Different Transmission Systems Microwave Frequency Features of Radio Transmission Radio Frequency Spectrum Utilization Radio Wave Propagation Fading Interference Microwave Radio Link Relay station (Passive)
Different Transmission Systems Coaxial cable
Microwave link
MUX
MUX
Satellite
Fiber optic cable
Microwave Frequency Frequency: 300MHZ~ 300GHZ
Frequency band: UHF: 0.3-1.12G KU: 12.4-18G S: 2.6-3.95 G U: 40-60G
LF
MF
HF
VHF
Wavelength: 1m~1mm
X: 8.2-12.4G LS: 1.7-2.6 G Ka: 26.5-40G XC: 5.85-8.2G
UHF
SHF
L: 1.12-1.7G K: 18-26G C: 3.95-5.85G
EHF
microwave
10Km
1Km
100m
10m
f
30KHz
300KHz
3MHz
30MHz
1m 300MHz
10cm 3GHz
1cm 30GHz
1mm 300GHz
Features of Radio transmission 1
Wavelength is short while frequency is high.
2
Wide frequency band
3
Line of sight propagation, reflection, diffraction and scattering
4
Free space loss
5
Fading caused by other types of path loss.
6
Interference
Radio Frequency Spectrum Utilization (1)
Regional network 1.5 2.5
2 8 34 Mbit/s
3.3 11 GHz National backbone network Regional and local network
34 140 155 Mbit/s
1
2
3
4
5
2 8 34 140 155 Mbit/s 8
10
20
GHz 30
40
50
Radio Frequency Spectrum Utilization (2) Low frequency band
High frequency band
Channel number 1
2
n
1'
2'
n'
F3
Fo Frequency F1 F2 Band width Fo: Center frequency
Radio Wave Propagation (1) The radio link propagation follows the line of sight: it requires a perfect clearing between transmitting and receiving antennas. The propagation medium is made of the lower layers of the atmosphere (a few meters to a few hundred of meters above ground)
The non homogeneity of the atmosphere influences the waves propagation: 1°) Path curvature 2°) Reflecting, diverging, focusing intermittent events Free space loss (Lfs)=92.4+20×log(f×d) (dB) f:GHz, d:km
Radio Wave Propagation (2) Atmosphere influence
Refraction
Partial reflection
Absorption Gaz and water vapor
Diffusion Diffusion volume
n2
n2
Frequ. < 15 GHz : insignificant 20 GHz : 0.1 dB / km
i.2
Rain i.1
n1
n1
Frequ. > ?10 GHzo
500Km
n1×sin i.1 = n2×sin i.2
Almost horizontal
Radio Wave Propagation (3) Ground influence
Diffraction Reflection
Diffraction on a ridge
Spherical diffraction
Radio Wave Propagation (4) Air refraction index at sea level: n = 1.000 315 N
N = 315 N units
h
Standard atmosphere
h
Ro Real Earth
N = - 39 N.units Km
K = R/Ro = 4/3
R Imaginary Earth
N : Gradient of air refraction index
N may reach more extreme values than + 250 or - 350, during short percentage of time
An imaginary earth with the radius of 8500km, allows to simplify analysis on Refraction propagation of radio wave.
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