Evaluation of the Accuracy of the Remote Determination of the Brewster Angle when Measuring Physicochemical Parameters of Soil

Gennadiy Ivanovich Linets, Anatoliy Vyacheslavovich Bazhenov, Sergey Vladimirоvich Malygin, Natalia Vladimirovna Grivennaya, Sergey Vladimirovich Melnikov, Vladislav Dmitrievich Goncharov
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Abstract

In precision farming technology, the moisture of the soil, its granulometric composition, specific conductivity and a number of other physical and chemical parameters are determined using remote radar sensing. The most important parameters are those measured in the area of the plant root system located well below the “air-surface” boundary. In order to create conditions for the penetration of electromagnetic waves through the “air-surface” interface with a minimum reflection coefficient, the irradiation of the Earth’s surface is carried out obliquely with an angle of incidence close to the Brewster angle. The reflection coefficient, and, consequently, the Brewster angle, depend on the complex dielectric permittivity of the surface soil layer and are not known a priori. To determine the Brewster angle, the usual method is to search for the minimum amplitude of the vertically polarized signal reflected from the surface. Another approach is when the first derivative of the dependence of the modulus of the complex amplitude of a vertically polarized interference wave, taken with respect to the angle of incidence, is set equal to zero. In turn, in real dielectrics such as agricultural soils, the amplitude of the vertically polarized signal reflected from the surface is directly proportional to the reflection coefficient and does not have a pronounced minimum, which reduces the accuracy of the measurements. Based on the solution of the Helmholtz wave equation for a three-layered structure of the propagation medium (air, upper fertile soil layer, soil layer below the groundwater level), a model of the process of forming an interference wave under oblique irradiation of a planar layered dielectric with losses has been developed. Using the developed model, factors influencing the accuracy of determining the Brewster angle have been identified. For the first time, it is proposed to use the phase shift between the oscillations of the interference waves with vertical and horizontal polarization to measure the Brewster angle. A comparative assessment of the accuracy of determining the Brewster angle using known amplitude methods and the proposed phase method has been carried out. The adequacy of the method was experimentally confirmed. Recommendations have been developed for the practical application of the phase method of finding the Brewster angle for assessing the dielectric permittivity of soil and its moisture content.
测量土壤理化参数时布鲁斯特角的远程测定精度评价
在精准农业技术中,土壤的水分、颗粒组成、比电导率和其他一些物理和化学参数是通过遥感雷达来确定的。最重要的参数是那些位于“空气-表面”边界以下的植物根系面积的测量值。为了给电磁波通过反射系数最小的“空气-表面”界面的穿透创造条件,以接近布鲁斯特角的入射角对地球表面进行斜照射。反射系数以及因此产生的布鲁斯特角取决于表层土壤的复介电常数,并且不是先验已知的。为了确定布鲁斯特角,通常的方法是寻找从表面反射的垂直极化信号的最小振幅。另一种方法是当垂直偏振干涉波的复振幅的模的依赖的一阶导数,相对于入射角,被设置为等于零。反过来,在实际的介质中,如农业土壤,从表面反射的垂直极化信号的振幅与反射系数成正比,并且没有明显的最小值,这降低了测量的准确性。在求解三层结构传播介质(空气、上层肥沃土层、地下水位以下土层)的亥姆霍兹波方程的基础上,建立了平面层状介质斜照射下具有损耗的干涉波形成过程模型。利用所建立的模型,确定了影响布鲁斯特角确定精度的因素。首次提出了用垂直偏振干涉波和水平偏振干涉波的振荡相移来测量布鲁斯特角的方法。对已知振幅法和所提出的相位法确定布鲁斯特角的精度进行了比较。实验证实了该方法的充分性。对于实际应用寻找布鲁斯特角的相法来评估土壤的介电常数及其含水率提出了建议。
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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