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Multi-Relaxation Temperature-Dependent Dielectric Model of the Arctic Soil at Positive Temperatures

  • Physics of Semiconductors and Dielectrics
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Russian Physics Journal Aims and scope

Frequency spectra of the dielectric permittivity of the Arctic soil of Alaska are investigated with allowance for the dipole and ionic relaxation of molecules of the soil moisture at frequencies from 40 MHz to 16 GHz and temperatures from –5 to +25°С. A generalized temperature-dependent multi-relaxation refraction dielectric model of the humid Arctic soil is suggested.

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Authors and Affiliations

  1. L. I. Kirensky Institute of Physics of the Siberian Branch of the Russian Academy of Sciences, Krasnoyarsk, Russia

    I. V. Savin & V. L. Mironov

  2. Siberian State Aerospace University Named after Academician M. F. Reshetnev, Krasnoyarsk, Russia

    V. L. Mironov

  3. National Research Tomsk State University, Tomsk, Russia

    V. L. Mironov

Authors
  1. I. V. Savin
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  2. V. L. Mironov
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Correspondence to I. V. Savin.

Additional information

Translated from Izvestiya Vysshikh Uchebnykh Zavedenii, Fizika, No. 7, pp. 41–47, July, 2014.

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Savin, I.V., Mironov, V.L. Multi-Relaxation Temperature-Dependent Dielectric Model of the Arctic Soil at Positive Temperatures. Russ Phys J 57, 907–914 (2014). https://doi.org/10.1007/s11182-014-0323-6

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  • DOI: https://doi.org/10.1007/s11182-014-0323-6

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