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22 Radio Engineering for Wireless Communication and Sensor Applications

In radio engineering we often consider a case where we have an interface with a good conductor. Fields penetrate only a short distance into a good conductor such as metal and not at all into a perfect conductor (s = ∞). We often approximate a good conductor with a perfect conductor, which is lossless. The boundary conditions at the interface of a dielectric and a perfect conductor are:

n × E = 0

(2.42)

n × H = Js

(2.43)

n ? D = r s

(2.44)

n ? B = 0

(2.45)

Such a boundary is also called an electric wall. Dual to the electric wall is the magnetic wall, where the tangential component of H vanishes.

2.4 Helmholtz Equation and Its Plane Wave Solution

In a source-free ( r = 0, J = 0), linear, and isotropic medium, Maxwell’s equations are simplified into the following forms:

= ? E = 0

(2.46)

= ? H = 0

(2.47)

= × E = −jvm H

(2.48)

= × H = jve E

(2.49)

When the = × operator is applied on both sides of (2.48), we obtain in a homogeneous medium

= × = × E = −jvm = × H

(2.50)

which leads, after utilizing vector identity

= × = × A = =(= ? A) − =2A

(2.51)

and (2.46), to

=2E = −v2meE = −k 2E

(2.52)

Fundamentals of Electromagnetic Fields

23

This equation is called the Helmholtz equation, which is a special case of the wave equation

=2E me

2E

= 0

(2.53)

 

t 2

 

 

The constant k = v me is called the wave number [1/m].

Let us first consider propagation of a wave in a lossless medium, where er and m r are real. Then k is also real. Let us assume that the electric field has only the x component, that the field is uniform in the x and y directions, and that the wave propagates in the z direction. The Helmholtz equation reduces to

2E x

+ k

2

E x = 0

(2.54)

 

z 2

 

 

 

 

 

 

The solution of this equation is

 

 

 

 

E x (z ) = E +e jkz + E e jkz

(2.55)

where E + and E are arbitrary amplitudes of waves propagating into the +z and z directions, respectively. The exact values of E + and E are determined by the sources and the boundary conditions. In the time domain, (2.55) can be rewritten as

E x (z , t ) = E + cos (vt kz ) + E cos (vt + kz )

(2.56)

where E + and E are now real constants.

The magnetic field of a plane wave can be solved from (2.49). The

result is

 

 

 

Hy =

1

(E +e jkz E e jkz )

(2.57)

h

 

 

 

that is, the magnetic field has a component that is perpendicular to the electric field and to the direction of propagation. The ratio of the electric and magnetic fields is called the wave impedance, and it is h = m /e . In vacuum h0 = m0 /e0 120pV ≈ 377V. Figure 2.5 illustrates a plane

24 Radio Engineering for Wireless Communication and Sensor Applications

Figure 2.5 Plane wave propagating into the +z direction.

wave propagating into the +z direction. The fields of a plane wave repeat themselves periodically in the z direction; the wavelength is

l =

2p

=

2p

=

1

 

(2.58)

k

v

 

 

f

 

 

me

me

The propagation velocity of the wave is

v = f l =

1

(2.59)

me

In a vacuum, the propagation velocity is the speed of light:

v = c =

1

2.998

× 108 m/s

(2.60)

 

 

m0 e0

 

 

 

 

In a lossy medium having conductivity s, Maxwell’s III and IV equations (the curl equations) are

= × E = −jvmH

(2.61)

= × H = sE + jveE

(2.62)

Now the Helmholtz equation gets the following form:

 

=2E + v 2me S1 j

s

DE = 0

(2.63)

ve

Fundamentals of Electromagnetic Fields

25

Compared to (2.52), here jk is replaced by a complex propagation constant,

 

 

 

s

 

g = a + jb = jv me 1 j

(2.64)

 

ve

where a is the attenuation constant and b is the phase constant. In the case of a plane wave propagating into the z direction, we have

2E x

g

2

E x = 0

(2.65)

z 2

 

 

 

 

 

leading to

E x (z ) = E +e gz + E e gz

(2.66)

In the time domain

E x (z , t ) = E +e az cos (v t bz ) + E e az cos (vt + b z )

In the case of a good conductor, that is, when s >> ve , we the propagation constant as

 

 

 

s

 

vms

g = a + jb jv me

= (1 + j )

 

 

jve

2

(2.67)

obtain

(2.68)

When a plane wave meets a surface of a lossy medium in the perpendicular direction and penetrates into it, its field is damped into 1/e part over a distance called the skin depth:

ds =

1

=

 

2

(2.69)

a

vms

 

 

 

Example 2.1

Find the attenuation of a 4 mm-thick copper layer at 10 GHz.

Solution

At a frequency of 10 GHz the skin depth in pure copper (s = 5.8 × 107 S/m, m = m 0 ) is only 6.6 × 107 m. Therefore, at this frequency a uniform