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Remote assessment of the degree of soil degradation from radiation properties of soils

机译:通过土壤的辐射特性远程评估土壤退化的程度

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摘要

The effect of the water and salt contents, the soil texture, and the groundwater level on the radiation properties of soils was studied. A methodology was developed for the remote assessment of the degree of soil degradation on the basis of measuring the brightness temperature and emissivity of soils in the microwave region. Criteria based on the remote measurements of radiation parameters of soils for recording changes in the water-physical and other properties of soils, which are necessary for detecting degradation processes at early stages, were substantiated. For the remote assessment of soil degradation, it was proposed to analyze trends in changes with time concerning the emissivities of unfrozen soils occurring at a positive temperature (depending on the soil water content and the groundwater level), the emissivities of frozen nonsaline soils (depending on the soil texture and thermodynamic temperature), and the brightness temperature (depending on the soil salinity and thermodynamic temperature).
机译:研究了水,盐含量,土壤质地和地下水位对土壤辐射特性的影响。在测量微波区域土壤的亮度温度和发射率的基础上,开发了一种用于远程评估土壤退化程度的方法。证实了基于远程测量土壤辐射参数以记录土壤水物理特性和其他特性变化的标准,这对于早期检测降解过程是必要的。为了对土壤退化进行远程评估,建议分析正温度下未冻结土壤的发射率(取决于土壤水含量和地下水位),冻结非盐渍土壤的发射率(取决于时间)的变化趋势。取决于土壤质地和热力学温度)以及亮度温度(取决于土壤盐度和热力学温度)。

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