Conclusions
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1.
In magnetic ores with ρe=1 Ω·m, despite the marked attenuation, in practice it is possible to achieve a range of 30–35 m at frequencies below 0.15 MHz with a transmitter power of 20–25 W and a receiver sensitivity of 0.5–1 μV/m.
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2.
In rocks and ores with ρe=1 Ω·m or more with the same equipment it is possible to achieve ranges of over 70–100 m.
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3.
In magnetic rocks and ores with ρe=1 Ω·m or more, b is almost independent of the magnetic susceptibility. An appreciable dependence of b on the magnetic susceptibility is observed only in magnetite ores with ρe=1 Ω·m.
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4.
In low-resistance rocks and ores of the Krivoi Rog deposit, in practice it is inadvisable to use frequencies above 1.0 MHz, owing to the high value of b, which rapidly rises with the frequency.
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Literature Cited
Z. A. Krutikhovskaya and G. K. Kuzhelov, Use of Geophysical Methods to Study the Iron-Ore Formation of the Ukrainian Crystalline Shield [in Russian], Gosgeoltekhizdat, Moscow (1960).
G. F. Gurevich, “Use of radio-wave sounding in low-resistance geolectric sections,” Tr. TsNIGRI, No. 58, Moscow (1964).
Additional information
Translated from Fiziko-Tekhnicheskie Problemy Razrabotki Poleznykh Iskopaemykh, No. 1, pp. 79–82, January–February, 1981.
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Savchenko, N.M. Propagation of radio waves in ferriferous rocks and ores. Soviet Mining Science 17, 72–75 (1981). https://doi.org/10.1007/BF02498396
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DOI: https://doi.org/10.1007/BF02498396