The time domain reflectometry is a technique used to estimate soil water content (θ) as a function of its apparent dielectric constant (Ka). In this study the main objective was to investigate the consequences of including or not measures of Ka in water on the TDR calibration curve. Three horizons with different clay content were used: 0.13kg kg-1, 0.23kg kg-1 and 0.64kg kg-1. In each horizon, Ka was measured from dry to saturated soil. Additionally, Ka was measured in water. Measurements were made using coaxial cables RGC58, 50 ohms and double stainless rod of 19cm. For each soil two data sets with θ and Ka were formed, one with and another without the addition of Ka measured in water. In each set a cubic polynomial equation was adjusted, estimating θ as a function of Ka. With the inclusion of Ka measured in water the cubic polynomial adjusted better the extreme saturated and avoided errors in the estimated θ. Since there is no certainty that the measures of Ka on field will not be greater than the measures of Ka in the saturated samples in the laboratory, it's recommend to include measures of Ka in water to obtain the calibration curve. Without this procedure and no field verification of Ka measurements, errors in estimated θ of the order of 0.1m3 m-3 can easily occur.
measurement of soil water; reflectometry; dielectric constant.
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