The authors present a numerical one-dimensional model which computes the so
il water content profile, along transmission line probes, from time-domain
reflectometry signal traces recorded with a reflectometer (TDR). Taking a d
iscrete time-domain approach, they first developed a direct iterative model
which computes simulated signal traces from the dielectric constant distri
bution of the propagation medium. The results tallied well with signal trac
es recorded in simple cases. The inverse model was developed in a second st
age, to compute water content distribution along the transmission line prob
es from a reflected signal trace. The results are shown both for controlled
media and field conditions and are compared to direct water content measur
ements. Filtering of the reflection coefficients had to be incorporated to
compensate for the high sensitivity to noise of the iterative computation a
nd the simplicity of the propagation hypothesis. The inverted profiles are
very close to the direct measurements, validating this model for measuremen
ts in low loss soils.