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Department of Water Resources Engineering, Lund University, Box 118, SE-221 00 Lund, Sweden
* Corresponding author (magnus.persson{at}tvrl.lth.se)
Time domain reflectometry (TDR) is a widely used technique for measuring the dielectric constant (Ka) and bulk electrical conductivity (
a) of soil. The Ka measurement can be converted to water content (
) by means of a (soil specific) calibration. Since the accuracy of the Ka measurement is dependent on the TDR probe length, probes longer than about 0.1 m are preferred. However, shorter probes are desired for many applications. The possible use of the
a measurement of short TDR probes for estimating
under conditions with constant soil solution electrical conductivity (
w) is investigated and the accuracy of the Ka and
a measurements of two reference TDR probes (0.20 m long) and four miniature probes (0.02 m long) is determined. The standard deviation of the Ka measured by the miniature probes was found to be ten times higher compared to the reference probes. The standard deviation of the
a measured by the miniature probes was only slightly larger compared with the reference probes. A calibration experiment in sand using the reference TDR probes showed that when
w is constant, the
estimations from Ka and
a measurements have the same accuracy. TDR measurements were taken with the miniature probes in small sand samples. From the Ka
and
a
relationships determined in the calibration experiment, the Ka and
a measurements of the miniature probes could be converted to
. The root mean square error (RMSE) of the
estimated by the Ka measurements was 10 to 20 times higher compared with the reference probe measurement. The RMSEs of the
estimated by the
a measurements was only two to three times higher compared with the reference probes. The results presented in this study clearly show that the
a measurement made with short TDR probes can give accurate
estimations under conditions of constant
w.
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