1990IEEE Transactions on Geoscience and Remote SensingRequires access

Microwave remote sensing of soil moisture: elimination of texture effect

P. V. Narasimha Rao, C. Suresh Raju, K. S. Rao

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Abstract

In view of the influence of soil texture on microwave radiation, an attempt is made to eliminate the textural effects on the microwave reflectivity/emission. To determine the appropriate soil moisture parameter that minimizes the textural influences on microwave radiation from soils, soil moisture is expressed in terms of gravimetric and volumetric units and percentage of field capacity (M/sub fc/) and is plotted individually against the microwave reflectivity of soils. Only when soil moisture is in volumetric units are the textural influences significantly reduced. Therefore, a parameter, termed the critical water content (W/sub c/), that takes into account the bound-water content of soils is used. An empirical relation between the interpolated values of W/sub c/ and the wilting point of soils has been developed. The soil water content above the W/sub c/ of each soil is considered as effective water M/sub eff/.>

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In view of the influence of soil texture on microwave radiation, an attempt is made to eliminate the textural effects on the microwave reflectivity/emission. To determine the appropriate soil moisture parameter that minimizes the textural influences on microwave radiation from soils, soil moisture is expressed in terms of gravimetric and volumetric units and percentage of field capacity (M/sub fc/) and is plotted individually against the microwave reflectivity of soils. Only when soil moisture is in volumetric units are the textural influences significantly reduced. Therefore, a parameter, termed the critical water content (W/sub c/), that takes into account the bound-water content of soils is used. An empirical relation between the interpolated values of W/sub c/ and the wilting point of soils has been developed. The soil water content above the W/sub c/ of each soil is considered as effective water M/sub eff/.>

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Available abstract

In view of the influence of soil texture on microwave radiation, an attempt is made to eliminate the textural effects on the microwave reflectivity/emission. To determine the appropriate soil moisture parameter that minimizes the textural influences on microwave radiation from soils, soil moisture is expressed in terms of gravimetric and volumetric units and percentage of field capacity (M/sub fc/) and is plotted individually against the microwave reflectivity of soils. Only when soil moisture is in volumetric units are the textural influences significantly reduced. Therefore, a parameter, termed the critical water content (W/sub c/), that takes into account the bound-water content of soils is used. An empirical relation between the interpolated values of W/sub c/ and the wilting point of soils has been developed. The soil water content above the W/sub c/ of each soil is considered as effective water M/sub eff/.>

Key concepts: Permanent wilting point, Water content, Soil water, Soil texture, Soil science, Microwave, Moisture, Environmental science

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