Temperature dependent dielectric model at 1.4 GHz for an agricultural soil thawed and frozen

V. Mironov, A. Karavaysky
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引用次数: 1

Abstract

A mono-frequency dielectric model for the agricultural soil both thawed and frozen has been developed. The model is based on the soil dielectric measurements carried out in the ranges of volumetric moisture from 0,03 to 0,51 cm3/ cm3, dry soil density from 1.12 to 1.64 g/cm3, and temperature from -30 to 25°C (heating run), at the frequency of 1.4 GHz used in the SMOS mission. To fit the results of measurements of the soil complex refractive index (CRI) as a function of soil moisture, the refractive mixing model was applied. As a result, the parameters of the refractive mixing model linked to soil solids, as well as the bound, transient, and free soil water components were derived as a function of temperature. The error of the proposed dielectric model was shown to be in the order of the dielectric measurement error itself.
冻融农用土壤1.4 GHz温度相关介电模型
建立了冻融农用土壤的单频介电模型。该模型基于在SMOS任务中使用的1.4 GHz频率下进行的土壤介电测量,其体积湿度范围为0.03至0.51 cm3/ cm3,干土密度范围为1.12至1.64 g/cm3,温度范围为-30至25°C(加热运行)。为了拟合土壤复折射率(CRI)随土壤水分变化的测量结果,采用了折射率混合模型。结果,折射率混合模型的参数与土壤固体有关,以及束缚、瞬态和自由土壤水组分作为温度的函数被导出。所提出的介电模型的误差与介电测量误差本身成正比。
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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