Project Sanguine Interference Mitigation Research

Valentino, A.; Abromavage, M.M.; McLellan, D.; Miller, Donald A.

doi:10.1109/tcom.1974.1092227

Cited by 3 publications

(1 citation statement)

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“…Wave propagation in SLF/ELF ranges has been studied widely in the 1990s and 1970s by many investigators (Schumann 1952a(Schumann , 1952bGalejs 1961Galejs , 1962Galejs , 1964bGalejs , 1965Galejs , 1972bBannister , 1984aGreifinger and Grifinger 1978;BehrooziToosi and Booker 1980;Yuan 2011) (Burrows 1974a(Burrows , 1974b, propagation computation and measurement (Pappert and Moler 1974;, signal and noise processing (Evans and Griffiths 1974;Ginsberg 1974), and environmental effect of a transmitting antenna (Valentino et al 1974). In this issue, Wait wrote a mourning article "Dedication to Janis Galejs".…”

Section: Slf Communication System and Slf/elf Propagation Theorymentioning

confidence: 99%

Historical and Technical Overview of SLF/ELF Electromagnetic Wave Propagation

Pan¹,

Li²

2013

Advanced Topics in Science and Technology in China

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In general, very low frequency (VLF) refers to electromagnetic waves with frequencies from 3 kHz to 30 kHz; ultra low frequency (ULF) refers to frequency range between 300 Hz to 3 kHz; the frequency range of 30 Hz to 300 Hz is defined as super low frequency (SLF); and the frequency below 30 Hz is referred to as extremely low frequency (ELF). In some early studies, alternative definitions may have been used with frequency range of 3 Hz to 3 kHz generally referred to ELF. In this book, the emphasis is on SLF (30-300 Hz) and ELF (below 30 Hz) ranges, using the MKS system of units and the time dependency e −iωt . Medium Characteristics of SLF/ELF Wave PropagationDue to the long wavelength, SLF/ELF waves, when excited and propagated on and near the Earth's surface, will cover lithosphere, atmosphere and ionosphere, whose electromagnetic characteristics differ significantly in their propagation paths. The permeability of the atmosphere and ionosphere is approximately μ 0 , the permeability in free space, as well as that of the lithosphere, except in the regions that are rich in iron, nickel, cobalt, etc. Therefore, the permeability of the lithosphere can be also treated as μ 0 , if neither the transmitter nor the receiver is located in mineral-rich areas. The atmosphere is a non-conductive medium with negligible conductivity, whose permittivity is close to ε 0 , the permittivity of free space. While the lithosphere is conductive, the conductivity of sea water σ sea is in the range of 2.5-5.5 S/m, and the conductivity σ g of rock and soil in the range of 10 −2 -10 −4 S/m. The dielectric constant ε r of the lithosphere does not have large effects on the propagation of SLF/ELF waves.The ionosphere is composed of partially ionized gas, which includes electrons, ions, and electrically neutral particles, above 70 km or so from the sea level. The electrons and ions make the ionosphere conductive, thus the majority of the energy of the incident VLF/SLF/ELF waves will be reflected by the ionosphere. When both the transmitter and the receiver are located in the space between the ground and the W. Pan, K. Li, Propagation of SLF/ELF Electromagnetic Waves,

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