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@PHDTHESIS{Izumoto:907312,
author = {Izumoto, Satoshi},
title = {{S}pectral induced polarization of calcite precipitation in
porous media},
volume = {569},
school = {Univ. Stuttgart},
type = {Dissertation},
address = {Jülich},
publisher = {Forschungszentrum Jülich GmbH Zentralbibliothek, Verlag},
reportid = {FZJ-2022-01955},
isbn = {978-3-95806-614-4},
series = {Schriften des Forschungszentrums Jülich Reihe Energie $\&$
Umwelt / Energy $\&$ Environment},
pages = {xviii, 106},
year = {2022},
note = {Dissertation, Univ. Stuttgart, 2021},
abstract = {Precipitation and dissolution dynamics of calcite in
response to variations in groundwater pH andalkalinity are
important in a range of subsurface engineering applications.
In the context of geotechnicalengineering and subsurface
remediation applications, induced calcite precipitation is
widely used. Theeffectiveness of induced calcite
precipitation is typically investigated by measuring
hydraulic pressure,analysing biochemical properties of
sampled solution, and cone penetration tests. However,
thesemethods are spatially and temporally limited, expensive
and laborious. Geophysical methods havepotential to overcome
these limitations. In particular, Spectral Induced
Polarization (SIP) measurementshave been shown to be
sensitive to calcite precipitation. However, previous
experimental studiesshowed inconsistent SIP responses and
have not explored what controls the SIP response of calcite.
Inthis context, the overall aim of this thesis was to better
understand how spatially variable and temporallydynamic
calcite precipitation processes affect the SIP response.In a
first step, the effect of solute concentration on the SIP
response of calcite precipitation wasinvestigated by a
four-phase experiment with SIP measurements on a column
filled with sand. In phaseI, Na2CO3 and CaCl2 solutions were
co-injected, which resulted in a calcite precipitation front
thatincreased the imaginary part of the electrical
conductivity (𝜎"). In phase II, several diluted (but
stilloversaturated) solutions were injected into the sample
with calcite precipitation from phase I, whichresulted in a
decrease of 𝜎". The results suggested that the 𝜎"
associated with calcite depends morestrongly on the solute
conductivity than in the case of sand and sandstone. In
phase III, the solutionsfrom phase I were injected first and
then the injection was stopped. Since calcite precipitation
continuedafter stopping the flow, this resulted in a
decrease of the solute concentration in the mixing zone and
anassociated decrease of 𝜎". In phase IV, the injection
rate of the Na2CO3 solution was reduced relativeto that of
the CaCl2 solution. This shifted the mixing zone away from
the calcite precipitation front andagain the 𝜎"
decreased. These results clearly suggested that the SIP
response of calcite is sensitive tothe solute concentration
near the precipitates.},
cin = {IBG-3},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217)},
pid = {G:(DE-HGF)POF4-2173},
typ = {PUB:(DE-HGF)3 / PUB:(DE-HGF)11},
urn = {urn:nbn:de:0001-2022051828},
url = {https://juser.fz-juelich.de/record/907312},
}