Abstract
The use of time domain reflectometry allows instantaneous highly accurate location of humidities in a cell filled with a porous medium. The principles and process of the method will be briefly surveyed. Then, reference will be given as to its performances when small quantities of water seep through the porous medium. This technique is likely to be increasingly used in a laboratory for further study of the kinetics of unsaturated flow as well as in a natural medium.
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