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@ARTICLE{Jelinkova:17432,
author = {Jelinkova, V. and Snehota, M. and Pohlmeier, A. and Van
Dusschoten, D. and Cislerova, M.},
title = {{E}ffects of entrapped residual air bubbles on tracer
transport in heterogeneous soil: {M}agnetic resonance
imaging study},
journal = {Organic geochemistry},
volume = {42},
issn = {0146-6380},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {PreJuSER-17432},
pages = {991 - 998},
year = {2011},
note = {The research was supported by the Czech Science Foundation
Project No. 103/08/1552, by MZP CR SP/2E7/229/07 and by the
Grant Agency of the Czech Technical University in Prague,
Grant No. SGS10/146/OHK1/2T/11. We thank our colleague
Martina Sobotkova from CTU in Prague, for her help with the
experiments and two anonymous reviewers who contributed
helpful comments to this work.},
abstract = {Magnetic resonance imaging (MRI) was used to study the
process of infiltration and solute transport in an
undisturbed soil sample of coarse sandy loam. The sample was
subjected to the recurrent ponded infiltration (RPI)
experiment, which was carried out in order to assess the
changes in the entrapped air volume and its impact on steady
state flow rates and solute breakthrough. The main stages of
the first and second experimental RPI runs were monitored
using an MRI sequence that follows both water density and
magnetic relaxation. In a steady state stage of each
experimental run a nickel nitrate pulse was injected in
order to visualize the solute breakthrough. Effluent from
the sample was collected for chemical analysis and a
breakthrough curve of the nickel was constructed. To obtain
information about the soil structure and to reveal potential
preferential pathways, the soil sample was scanned using
computed tomography. The local nickel ion transport
breakthrough was evaluated from MR images in a series of
local observation points distributed along the selected
preferential pathways.The preferential flow instability
phenomenon with the emphasis on air bubble formation was
shown by detecting a $60\%$ decrease of the steady state
infiltration rate. The detailed analyses of MRI measurements
at observation points revealed air bubble formation,
producing a flow rate decrease accompanied by redirection of
nickel ion transport trajectories. By analyzing M0 maps it
was found that the volumetric water content decrease was
$2.2\%.$ (C) 2011 Elsevier Ltd. All rights reserved.},
keywords = {J (WoSType)},
cin = {IBG-3 / IBG-2},
ddc = {540},
cid = {I:(DE-Juel1)IBG-3-20101118 / I:(DE-Juel1)IBG-2-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Geochemistry $\&$ Geophysics},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000295215300014},
doi = {10.1016/j.orggeochem.2011.03.020},
url = {https://juser.fz-juelich.de/record/17432},
}