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Soil Science Society of America Journal 67:478-482 (2003)
© 2003 Soil Science Society of America

DIVISION S-1—SOIL PHYSICS

Estimating Water Content from Electrical Conductivity Measurements with Short Time-Domain Reflectometry Probes

Magnus Persson* and Sahar Haridy

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 ({sigma}a) of soil. The Ka measurement can be converted to water content ({theta}) 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 {sigma}a measurement of short TDR probes for estimating {theta} under conditions with constant soil solution electrical conductivity ({sigma}w) is investigated and the accuracy of the Ka and {sigma}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 {sigma}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 {sigma}w is constant, the {theta} estimations from Ka and {sigma}a measurements have the same accuracy. TDR measurements were taken with the miniature probes in small sand samples. From the Ka{theta} and {sigma}a{theta} relationships determined in the calibration experiment, the Ka and {sigma}a measurements of the miniature probes could be converted to {theta}. The root mean square error (RMSE) of the {theta} estimated by the Ka measurements was 10 to 20 times higher compared with the reference probe measurement. The RMSEs of the {theta} estimated by the {sigma}a measurements was only two to three times higher compared with the reference probes. The results presented in this study clearly show that the {sigma}a measurement made with short TDR probes can give accurate {theta} estimations under conditions of constant {sigma}w.




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