+ ( n

2

− n

1

)

2

( n

2

− n

3

)

2

− 2 ( n 2

2

− n 2

1

) ( n 2

2

( n

1

+ n

2

)

2

( n

2

+ n

3

)

2

+ ( n

2

− n

1

)

2

(

16 n

1 n

3 n 2

2 n

2

− n

3

)

2

− 2 ( n 2

2

− n 2

1

) ( n 2

2

− n 2

3

− n

) 1 − 2 sin

2

2

3

) cos (2 k

2 d k

2 d )

=

( n

1

+ n

2

)

2

( n

2

+ n

3

)

2

16 n

1 n

3 n 2

2

+ ( n

2

− n

1

)

2

( n

2

− n

3

)

2

− 2 ( n 2

2

− n 2

1

) ( n 2

2

− n 2

3

) + 4 ( n 2

2

− n 2

1

) ( n 2

2

− n 2

3

) sin

2 k

2 d

FIG. 1: Problem 5. Notice that the directions of the wave propagation are drawn at an angle to the slab only to avoid cluttering the plot. In reality, the incidence is normal.

1 2 3

5 t12 t12t23exp(ik2d) t12r23 t12r23r21 t12t23r23r21exp(3ik2d) t12t23(r23r21)^2exp(5ik2d)

Denoting α = n

1

+ n

2

, β = n

2

+ n

3

, γ = n

2

− n

1

, δ = n

2

− n

3

, we have

( n

1

+ n

2

)

2

( n

2

+ n

3

)

2

+ ( n

2

− n

1

)

2

( n

2

+ n

3

)

2

− 2 n

2

2

− n

2

1 n

2

2

− n

2

3

= α 2 β 2

= n

1 n

2

+ γ 2 δ 2

+ n

2

2

+

− n

2

1

αγβδ n

3

+ n

= (

2 n

3

αβ

− n

2

2

γδ ) 2

+ n

1

= [( n

1 n

2

+ n

+ n

2

2 n

3

) ( n

2

+ n

3

) − ( n

2

2

− n

1

) ( n

2

− n

1 n

3

= 4 [ n

1 n

2

+ n

2 n

3

]

2

− n

3

)]

2

= 4 n

2

2

( n

1

+ n

3

)

2

.

Substituting this back into T, we get

T =

( n

1

+ n

3

)

2

+

4 n

1 n

3

( n 2

2

− n 2

1

)( n 2

2 n 2

2

− n 2

3

) sin

2 k

2 d

.

X

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