2010 Radio
2010 Radio
2010 Radio
STRUCTURE OF AN ATOM
THERE ARE 108 ELEMENTS IN NATURE
ATOMS ARE THE SMALLEST PARTICLE OF AN
ELEMENT THAT SHOWS ITS PROPERTIES.
ATOMS
NUCLEUS
B)
ORBITS
BOHRS ATOM
NUCLEUS
THE CENTRAL PART OF THE ATOM
CONTAINS :
PROTONS
( + ve CHARGE )
NEUTRONS
( NEUTRAL )
ORBITS
OUTER PART OF THE ATOM
CONTAINS ELECTRONS WHICH HAVE
A - ve CHARGE.
MASS OF ELECTRON IS NEGLIGIBLE.
CHARGE IS EQUAL AND OPPOSITE TO
THAT OF A PROTON.
ATOMIC NO = NO OF PROTONS
= NO OF ELECTRONS
ATOM
CONSTITUEN
T
SYMBOL
CHARGE
MASS
ELECTRONS
E-
-1
9.1 X 10-28 G
PROTONS
P+
+1
NEUTRONS
APPROXIMATELY THAT
OF P+
ELECTROMOTIVE FORCE
FOR A CHARGE TO FLOW THROUGH, A
CONDUCTOR REQUIRES A FORCE.
THIS FORCE IS PROVIDED BY THE
POTENTIAL DIFFERENCE APPLIED
ACROSS THE TERMINALS.
ALTERNATING CURRENT
THE CURRENT THAT PERIODICALLY
CHANGES
DIRECTION
&
CONTINUOUSLY CHANGES MAGNITUDE
IT CAN BE PRODUCED BY :
a) STATIONARY COIL AND MOVING
MAGNETIC FIELD
b) STATIONARY MAGNETIC FIELD AND
MOVING COIL
THE
ELECTROMAGNETIC
SPECTRUM
THE ELECTROMAGNETIC
SPECTRUM
(ANGS)
(cm)
C
(HZ)
ENERGY
(EV)
RADIO
> 109
> 10
< 3 X 109
< 10-5
MICRO
109 - 106
10 - 0.01
3 X 109 - 3 X 1012
10-5 - 0.01
INFRARED
106 - 7000
0.01 - 7 X 10-5
0.01 - 2
7000 - 4000
7 X 10-5
4 X 10-5
4.3 X 1014
7.5 X 1014
2-3
UV
4000 - 10
4 X 10-5 - 10-7
3 - 103
X-RAYS
10 - 0.1
10-7 - 10-9
3 X 1017 - 3 X 1019
103 - 105
GAMMA
< 0.1
< 10-9
> 3 X 1019
> 105
VISIBLE
RADIO WAVES
RADIO WAVE IS AN ELECTRO-MAGNETIC WAVE
WHICH
HAS
ELECTRICAL
AND
MAGNETIC
LIGHT.
ITS FREQUENCY IS FROM 3 K Hz TO 300 G Hz
Frequen
cy
Range
3 to 30
Hz
ELF
SLF
30 to
300 Hz
Wavelengt
h Range
10,000 to
100,000
km
1000 to
10,000 km
ULF
300 to 3
kHz
100 to
1000 km
VLF
3 to 30
kHz
10 to 100
km
LF
1 to 10 km
MF
100 to
1000 m
AM broadcasting,
HF
10 to 100
m
VH
F
30 to
300 MHz
1 to 10 m
UH
F
300 to
3000
MHz
10 to 100
cm
10
SH
F
3 to 30
GHz
1 to 10 cm
11
EH
F
30 to
300 GHz
1 to 10
mm
30 to
300 kHz
300 to
3000
kHz
3 to 30
MHz
Typical sources
deeply-submerged submarine communication
submarine communication, ac power grids
VL Very Low
F Frequency
VF Voice Frequency
EL
F
UL
F
Extremely low
Frequency
Ultra Low
Frequency
3
kHz
300
Hz
30
Hz
30
kHz
3
kHz
300
Hz
30
3 Hz
Hz
OSCILLATOR WAVES
TYPES OF OSCILLATOR
MASTER OSCILLATOR
CRYSTAL OSCILLATOR
BEAT FREQUENCY OSCILLATOR
LOCAL FREQUENCY OSCILLATOR
PHOTO OF OSCILLATOR
THEREFORE MAGNETIC
COMPONENT IS VERY SMALL
WAVE LENGTH ( =
100 CM = 1 METERS
RADIO SPECTRUM
ABREVIATION
VLF
LF
FREQUENCY
3 - 30 K Hz
30 - 300 K Hz
WAVELENGTH
100 - 10 km
10,000 - 1000
MF
300 - 3000 K Hz
1000 - 100 m
HF
3 - 30 M Hz
100 - 10 m
30 - 300 M Hz
10 - 01 m
VHF
UHF
SHF
300 - 3000 M Hz
100 - 10 cm
3000 - 30000 M Hz
10 - 01 cm
PHASE
THE INSTANTANEOUS POSITION OF A
PARTICLE IN A WAVE OR POSITION OF A
PARTICLE AT A GIVEN TIME
TWO WAVES OF THE SAME FREQUENCY
WHEN TRANSMITTED AT THE SAME TIME
ARRIVE AT A POINT IN PHASE
PHASE DIFFERENCE IS THE ANGULAR
DIFFERENCE
BETWEEN
THE
CORRESPONDING
POINTS
ON
THE
WAVEFORMS
PHASE
PHASE DIFFERENCE
EXAMPLES
POLAR DIAGRAM
IT IS THE LINE JOINING POINTS OF
EQUAL INTENSITY AT A GIVEN TIME.
