On the Possibility of the Existence of a Surface Electromagnetic Wave in the Permafrost Area


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The results of measurements of the vertical component of electric field at a radio path with the permafrost at a frequency of 255 kHz have been interpreted. An analysis of the results has shown that the considered radio path exhibits the properties of a two-part impedance surface, i.e., it consists of two sections. At a distance of 70 km from a radiation source and at a frequency of 255 kHz of the electromagnetic wave, the field decreases with the distance R according to the power law as R-1.5 and a power index takes an intermediate value between the power indices for decreasing the field in free space R-2 and for the decrease in the field above an ideal conducting surface R-1. With further propagation at a distance of 70–220 km, the field shows the specific behavior of a surface electromagnetic wave.

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V. Balkhanov

Physical Material Science Institute, Siberian Branch

编辑信件的主要联系方式.
Email: ballar@yandex.ru
俄罗斯联邦, Ulan-Ude, 670047

Yu. Bashkuev

Physical Material Science Institute, Siberian Branch

Email: ballar@yandex.ru
俄罗斯联邦, Ulan-Ude, 670047

V. Advokatov

Physical Material Science Institute, Siberian Branch

Email: ballar@yandex.ru
俄罗斯联邦, Ulan-Ude, 670047

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