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@ARTICLE{HaberPohlmeier:11685,
author = {Haber-Pohlmeier, S. and Bechtold, M. and Stapf, S. and
Pohlmeier, A.},
title = {{W}aterflow {M}onitored by {T}racer {T}ransport in
{N}atural {P}orous {M}edia {U}sing {M}agnetic resonance
{I}maging},
journal = {Vadose zone journal},
volume = {9},
issn = {1539-1663},
address = {Madison, Wis.},
publisher = {SSSA},
reportid = {PreJuSER-11685},
pages = {834 - 845},
year = {2010},
note = {We would like to thank the German Research Foundation (DFG)
for financial support (Sta 511/4-1, PO 746/2-1,
Transregional SFB TR32). We further thank Horst Hardelauf
for support when coupling the finite-volume flow model to
the PARTRACE code, and Ms. Wettengl and Ms. Lippert,
Forschungszentrum Julich, for the chemical analysis of Gd in
the used soil material.},
abstract = {Magnetic resonance imaging (MRI) was applied to the study
of flow processes in model and natural soil cores. Flow
velocities in soils are mostly too slow to be monitored
directly by MRI flow velocity imaging. Therefore, we used
for the first time diethylenetriaminepentaacetate in the
form Gd-DTPA(2-) as a tracer in spin echo multislice imaging
protocols with strong weighting of longitudinal relaxation
time T-1 for probing slow flow velocities in soils. Apart
from its chemical stability, the main advantage of
Gd-DTPA(2-) is the anionic net charge in neutral aqueous
solution. We showed that this property hinders adsorption at
soil mineral surfaces and therefore retardation. We found
that Gd-DTPA(2-) is a very convenient conservative tracer
for the investigation of flow processes in model and natural
soil cores. With respect to the flow processes in the
coaxial model soil column and the natural soil column, we
observed totally different flow patterns. In the first case,
the tracer plume moved quite homogeneously in the inner
highly conductive core only and the migration into the outer
fine material was very limited. A numerical forward
simulation based on independently obtained parameters showed
good agreement between experiment and simulation and thus
proves the convenience of Gd-DTPA as a tracer in MRI for
soil physical investigations. The natural soil core, in
contrast, showed a flow pattern characterized by
preferential paths, avoiding dense regions and preferring
loose structures. In the case of the simpler model column,
the local flow velocities were also calculated by applying a
peak tracking algorithm.},
keywords = {J (WoSType)},
cin = {ICG-4},
ddc = {550},
cid = {I:(DE-Juel1)VDB793},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Environmental Sciences / Soil Science / Water Resources},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000287739800004},
doi = {10.2136/vzj2009.0177},
url = {https://juser.fz-juelich.de/record/11685},
}