OR
A LINE SO PLOTTED THAT IT GIVES
THE RELATIVE VALUES OF THE
FIELD STRENGTHS OR THE POWER
RADIATED AT VARIOUS POINTS IN
BOTH HORIZONTAL AND VERTICAL
PLANES.
POLAR DIAGRAM
POLARIZATION
ELECTRICAL AND MAGNETIC
FIELDS ARE PRODUCED WHEN E/M
WAVES TRAVEL THROUGH SPACE
THESE FIELDS ARE AT RIGHT
ANGLES TO EACH OTHER
A VERTICAL AERIAL TRANSMITS
THE ELECTRICAL FIELD IN A
VERTICAL PLANE
POLARISATION
POLARISATION
ANTENNAS ARE DESIGNED TO PICK UP
ELECTRICAL COMPONENT ONLY
MODULATION
PROCESS
OF
IMPRESSING
INTELLIGENCE
ON
A
RADIO
CARRIER WAVE (CW) IN ORDER TO
CONVEY INFORMATION
VARIOUS
ARE
TYPE
OF
MODULATION
(a) KEYING
(b) AMPLITUDE MODULATION
(c) FREQUENCY MODULATION
LOWER THE
FREQUENCY LOWER THE RANGE.
3.
WIRELESS COMMUNICATION :
AUDIO
FREQUENCIES
WHEN
TRANSMITTED
THROUGH
SPACE
GET ATTENUATED.
TYPES OF MODULATION
AMPLITUDE MODULATION
FREQUENCY MODULATION
PULSE MODULATION
AMPLITUDE MODULATION
THE AMPLITUDE OF THE
CARRIER IS CHANGED IN
ACCORDANCE
WITH
THE
INTENSITY OF THE SIGNAL
THE FREQUENCY OF THE
CARRIER
WAVE
IS
KEPT
CONSTANT
AMPLITUDE MODULATION
AMPLITUDE MODULATION
(AM)
MODULATION DEPTH
THE RATIO OF THE AMPLITUDES
OF THE
SIGNAL TO
THE
UNMODULATED CARRIER WAVE
EXPRESSED IN PERCENTAGE
MOD. DEPTH = AMPLITUDE OF SIGNAL *100
AMPLITUDE OF CW
TEMPORAL REPRESENTATIONS OF
DSB-AM SIGNALS
FREQUENCY MODULATION
THE FREQUENCY OF THE
CARRIER IS CHANGED
IN
ACCORDANCE
WITH THE
INTENSITY
OF THE
AF
SIGNAL
THE AMPLITUDE OF THE
CARRIER
WAVE
IS
KEPT
CONSTANT
FM
ADVANTAGES OF FM
1. NOISELESS RECEPTION
2.
HIGH EFFICIENCY
3. HI-FI RECEPTION.
DISADVANTAGES OF FM
1. COMPLICATED RECEIVERS
2. OPERATES ON VHF, HENCE
RANGE IS LESS.
