A noninvasive approach for measurements of near‐surface water content (θ) and bulk electrical conductivity (σ a ) using time domain reflectometry (TDR) is presented. In this approach, an ordinary three‐rod TDR probe is used together with a polyvinyl chloride (PVC) surface block that surrounds half the measurement volume. Theoretical and experimental results show that an analytical solution of the apparent dielectric constant K a and the σ a of the soil is possible. Thus, the suggested technique does not require a separate calibration of the relationship between the measured effective K a and K a of the soil. The variability of the measurements was shown to be slightly higher than using the traditional approach. The spatial sensitivity of the suggested technique was also investigated. It was shown that using a three‐rod TDR probe with a rod spacing of 0.05 m allows the θ and σ a to be measured in the uppermost 2 cm of the soil.
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Persson et al. (1998) studied this question.
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