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@ARTICLE{Zhao:186333,
author = {Zhao, Yulong and Zimmermann, Egon and Huisman, J. A. and
Treichel, A. and Wolters, Bernd and van Waasen, S. and
Kemna, A.},
title = {{P}hase correction of electromagnetic coupling effects in
cross-borehole {EIT} measurements},
journal = {Measurement science and technology},
volume = {26},
number = {1},
issn = {0957-0233},
address = {Bristol},
publisher = {IOP Publ.},
reportid = {FZJ-2015-00409},
pages = {015801},
year = {2015},
abstract = {Borehole EIT measurements in a broad frequency range (mHz
to kHz) are used to study subsurface geophysical properties.
However, accurate measurements have long been difficult
because the required long electric cables introduce
undesired inductive and capacitive coupling effects.
Recently, it has been shown that such effects can
successfully be corrected in the case of single-borehole
measurements. The aim of this paper is to extend the
previously developed correction procedure for inductive
coupling during EIT measurements in a single borehole to
cross-borehole EIT measurements with multiple borehole
electrode chains. In order to accelerate and simplify the
previously developed correction procedure for inductive
coupling, a pole–pole matrix of mutual inductances is
defined. This consists of the inductances of each individual
chain obtained from calibration measurements and the
inductances between two chains calculated from the known
cable positions using numerical modelling. The new
correction procedure is successfully verified with
measurements in a water-filled pool under controlled
conditions where the errors introduced by capacitive
coupling were well-defined and could be estimated by FEM
forward modelling. In addition, EIT field measurements
demonstrate that the correction methods increase the phase
accuracy considerably. Overall, the phase accuracy of
cross-hole EIT measurements after correction of inductive
and capacitive coupling is improved to better than 1 mrad
up to a frequency of 1 kHz, which substantially improves
our ability to characterize the frequency-dependent complex
electrical resistivity of weakly polarizable soils and
sediments in situ.},
cin = {ZEA-2 / IBG-3},
ddc = {600},
cid = {I:(DE-Juel1)ZEA-2-20090406 / I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255) / 255 - Terrestrial Systems: From Observation to
Prediction (POF3-255)},
pid = {G:(DE-HGF)POF3-255 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000346360300026},
doi = {10.1088/0957-0233/26/1/015801},
url = {https://juser.fz-juelich.de/record/186333},
}