COMPARISON OF AM AND FM
AM
FM
1. TRANSMITTER
2. RECEIVER
COMPLEX
3. STATIC
COMPLEX
SIMPLE
SIMPLE
EXCESSIVE
4. BAND WIDTH
5. POWER FOR TX
SMALL
LARGE
ALMOST
NIL
LARGE
SMALL
SIDE BANDS
WHENEVER A CONTINUOUS
WAVE IS MODULATED BY A
FREQUENCY
LOWER THAN
ITSELF,
ADDITIONAL
FREQUENCIES
OCCUR
ON
EITHER SIDE OF THE CW
FREQUENCY
THESE
ARE
CALLED SIDE BANDS.
THE
INTELLIGENCE IS CARRIED IN
AM CW
COMPRISES OF
CW FREQ
CW FREQ + AUDIO
FREQ
CW FREQ - AUDIO
FREQ
AM CW SIDEBANDS
SPECTRAL REPRESENTATIONS OF
DSB-AM SIGNALS
FM CW
LARGER BAND WIDTH DUE
MULTIPLE SIDE BANDS. THIS
IS WHY FM CW CAN OPERATE
MAINLY IN VHF BAND.
FM CW
PULSE MODULATION
PHASE MODULATION CONSISTS OF
PULSE AMPLITUDE
PULSE FREQUENCY
PULSE WIDTH
MAINLY USED IN RADARS
ELECTROMAGNETIC WAVES
WHEN WAVES MEET A BOUNDARY, WHERE
THE MEDIUM CHANGES, THEY MAY:
REFLECT - BOUNCE BACK
REFRACT - GO THROUGH THE BOUNDARY,
USUALLY
CHANGING
SPEED
AND
DIRECTION
GET ABSORBED - GIVE UP THEIR ENERGY,
DIFFRACTION
WHEN WAVES MEET A GAP IN A BARRIER, THEY
CARRY ON THROUGH THE GAP. THIS MAY SEEM
OBVIOUS, BUT WHAT HAPPENS ON THE FAR SIDE
OF THE GAP ISN'T SO STRAIGHTFORWARD.
THE WAVES ALWAYS 'LEAK' TO SOME EXTENT
INTO THE SHADOW AREA BEYOND THE GAP. THIS
IS CALLED DIFFRACTION
THE EXTENT OF THE SPREADING DEPENDS ON
HOW THE WIDTH OF THE GAP COMPARES TO THE
WAVELENGTH OF THE WAVES
WAVES
OBJECTS
TRAVEL
IN
GROUND WAVES
SURFACE WAVES
SKY WAVES
SPACE WAVES
DIRECT WAVES
WAVES
GROUND
REFLECTED
RADIO SPECTRUM
ABREVIATION
VLF
LF
FREQUENCY
3 - 30 K Hz
30 - 300 K Hz
WAVELENGTH
100 - 10 km
10,000 - 1000
MF
300 - 3000 K Hz
1000 - 100 m
HF
3 - 30 M Hz
100 - 10 m
30 - 300 M Hz
10 - 01 m
VHF
UHF
SHF
300 - 3000 M Hz
100 - 10 cm
3000 - 30000 M Hz
10 - 01 cm
SURFACE WAVES
DIFFRACTION
DIFFRACTION
FREQUENCY
SURFACE WAVES
ATTENUATION
FACTORS
1. SURFACE
ATTENUATION
2. FREQUENCY
FREQUENCY
SURFACE WAVES
DIFFRACTION
VLF LEAST
MAXIMUM
LF
LESS
REDUCING
MF
INCREASING
REDUCING
RANGE
3000 - 4000 nm
~ 1500 nm
HF
VHF
SEVERE
LEAST
NIL
70 - 100 nm
LOS ONLY
SPACE WAVES
D = 1.25
HT
1.25
HR
IONOSPHERE
U/V RAYS
ELECTRONS
GAS MOLECULES
THE IONOSPHERE
ELECRICALLY CONDUCTING SPHERE
D LAYER : 50 - 100 KM, AVG 75 KM
E LAYER : 100 - 150 KM, AVG 125 KM
F LAYER : 150 - 350 KM, AVG 225 KM
DENSITY OF IONOSPHERE
D LEAST , F MAXIMUM
DIURNAL ACTIVITY : DAY -- DENSITY INCREASES
REFLECTING HT MOVES DN
SEASONAL ACTIVITY : MAX -- EARTH CLOSEST
TO SUN. CAUSES SPORADIC ACTIVITY,
RESULTING IN SPORADIC-E RECEPTION IN VHF
BAND (~150 MHz )
11 YEAR SUN-SPOT CYCLE : ENHANCED UV & XRADIATION, VHF SIGNALS MAY RETURN
ATTENUATION IN ATMOSPHERE
DENSITY OF LAYERS :
GREATER DENSITY -- GREATER
ATTENUATION
FREQ IN USE
LOWER FREQ -- GREATER ATTENUATION
