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14 The Antenna Development in Japan: Past and Present 14.1 Introduction . . 14.2 Maxwell, Hertz, and Their Followers in Japan. . 14.3 Marconi and the First Japanese Wireless Communication 14.4 Sea Battle of the Tsushima Straits and the Japanese . Radiotelegraph . 14.5 Yagi-Uda Antenna. . 14.6 Kinjiro Okabe and his Split-Anode Magnetron . . . 14.7 Radar in World War I1 . 14.8 Electrical Engineering Milestones in Japan . . 14.9 Conclusion References . 15 Historical Background and Development of Soviet Quasioptics at Near-mm and Sub-mm Wavelengths 15.1 Introduction . . 15.2 Quasioptics in the Broad and Narrow Sense . 15.3 Pioneering Research into Hertz Optics (1888-1900) and Lebedev s Contribution . . 15.4 Early Success: Free Space Gaussin-Beam Quasioptical Technologies . . 15.4.I Reflector and Lens Antennas . 15.4.2 Circuitsfor Antenna Feeding and Gyrotron Coupling. . 15.4.3 Componentsfor Beam Manipulation . 15.4.4 Measuring Systemsfor Spectroscopy and Plasma Diagnostics . . 15.4.5 Long Distance Microwave Power Transmission

CREATE TABLE demo314(a,b,c,d,e,f,g); CREATE INDEX demo314_idx ON demo314(a,b,c,d,e,f);

or, in the more compact vector form: u y u x m t bg T u m k - re + r + ku = t k + m t x + sk x y s t z y t (3.39)

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formed in less than 3 Ma and the Kerguelen Plateau in 45 Ma Most of the volcanic activity occurred in short, violent episodes separated by long periods of relative quiescence Estimates of the average rates of formation, which include the periods of quiescence, are 12 18 km3 a 1 for the Ontong Java Plateau and 2 8 km3 a 1 for the Deccan Traps Ontong Java s rate of emplacement may have exceeded the contemporaneous global production rate of the entire mid-ocean ridge system (Cof n & Eldholm, 1994) The outpouring of large volumes of ma c magma in such short periods of time requires a mantle source This characteristic has encouraged interpretations involving deep mantle plumes (Sections 55, 1210), although the existence and importance of these features are debated widely (Anderson & Natland, 2005).

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It is interesting that it takes only 4 or 5 steps to turn the values away from the starting values to values that are already relatively close to the respective limits. 4. The values of the exact solution of the Laplace equation are u(1, 1) 4, u(2, 1) u(1, 2) 7, u(2, 2) 2, 64. 2, 2, 2.

Mantle plumes may form large oceanic plateaux and some continental ood basalts also may be attributed to them Beneath the Ethiopian Plateau and the Kenya Dome (in the East African Plateau), extensive volcanism and topographic uplift appear to be the consequences of anomalously hot asthenosphere (Venkataraman et al, 2004) The isotopic characteristics of the volcanic rock and the large volume of ma c lava erupted over a short period of time (Hofmann et al, 1997; Ebinger & Sleep, 1998) suggest that a plume or plumes below the uplifts tap deep undegassed mantle sources (Marty et al, 1996; Furman et al, 2004) As the deep plumes ascend they undergo decompression melting with the amount of melt depending on the ambient pressure (Section 742) Consequently, less melting is expected under thick continental lithosphere than under thick oceanic lithosphere.

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