% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Minet:19605,
author = {Minet, J. and Lambot, S. and Delaide, G. and Huisman, J.A.
and Vereecken, H. and Vanclooster, M.},
title = {{A} {G}eneralized {F}requency {D}omain {R}eflectometry
{M}odeling {T}echnique for {S}oil {E}lectrical {P}roperties
{D}etermination},
journal = {Vadose zone journal},
volume = {9},
issn = {1539-1663},
address = {Madison, Wis.},
publisher = {SSSA},
reportid = {PreJuSER-19605},
pages = {1063 - 1072},
year = {2010},
note = {This work was supported by the Belgian Science Policy
Office in the frame of the Stereo II program-project
SR/00/100 (HYDRASENS), the DIGISOIL project financed by the
European Commission under the 7th Framework Program for
Research and Technological Development, Area "Environment",
Activity 6.3 "Environmental Technologies", and the Fonds de
la Recherche Scientifique (FNRS, Belgium). The authors are
grateful to David Robinson and two anonymous reviewers for
their constructive comments.},
abstract = {We have developed a generalized frequency domain
reflectometry (FDR) technique for soil characterization that
is based on an electromagnetic model decoupling the cable
and probe head from the ground using frequency-dependent
reflection and transmission transfer functions. The FDR
model represents an exact solution of Maxwell's equations
for wave propagation in one-dimensional multilayered media.
The benefit of the decoupling is that the FDR probe can be
fully described by its characteristic transfer functions,
which are determined using only a few measurements. The soil
properties are retrieved after removing the probe effects
from the raw FDR data by iteratively inverting a global
reflection coefficient. The proposed method was validated
under laboratory conditions for measurements in water with
different salt concentrations and sand with different water
contents. For the salt water, inversions of the data led to
dielectric permittivity and electrical conductivity values
very close to the expected theoretical or measured values.
In the frequency range for which the probe is efficient, a
good agreement was obtained between measured, inverted and
theoretically predicted signals. For the sand, results were
consistent with the different water contents and also in
close agreement with traditional time domain reflectometry
measurements. The proposed method offers great promise for
accurate soil electrical characterization because it
inherently permits maximization of the information that can
be retrieved from the FDR data and shows a high
practicability.},
keywords = {J (WoSType)},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Environmental Sciences / Soil Science / Water Resources},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000287739800023},
doi = {10.2136/vzj2010.0004},
url = {https://juser.fz-juelich.de/record/19605},
}