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Moisture content investigation in the soil samples using microwave dielectric constant measurement method

机译:使用微波介电常数测量法测定土壤样品中的水分含量研究

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The microwaves of typical frequency ranges of 3 GHz to 30 GHz have been in use for remote sensing applications which are progressing rapidly. The microwaves can sense existing moisture in any material that absorbs moisture such as soil or vegetation. In case of soils which may be comprised of variable mix proportionate of solids, liquids or gases and distinct textures subjected to the associated size and the arrangements of soil particles. Hence, the moisture absorption by a specific type of soil used to be different. The inherent physical and electrical properties such as color, texture, grains, dielectric constant, conductivity or permeability, etc. differentiate various soils. In this work, authors present soil moisture measurement by simple estimation of emissivity i.e. the ratio of energy radiated by an object to absorbing the body of same physical temperature. A strategic method of measuring dielectric constant using a microwave signal is used in this research work. The measurement of the dielectric constant of the soils collected from the specific regions and analysis of results has been reported. The proposed method is less complex and can further be used for the identification of soil moisture and agricultural applications.
机译:典型频率范围为3 GHz至30 GHz的微波已用于遥感应用程序,这些应用程序正在迅速发展。微波可以在任何吸收水分如土壤或植被的任何材料中感测现有的水分。在土壤的情况下,可以由可变混合比例的固体,液体或气体和经过相关尺寸的不同纹理和土壤颗粒的布置。因此,通过使用特定类型的土壤吸收的水分吸收。固有的物理和电性能,如颜色,纹理,晶粒,介电常数,导电性或渗透性等。区分各种土壤。在这项工作中,作者通过简单地估计发射率的土壤湿度测量。物体辐射的能量与吸收相同物理温度的主体的比率。使用微波信号测量使用微波信号测量介电常数的战略方法。已经报道了从特定区域收集的土壤的介电常数和结果分析。所提出的方法不太复杂,可以进一步用于识别土壤水分和农业应用。

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