Electric properties of ice near solidification and melting temperature

• Autorzy: Rusiniak, L.
• Języki publikacji: EN

Abstrakty

EN

The dielectric permittivity, conductivity and loss tangent of ice were measured for different thicknesses of the sample (0.1-4 mm). In this investigation, the measurement of thin samples can be treated as a laboratory test of surface proper-ties and that of thick samples as a test of bulk properties. The measurements were carried out from 3.5 to -13.5°C with descending and growing temperature. Two domain Debye resonances were observed. The one at low frequency is interpreted as being associated with transversal mode, and the other, at higher frequency, is associated with longitudinal mode of proton domain. The resonance frequencies depend on sample size and temperature. Temperature hysteresis of resonance frequencies was observed. As the temperature grows starting from low temperature, the resonance frequencies move towards each other and finally the two modes join to form one mode. The dielectric constant associated with transversal mode is higher than 104. The dielectric constant associated with longitudinal mode is about 102. The dipole dielectric constant vanishes after solidification. As the temperature grows, the di-pole dielectric constant grows too. Oscillation of dielectric permittivity and conductance for a small value of oscillator level was observed. The experimental data show that ice could be both a ferroelectric and a piezoelectric material.

Słowa kluczowe

EN

ice; dielectric permittivity; conductivity; loss tangent; ferroelectrics; piezoelectrics

• Czasopismo: Acta Geophysica Polonica
• Rocznik: 2004
• Tom: Vol. 52, nr 3
• Strony: 363-380
• Opis fizyczny: Bibliogr. 38 poz.

Twórcy

autor

Rusiniak, L.

• Institute of Geophysics, Polish Academy of Sciences, Księcia Janusza 64, 01-452 Warszawa,

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