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@ARTICLE{Kelter:856109,
author = {Kelter, Matthias and Huisman, Johan Alexander and
Zimmermann, Egon and Vereecken, H.},
title = {{F}ield evaluation of broadband spectral electrical imaging
for soil and aquifer characterization},
journal = {Journal of applied geophysics},
volume = {159},
issn = {0926-9851},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2018-05755},
pages = {484 - 496},
year = {2018},
abstract = {Spectral electrical impedance tomography (EIT) involves the
imaging of the complex electrical distribution in the mHz to
kHz range. Until now, field EIT measurements were limited to
frequencies below 100 Hz because strong electromagnetic
coupling effects associated with longer cables and high
electrode contact impedances prohibit accurate field
measurements at higher frequencies. In this paper, we aim to
evaluate the capability of recent improvements in the
pre-processing and inversion of wideband EIT measurements to
improve the accuracy and spectral consistency of field EIT
measurements of the complex electrical conductivity
distributions in the mHz to kHz frequency range. In a first
case study, time-lapse surface EIT measurements were
performed during an infiltration experiment to investigate
the spectral complex electrical conductivity as a function
of water content. State-of-the-art data processing and
inversion approaches were used to obtain images of the
complex electrical conductivity in a frequency range from
100mHz to 1 kHz, and integral parameters were obtained
using Debye decomposition. Results showed consistent
spectral and spatial variation of the phase of the complex
electrical conductivity in a broad frequency range, and a
complex dependence on water saturation. In a second case
study, borehole EIT measurements were made in a
well-characterized gravel aquifer. These measurements were
inverted to obtain broadband images of the complex
conductivity after correction of inductive coupling effects
using a recently developed correction procedure that relies
on a combination of calibration measurements and model-based
corrections. The inversion results were spatially and
spectrally consistent in a broad frequency range up to
1 kHz only after removal of inductive coupling effects.
Overall, it was concluded that recent improvements in
spectral EIT measurement technology combined with advances
in inversion and data processing now allow accurate
broadband EIT measurements up to 1 kHz.},
cin = {IBG-3 / ZEA-2},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)ZEA-2-20090406},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000453644600048},
doi = {10.1016/j.jappgeo.2018.09.029},
url = {https://juser.fz-juelich.de/record/856109},
}