Title: Antennas: from Theory to Practice 3. Field Concepts and Radio Waves
1Antennas from Theory to Practice3. Field
Concepts and Radio Waves
- Yi HUANG
- Department of Electrical Engineering
Electronics - The University of Liverpool
- Liverpool L69 3GJ
- Email Yi.Huang_at_liv.ac.uk
2Objectives of This Chapter
- Use Maxwells equations to obtain wave solutions.
- Introduce the concepts of the plane wave,
intrinsic impedance, and polarisation - Discuss radio propagation mechanisms and
propagation characteristics in various media - Review basic radio propagation models
- Compare the circuit concepts and field concepts
- Examine the concept of skin depth from both the
field and circuit points of views.
33.1 Wave Equation and Solutions
For a time harmonic case the time factor is
Maxwells equations
4In source free region, we obtain the wave equation
A solution is
5For the loss-free case,
the velocity of an electromagnetic wave
(including light) in free space is about
30,000,000 m/s
63.2 Plane Wave, Intrinsic Impedance and
Polarisation
Plane wave
H ? E? z
The power density
7Polarisation is described by the locus of the
tip of the E vector as time progresses. For a
wave propagating towards z-direction
y
y
E
E
E
x
x
Circular a b
Linear a or b 0
Elliptical Axial ratio a/b
Note there are RCP and LCP
8Intrinsic impedance of the material is defined as
the ratio of the electric and magnetic fields. In
a loss-free medium
In free space
Generally speaking
93.3 Radiowave Propagation Mechanisms
- Reflection and transmission
Snells law
Reflection and transmission coefficients
How to obtain them?
10Two principal polarisations
To obtain the reflection and transmission
coefficients, we introduce equivalent
transmission line model
11The characteristic Impedances are
Thus
From the power point of view
12Example 3.1
- Perfect conductor obtain the reflection and
transmission coefficients between air and a
perfect conductor.
The conductivity of a perfect conductor is
infinite the characteristic impedance of its
equivalent transmission line is zero for any
polarisation and incident angle, i.e. Z2 0,
thus
13Example 3.2
- Ground if the relative permittivity of a ground
is 9 and the conductivity is very small and
negligible, plot the reflection coefficient as a
function of the incident angle for both parallel
and perpendicular polarisations.
14Brewsters angle
- For parallel polarisation, the reflection
coefficient vanishes ( 0) at a particular
incident angle, this angle is called Brewsters
angle - When the incident angle is greater than the
Brewsters angle for parallel polarisation,
15- The critical angle is the incident angle that
gives a transmitted angle of 90 degrees when the
wave is from a dense medium to a less dense
medium, such as from water into air. From Snells
law, we obtain this special angle - For non-normal incidence, the reflection
coefficients are different for the two principle
polarisations. As a result, if an incident wave
is a combination of these two orthogonal waves,
the combined signal after the reflection will be
changed. e.g., for a conductor RCP wave becomes
a LCP wave!
16Radio propagation through a wall
17Example 3.3
- A brick wall has a relative permittivity of 4 and
a thickness of 20 cm, the loss is negligible. - a). If the operational frequency is 2.45 GHz for
wireless applications (such as bluetooth), plot
the reflection coefficient as a function of the
incident angle for both parallel and
perpendicular polarisations. - b). If the incident angle is 45 degrees, plot the
reflection coefficient as a function of the
frequency for both parallel and perpendicular
polarisations.
18The reflection is minimised when the thickness of
the wall is an integer of half of the effective
wavelength.
19Diffraction and Huygenss Principle
Huygens Principle states that each point on a
primary wave front can be considered as a new
source of a secondary spherical wave. The
relative (to the direct ray) power density
20Scattering
- Unlike the other propagation mechanisms where the
size of the medium or the obstacle is much larger
than the wavelength, scattering occurs when the
obstacle is comparable or even small than the
wavelength. - In scattering, there are no energy transformation
results, only a change in the spatial
distribution of the radiation.
213.4 Radio Wave Propagation Characteristics in
Media
This classification is useful for evaluating the
EM properties in terms of the loss tangent but is
not accurate for classifying whether a medium is
lossy or not!
22A more accurate consideration should take the
complex permittivity spectrum into account
23Propagation Through the Ionosphere
- The ionosphere is the region above the
troposphere (where the air is), from about 80 to
400 km above the earth. It is a collection of
ions, which are atoms that have some of their
electrons stripped off leaving two or more
electrically charged objects. The sun's rays
cause the ions to form which slowly recombine. - Reflection at low frequencies (up to about 30
MHz). - Scattering, refraction and absorption when high
frequency waves (above 100 MHz) pass through it. - Faraday rotation the wave polarisation
plane/line is rotated through the ionosphere .
24Propagation in Rain
- The major effect of rain on radiowaves is
attenuation due to absorption and scattering over
a wide range of the spectrum
where R is the rain rate in mm/h, and a and b are
constants that depend on frequency and
temperature of the rain.
253.5 Radio Wave Propagation Models
Received power
Path loss
26Two-ray Model/Plane Earth Model
The 1st Fresnel zone Path-loss (not a
function of freq) 20 dB/dec, d lt Df
Received power
40 dB/dec, d gt Df
Path-loss
27Multipath Models
- No analytical equations to give an accurate
prediction of the radio propagation pathloss. - Empirical and statistical representations are
available for various scenarios. - Most of the popular outdoor pathloss prediction
tools are based on Okumura and Hatas formulation - based on measured data for 100 MHz and 3 GHz
- General form for pathloss
1.5 lt n lt 4 0 lt X lt 20
28- Multipath fast fading the received signal
changes significantly (gt 30 dB) over a very short
distance (few wavelengths), resulted from the
complex and vector summation of signals. - Delay spread multi-copies of the original signal
arrive at the destination at different time
through different paths, which may cause
dispersion and inter-symbol interference - The delay spread is often employed to define the
channels coherence bandwidth BC (similar to a
filters bandwidth in certain sense). - Doppler frequency shift is employed to define the
channels coherence time Tc
29Fading channels
Freq selective
Signal BW
Freq selective
Slow fading
Fast fading
Bc
Flat
Flat
Slow fading
Fast fading
Tc
Pulse duration
- Typical values of RMS delay spread is,
- 2 ms for outdoor urban cellular (Bc 100kHz)
- 100 ns for indoor environment (Bc 2MHz)
30- Statistically, the power density function (PDF)
of the received (short-term) signal envelope
follows certain distribution - When there is a line-of-sight ray, it follows the
Gaussian distribution and this channel is
therefore called the Gaussian channel - When there is a partial line-of-sight ray (the
path is partially blocked by obstacles such as
trees), it follows the Rician distribution and
this channel is therefore called the Rician
channel - When there is no line-of-sight ray, it follows
the Rayleigh distribution and this channel is
therefore called the Rayleigh channel.
313.6 Comparison of Circuit Concepts and Field
Concepts
32Correspondence of the Circuit Concepts and the
Field Concepts
33Skin Depth d
- Field concept skin depth is defined as the
distance d through which the amplitude of a
traveling plane wave decreases by factor 1/e, or
37, or 8.686 dB over one skin depth - Circuit concept skin depth is defined as the
depth below the surface of the conductor at which
the current density decays to 1/e (about 37) of
the current density at the surface. The per unit
resistance of a wire
34Skin depth and resistance of a gold track of
dimensions 7mm x 16mm x 30000mm