New Approach for Calculating the Effective Dielectric Constant of the Moist Soil for Microwaves

微波食品加热 含水量 电介质 遥感 环境科学 土壤科学 介电常数 均方误差 微波辐射计 材料科学 多孔性 辐射计 地质学 计算机科学 数学 复合材料 岩土工程 光电子学 电信 统计
作者
Chang-Hwan Park,Andreas Behrendt,E. LeDrew,Volker Wulfmeyer
出处
期刊:Remote Sensing [Multidisciplinary Digital Publishing Institute]
卷期号:9 (7): 732-732 被引量:40
标识
DOI:10.3390/rs9070732
摘要

Microwave remote sensing techniques are used, among others, for temporally and spatially highly-resolved observations of land-surface properties, e.g., for the management of agricultural productivity and water resource, as well as to improve the performances of numerical weather prediction and climate simulations with soil moisture data.In this context, the effective dielectric constant of the soil is a key variable to quantify the land surface properties.We propose a new approach for the effective dielectric constant of the multiphase soil that is based on an arithmetic average of the dielectric constants of the land-surface components with damping.The results show, on average, better agreement with experimental data than previous approaches.Furthermore, the proposed new model overcomes the theoretical limitation of previous models in the incorporation of non-physical parameters to simulate measured data experimentally with satisfactory accuracy.For microwave remote sensing such as SMAP (Soil Moisture Active Passive), SMOS (Soil Moisture and Ocean Salinity) and AMSR-E (Advanced Microwave Scanning Radiometer for EOS), the physical-based model in our study showed a 23-35% RMSE (root-mean-square error) reduction compared to the most prevalent refractive mixing model in the prediction of the dielectric constant for the real and imaginary part, respectively.Furthermore, in radiowave bands used in portable soil sensors such as TDR (time-domain reflectometer) and GPR (ground-penetrating radar) the new dielectric mixing model reduced RMSE by up to 53% in the prediction of the dielectric constant.We found that the permittivity over the saturation point (porosity of dry soil) has a very different and varying pattern compared to that measured in the unsaturated condition.However, in our study, this pattern was mathematically derived from the same mixing rule applied for the unsaturated condition.It is expected that the new dielectric mixing model might help to improve the accuracy of flood monitoring by satellite.

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