2022
DOI: 10.1109/tgrs.2022.3180727
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The Effect of Dielectric Relaxation Processes on the Complex Dielectric Permittivity of Soils at Frequencies From 10 kHz to 8 GHz—Part I: Experimental

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Cited by 12 publications
(4 citation statements)
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“…Despite having many advantages, this method of sample preparation is associated with a lot of disadvantages. It has been observed that there has been a change in mechanical strength, electrical resistance, and dielectric permittivity of soil at low frequencies within a few hours after the addition of water to dried soil samples (Bobrov et al, 2019(Bobrov et al, , 2022Fedotov et al, 2005).…”
Section: Moisture Content Analysis and Sample Preparation Of Soil Sam...mentioning
confidence: 99%
“…Despite having many advantages, this method of sample preparation is associated with a lot of disadvantages. It has been observed that there has been a change in mechanical strength, electrical resistance, and dielectric permittivity of soil at low frequencies within a few hours after the addition of water to dried soil samples (Bobrov et al, 2019(Bobrov et al, , 2022Fedotov et al, 2005).…”
Section: Moisture Content Analysis and Sample Preparation Of Soil Sam...mentioning
confidence: 99%
“…For clayey materials in the GPR operating frequency range, the relationship between grain size, mineralogy, volumetric water content, and the constitutive parameters εnormalenormalfnormalf ${\varepsilon }_{\mathrm{e}\mathrm{f}\mathrm{f}}^{\prime }$ and σnormalenormalfnormalf ${\sigma }_{\mathrm{e}\mathrm{f}\mathrm{f}}^{\prime }$ is non‐trivial and still a topic of current research (e.g., Bobrov et al., 2022; Loewer et al., 2017). Even minor amounts of clay (5%–10%) has been shown to greatly change both the value and frequency‐dependence of εnormalenormalfnormalf ${\varepsilon }_{\mathrm{e}\mathrm{f}\mathrm{f}}^{\prime }$ and σnormalenormalfnormalf ${\sigma }_{\mathrm{e}\mathrm{f}\mathrm{f}}^{\prime }$ (Patriarca et al., 2013).…”
Section: Radar Wave Propagationmentioning
confidence: 99%
“…For clayey materials in the GPR operating frequency range, the relationship between grain size, mineralogy, volumetric water content, and the constitutive parameters 𝐴𝐴 𝐴𝐴 ′ ef f and 𝐴𝐴 𝐴𝐴 ′ ef f is non-trivial and still a topic of current research (e.g., Bobrov et al, 2022;Loewer et al, 2017). Even minor amounts of clay (5%-10%) has been shown to greatly change both the value and frequency-dependence of 𝐴𝐴 𝐴𝐴 ′ ef f and 𝐴𝐴 𝐴𝐴 ′ ef f (Patriarca et al, 2013).…”
mentioning
confidence: 99%
“…В данной работе исследовано влияние объемной влажности от 0% до 40% (вертикальных профилей влажности), плотности сухого сложения от 0.4 до 1.8 г/см 3 , содержания глинистой фракции от 0.15 до 0.55 г/г (типа агропочвы), среднеквадратических отклонений (СКО) высот неровностей поверхности от 0 до 4 см почвенного покрова на вариации коэффициента отражения в сверхширокой полосе частот от 100-400 МГц до 1. 26 частот (ниже первых десятков МГц) [7]; с другой стороны, волны СВЧ диапазона (первые единицы ГГц) обладают ограниченной глубиной проникновения в почву и значительным рассеянием на случайных неровностях поверхности почвы и элементах растительного покрова [8].…”
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