Measurement of Typic Quartzipsamment Soil Permittivity at Different Depths

Cristiano Miranda Correia Lima, J. N. Carvalho, Alexandre Fonseca D’Andrea
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Abstract

This work presents the characterization of the electrical permittivity of typic quartzipsamment soil, found in the Restinga de Cabedelo National Forest (Cabedelo FLONA). For measurement, a rectangular resonant cavity was constructed, excited by a waveguide iris and the cavity perturbation technique was employed. The 16451B Vector Network Analyzer was used to measure the resonance frequency shift when the cavity is loaded with the material sample. For validation, the coaxial probe technique was used, through Dielectric Probe 85070 software. Results were presented for soils collected at different depths. The results show that the permittivity has small variation with depth, being higher in the shallower layers, with more organic matter. It was also verified a variation of the dielectric loss of the soil with the depth and variable with the frequency, indicating that it is possible to identify soil properties through the measurement of the dielectric properties.
不同深度典型石英土介电常数的测量
本文介绍了在Restinga de Cabedelo国家森林(Cabedelo FLONA)中发现的典型石英土的介电常数特征。测量时,构造了一个矩形谐振腔,由波导虹膜激发,并采用腔微扰技术。采用16451B矢量网络分析仪测量材料试样加载空腔时的谐振频移。为了验证,使用了同轴探针技术,通过介电探针85070软件。给出了不同深度土壤采集的结果。结果表明:介电常数随深度变化不大,有机质含量越高,介电常数越浅;还验证了土壤的介电损耗随深度的变化和随频率的变化,表明可以通过测量介电特性来识别土壤性质。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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