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Titlebook: Lateral Electromagnetic Waves; Theory and Applicati Ronold W. P. King,Margaret Owens,Tai Tsun Wu Book 1992 Springer-Verlag New York, Inc. 1

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书目名称Lateral Electromagnetic Waves
副标题Theory and Applicati
编辑Ronold W. P. King,Margaret Owens,Tai Tsun Wu
视频video
图书封面Titlebook: Lateral Electromagnetic Waves; Theory and Applicati Ronold W. P. King,Margaret Owens,Tai Tsun Wu Book 1992 Springer-Verlag New York, Inc. 1
描述The propagation of waves along and across the boundary between two media with different characteristic velocities is much more complicated when the source is on or near the boundary than when it is far away and the incident waves are plane. Examples of waves generated by localized sources near a boundary are the electromagnetic waves from the currents in a dipole on the surface of the earth and the seismic waves from a slip event in a fault in the earth‘s crust like the San Andreas fault in California. Both involve a type of surface wave that is called a lateral wave in electro­ magnetics and a head wave in seismology. Since the two are analogous and the latter is more easily visualized, it is conveniently used here to introduce and describe this important type of surface wave using the data of Y. Ben­ Zion and P. Malin ("San Andreas Fault Zone Head Waves Near Parkfield, CA," Science 251, 1592-1594, 29 March 1991).
出版日期Book 1992
关键词CA; antenna; communication; electromagnetic wave; remote sensing; seismology; surface; television; waves
版次1
doihttps://doi.org/10.1007/978-1-4613-9174-6
isbn_softcover978-1-4613-9176-0
isbn_ebook978-1-4613-9174-6
copyrightSpringer-Verlag New York, Inc. 1992
The information of publication is updating

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Book 1992a head wave in seismology. Since the two are analogous and the latter is more easily visualized, it is conveniently used here to introduce and describe this important type of surface wave using the data of Y. Ben­ Zion and P. Malin ("San Andreas Fault Zone Head Waves Near Parkfield, CA," Science 251, 1592-1594, 29 March 1991).
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Historical and Technical Overview of Electromagnetic Surface Waves; Introduction to Lateral Waves,ial direction of propagation which is also the direction of the Poynting vector .(., . . .(r, . × .(., . The expanding spherical surfaces of constant phase axe defined by . Each surface travels radially outward with the velocity . The distance between adjacent spherical surfaces of the same phase at any given istant is . Where λ is the wevelength.
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Lateral Waves in a One-Dimensionally Anisotropic Half-Space,fferent conductivities to the components of current parallel to the bedding surfaces and those perpendicular to them. In this case, . and . may differ somewhat from each other and more substantially from ..
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