Page 61 - Radar Technology Encyclopedia
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array, Yagi-Uda                                                                   ATMOSPHERE        51



           A Yagi-Uda array  is one  formed from  a  series of dipoles  Ref.: Evans (1968); Hovanessian (1984),  p. 349-357; Skolnik (1970), pp.
           located in parallel in a common plane and forming a “wave  33.1–32.24.
           channel.” One of  the  dipoles is the actively driven element
           (Fig. A91) (1) and the rest are passive. One of the passive ele-
           ments located behind the actively fed antenna plays the role
           of reflector (2), while the others, placed  in front of the  Transmitter    T/R switch     Preamplifier
           actively fed antenna, play the role of directors (3). The reflec-
           tor length is somewhat greater than l/2, while driver length is
                                                                                        Local          Multiple
           somewhat less than  l/2.                                     Exciter        oscillator    superheterodyne
                                                                                                       receiver
               This array is a type of end-fire array named after S. Uda
           and H. Yagi, who were the first to describe it correspondingly
                                                                        Master          Variable       Doppler
           in Japanese and in English. Yagi-Uda arrays with a large     oscillator     oscillator     compensation
           number of dipoles can be treated as surface-wave antennas.
           The main advantages of such antennas are design simplicity,
                                                                        System                        Matched
           high directive gain,  and low weight. The  antenna’s narrow   timing                          filter
           bandwidth is a drawback. They are used in VHF radars and
           sometimes are called wave-channel antennas. AIL
                                                                          Digital                     Square-law
           Ref.: Fradin (1977), p. 194; Johnson (1993), pp. 3.13–3.15.  voltmeter                       detector

                                                                        Computer
                                                                       integration


                                                                        Display
                                                    Supporting
                                                      structure   Figure A92 Block diagram of a radar astronomy system (after
                                                                  Hovanessian, 1984, Fig. 13-5, p. 353).
                                3
                        1
                2
               Reflector  Driven element  Directors                                  Table A8
              Figure A91 Yagi-Uda array.                          Detectability of Radar Targets Relative to the Moon.
                                                                                      4
                                                                                   s /R  (relative to
           ASTRONOMY, radar.  Radar  astronomy is the  branch of      Target                         Level in dB
           astronomy investigating celestial objects with radar methods.           value for moon)
           The main problem in radar astronomy arises from the fact that  Large aircraft  1,000          30
           tremendous distances are involved, so extreme receiver sensi-
           tivity and transmitter power are required for the detection of  Moon          1               0
           weak signals. The detectability of radar targets relative to the                -5
                                                                 Sun                  1 ´  10           -50
           moon is shown in Table A8. It shown that very sophisticated
           equipment is required to detect the distant targets. The gen-  Venus       2 ´  10 -7        -67
           eral block diagram  of  an  astronomical radar is shown  in                      -8
           Fig. A92.                                             Mars                 1.3 ´  10        -78.9
               The most common type of antenna is the large, steerable                      -9
                                                                 Mercury              1.7 ´  10        -87.7
           parabolic reflector. The Cassegrainian antenna is a good solu-
           tion for astronomical radar antennas because the feed is closer  Jupiter  3.3 ´  10 -10     -94.8
           to the main mirror in double-reflector antennas, so the trans-                  -11
           mission line losses are less, as lengthy transmission lines can  Saturn   1.7 ´  10         -107.7
           be eliminated and  the  receiver can be mounted at  the  feed                   -13
                                                                 Uranus              1.7 ´  10         -127.7
           since it is easily accessible for maintenance. The transmitters
           typically must be coherent and capable of handling high aver-  Neptune    2.3 ´  10 -14     -136.4
           age powers (the main difference between operation mode of
           transmitters for  radar astronomy  relative to conventional
           radars is that they require higher average power rather than  ATMOSPHERE.  Earth’s atmosphere consists of several
           high peak power). The receiver is usually a superheterodyne  concentric shells containing gases, vapors, and other material
           receiver with parametric amplifiers to reduce self-generated  in suspension and bound to the earth by gravitational force.
           noise and increase sensitivity. The performance of some facil-  The  composition of  the  atmosphere by weight is approxi-
           ities used in radar astronomy are given in the Table A9. SAL  mately 76.8% nitrogen and 23.2% oxygen. The atmosphere
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