Abstract

ABSTRACT Widely represented in many arid regions of the world, dry marshes pose a potential threat to the adjacent areas because of soil salinization caused by wind transfer (for long distances) of toxic mineral salts from the dried surface. For environmental monitoring of such soils, remote microwave sensing methods are used. In this work, we study at a 2.3 cm wavelength the summer diurnal dynamics of microwave radiation of sodic solonchak formed on the dried bottom of a hypersaline lake. It has been established that the study indicator (in the centimetre range) depends on the cumulative changes in temperature, moisture and salinity of soils. With rise in soil temperature, intensive evaporation and topsoil drying, a salt crust and the underlying layer with less moisture (accompanied by microwave radiation interference on the layered structure of solonchak) can be formed. In the experiment, a daily variation in the brightness temperature of the study object (a specific object) by 25 K occurred with change in thermodynamic temperature of the skin layer by 10 K.

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