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@ARTICLE{Minet:15984,
author = {Minet, J. and Wahyudi, A. and Bogaert, P. and Vanclooster,
M. and Lambot, S.},
title = {{M}apping shallow soil moisture profiles at the field scale
using full-waveform inversion of ground penetrating radar
data},
journal = {Geoderma},
volume = {161},
issn = {0016-7061},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {PreJuSER-15984},
year = {2011},
note = {The research presented in this paper was funded by the
Belgian Science Policy Office in the frame of the Stereo 11
programme project SR/00/100 (HYDRASENS), the DIGISOIL
project financed by the European Commission under the 7th
Framework Programme for Research and Technological
Development, Area "Environment" Activity 6.3 "Environmental
Technologies," and the Fonds de la Recherche Scientifique
(FNRS), Belgium. We thank Faycal Rejiba for his constructive
review of the paper. Maxime Dupriez is acknowledged for the
field assistance during the field campaign, as well as Guido
Rentmeesters for the GPR platform construction. Access to
the field was given by Christian Rieulaux, farmer at
Walhain-St-Paul.},
abstract = {Full-waveform inversions were applied to retrieve surface,
two-layered and continuous soil moisture profiles from
ground penetrating radar (GPR) data acquired in an 11-ha
agricultural field situated in the loess belt area in
central Belgium. The radar system consisted of a vector
network analyzer combined with an off-ground horn antenna
operating in the frequency range 200-2000 MHz. The GPR
system was computer controlled and synchronized with a
differential GPS for real-time data acquisition. Several
inversion strategies were also tested using numerical
experiments, which in particular demonstrated the
potentiality to reconstruct simplified two-layered
configurations from more complex, continuous dielectric
profiles as prevalent in the environment. The surface soil
moisture map obtained assuming a one-layered model showed a
global moisture pattern mainly explained by the topography
while local moisture patterns indicated a line effect.
Two-layered and profile inversions provided consistent
estimates with respect to each other and field observations,
showing significant moisture increases with depth. However,
some discrepancies were observed between the measured and
modeled GPR data in the higher frequency ranges, mainly due
to surface roughness effects which were not accounted for.
The proposed GPR method and inversion strategies showed
great promise for high-resolution, real-time mapping of soil
moisture at the field scale. (C) 2011 Elsevier B.V. All
rights reserved.},
keywords = {J (WoSType)},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Soil Science},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000288474300013},
doi = {10.1016/j.geoderma.2010.12.023},
url = {https://juser.fz-juelich.de/record/15984},
}