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Measurement of soil water and nutrients by its electrical properties

Abstract An instrument for measurement of soil dielectric constant ϵ r , electrical conductivity EC a, and soil temperature was tested on soils under potato crop to investigate contents of soil volumetric water θ and nutrients for eventual use in a field crop model. To approximate the dependence of θ on ϵ r , a logarithmic equation was chosen. Satisfactory results were obtained on stone-free areas, with the mean relative variance between θ-values determined by dielectric constant and converted from a gravimetric method remaining within the limits of measuring error. However, variances were higher for stony soils, with ϵ r -values at the same θ being considerably higher. To reconcile data from stony and stone-free soils, a formula was composed. Salinity, calculated by a semi-empirical model based on Hilhorst's theory using measured values of EC a, ϵ r , and soil temperature, correlated well with contents of K and Mg in the soil. A lower correlation resulted for P, and was practically absent for Ca. Inequality of these regression equations at different measuring sites demonstrates the necessity of considering soil pH when assessing plant nutrients in the soil.