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@ARTICLE{Moghadas:22332,
author = {Moghadas, D. and Andre, F. and Bradford, J.H. and van der
Kruk, J. and Vereecken, H. and Lambot, S.},
title = {{E}lectromagnetic induction antenna modelling using a
linear system of complex antenna transfer functions},
journal = {Near surface geophysics},
volume = {10},
number = {3},
issn = {1569-4445},
address = {Houten},
publisher = {EAGE},
reportid = {PreJuSER-22332},
pages = {237 - 247},
year = {2012},
note = {This research was supported by the Forschungszentrum Julich
(FZJ, Germany), Universite catholique de Louvain (UCL,
Belgium), Fonds National de la Recherche Scientifique (FNRS,
Belgium) and Boise State University (BSU, USA) in the
framework of 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". Davood Moghadas is
currently supported by the MUSIS project funded by Deutsche
Forschungsgemeinschaft (DFG, Germany).},
abstract = {The quantitative retrieval of soil apparent electrical
conductivity using electromagnetic induction (EMI) has
remained limited due to strong simplifications regarding EMI
antenna modelling. In this paper, a new technique for EMI
antenna modelling is applied for the common-offset EMI
systems. The EMI system is efficiently described using
global transmission and reflection coefficients and Green's
functions are used to describe wave diffusion for horizontal
and vertical dipole modes. We performed EMI measurements
along a 180-metre-long transect with two different
instrument heights above the soil surface, as well as with
different orientations and frequencies. To ensure proper
retrieval of the soil apparent electrical conductivity, the
reference values were obtained from electrical conductivity
data measured from 11 undisturbed soil cores taken along the
EMI transect. The apparent electrical conductivity values
calculated by applying the proposed model have a good
agreement with reference values, however some discrepancies
can be observed that are mainly attributed to the presence
of local heterogeneities and also errors due to the
variations in the height of the EMI instruments above the
ground. The proposed method appears to be promising for
quantitative retrieval of soil apparent electrical
conductivity and resolving calibration issues that are
typically encountered using EMI. In addition, the model
calibration (antenna transfer functions determination) was
successfully accomplished using conductivity values measured
from the soil cores.},
keywords = {J (WoSType)},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Geochemistry $\&$ Geophysics},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000305376700005},
doi = {10.3997/1873-0604.2012002},
url = {https://juser.fz-juelich.de/record/22332},
}