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@PHDTHESIS{Tan:878387,
author = {Tan, Xihe},
title = {{D}evelopment of {E}lectromagnetic {I}nduction
{M}easurement and {I}nversion {M}ethods for {S}oil
{E}lectrical {C}onductivity {I}nvestigations},
volume = {62},
school = {RWTH Aachen},
type = {Dissertation},
address = {Jülich},
publisher = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
reportid = {FZJ-2020-02823},
isbn = {978-3-95806-490-4},
series = {Schriften des Forschungszentrums Jülich. Reihe Information
/ Information},
pages = {ix, 124 S.},
year = {2020},
note = {RWTH Aachen, Diss., 2020},
abstract = {Electromagnetic induction (EMI) is a promising contact-free
technique for non-invasive nearsurface geophysical
investigations. Frequency-domain rigid-boom EMI systems with
fixed distances between transmitter (Tx) and receivers (Rx)
have been increasingly used for characterizing the upper
meters (up to depths of approximately 1.5 times the maximum
coil separation) of the subsurface. Such EMI systems enable
the estimation of subsurface electrical conductivity
distributions by inverting the apparent electrical
conductivity (ECa) values measured from multiple different
Tx-Rx configurations. However, calibration issues due to the
thermal effects of the internal electronics as well as
external electromagnetic influences hinder a reliable
quantitative EMI data analysis. For a custom-made EMI
system, a transfer function analyzer (TFA) circuit is
developed to monitor thermal drift effects of the electrical
parameters of the receiver circuit. In addition, ambient
temperature sensors (ATS) were included into the setup.
Here, three correction methods were compared based on data
from ATS, TFA, and a combination of both TFA and ATS. The
presented work tested these three methods in three different
experimental studies where the transmitter unit temperature
is kept constant while the receiver unit is heated and
cooled (1) manually, (2) by cloudy ambient conditions and
(3) by partly sunny weather conditions. The results
demonstrate that the TFA in the receiver circuit provides
suitable data for correcting the phase drift originated
within the receiver coil but not for correcting the drift
caused by electrical components in the read-out circuit. The
latter drifts need to be corrected using ATS data.
Consequently, the combination of TFA and ATS data returned
the best correction results achieving a worst-case accuracy
of 2.3mS/m compared to 10.2mS/m (ATS-only) and 24.9mS/m
(TFA-only). The experimental results indicate that the drift
of the transmitter unit is not negligible and needs to be
corrected by a similar TFA circuit that should be
investigated in future studies. In addition to the thermal
effects, the external electromagnetic influences also shift
the measured ECa data which are caused by the presence of
the operator, cables or metallic objects included in the
field setup. The presented work introduces a novel
multi-elevation [...]},
cin = {ZEA-2},
cid = {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)3 / PUB:(DE-HGF)11},
urn = {urn:nbn:de:0001-2020102027},
url = {https://juser.fz-juelich.de/record/878387},
}