PENETRATION DEPTH
HIGHER THE FREQ -- GREATER THE PENETRATIONGREATER ATTENUATION
RANGES AVAILABLE
TRANSMISSION POWER
DEPTH OF PENETRATION
ANGLE OF INCIDENCE -- MAX RANGE BY WAVE
LEAVING TANGENTIAL TO EARTH
CRITICAL ANGLE
2
1
2 IS
CRITICAL ANGLE
2
1
FOR THE SAME FREQUENCY AN INCREASE IN INCIDENCE
BEYOND
WOULD
ENSURE
AN
POWER
MAY
RETURN ALTHOUGH
INCREASED
UNINTERRUPTED
HAVE
TO
BE
2 ,
THE
MEANS
HIGHER
RANGE
WOULD
BE
HF COMMUNICATION
CRITICAL FREQUENCY fC FOR PREVAILING
ATMOSPHERIC CONDITIONS
MUF = fC X sec i
LUHF
NIGHT TRANSMISSION
DEPTH OF PENETRATION
NIGHT TRANSMISSION
RECOMBINATION
REFLECTING HT MOVES UP
o 30 Hz
10,000 to 100,000
km
o 300 Hz
1000 to 10,000 km
to 3 kHz
100 to 1000 km
30 kHz
10 to 100 km
1 to 10 km
to 3000
kHz
100 to 1000 m
AM broadcasting,
30 MHz
10 to 100 m
1 to 10 m
300 kHz
300 MHz
to 3000
MHz
10 to 100 cm
30 GHz
1 to 10 cm
microwave oven, television broadcast, GPS, mobile phone communication (GSM, UMTS
(DECT), WLAN (Wi-Fi), Bluetooth
NIGHT TRANSMISSION
FOR A GIVEN FREQ, SKIP DIST VARIOUS WITH TIME OF THE DAY
( AND ALSO SEASONS)
DEAD SPACE POSSIBLE ONLY IN HF
VL Very Low
F Frequency
VF Voice Frequency
EL
F
UL
F
Extremely low
Frequency
Ultra Low
Frequency
3
kHz
300
Hz
30
Hz
30
kHz
3
kHz
300
Hz
30
3 Hz
Hz
ANTANNAE
An antenna (or aerial) is a transducer designed to transmit or
receive electromagnetic waves. In other words, antennas convert
electromagnetic waves into electrical currents and vice versa.
They are used with waves in the radio part of the
electromagnetic spectrum, that is, radio waves, and are a
necessary part of all radio equipment.
They are used with waves in the radio part of the
electromagnetic spectrum, that is, radio waves, and are a
BEGINNING OR END all radio equipment.
1.
Atannae gain is ratio between radiation
intensity in a given direction and that produced by an
ideal antannae which transmits in all direction. What is
loop antannae with two arms used in ADF
2.
EIRP stands for effective isotropically
radiated power. it is the amount of power that a
theoretical isotropical antennae would emit to produce
peak power in direction of maximum antannae gain.
EIRP = power at transmitter - cable loss + antannae gain
microphone
speaker
OSCILLATOR
PRODUCES RF
RF AMPLIFIER
AMPILFIES RF
MODULATOR
MODULATES RF
WITH AF
MICROPHONE
CONVERTS AW
TO AF
AF AMPLIFIER
AMPLIFIES AF
POWER AMPLIFIER
AMPLIFIES RF+AF
DEMODULATOR
SUPRESSES RF
AND PRODUCES
AF
AF AMPLIFIER
AMPLIFIES AF
AMPLIFIER
AMPLIFIES RF+AF
SPEAKER
CONVERTS AF INTO
AW
DETECTOR
CONVERTS
IF INTO AF
BFO AVC
LFO PRODUCES LF
8000 K Hz
LF AMPLIFIERS
AMPLIFIES LF
SQUELCH
AF AMPLIFIER
AMPLIFIES AF
Qualities of reciever
superhetrodyne
QUESTIONS ?