A multisection model is presented to simulate electromagnetic wave propagat
ion in an unmatched time domain reflectometry (TDR) probe and layered soil
system. The model uses a linear-time-invariant feedback system to model eac
h section and links each section in a bottom-up fashion. Multiple sections
can be incorporated in this model by a simple extension of a single-section
system. An unmatched TDR probe system is modeled by dividing it into equiv
alent sections and matching the simulated waveform with the actual waveform
. The excellent match between the simulated and the recorded waveforms veri
fies the model. This model eliminates the requirement of a matched 50-Ohm p
robe handler in probe design for dielectric measurement. It can also be use
d to assist probe design and TDR data interpretation. The reflected wavefor
ms in layered soil specimens are modeled, and the simulated waveforms are c
ompared to those obtained from experiments. The method of using apparent di
electric constant to obtain average volumetric water content is examined fo
r the layered soil system. The results show that apparent dielectric consta
nt is applicable for the measurement of average volumetric water content fo
r a layered soil, but caution has to be used when interpreting the waveform
s.