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@ARTICLE{Bechtold:17431,
author = {Bechtold, M. and Haber-Pohlmeier, S. and Vanderborght, J.
and Pohlmeier, A. and Ferre, T.P.A. and Verreecken, H.},
title = {{N}ear-surface solute redistribution during evaporation},
journal = {Geophysical research letters},
volume = {38},
issn = {0094-8276},
address = {Washington, DC},
publisher = {American Geophysical Union},
reportid = {PreJuSER-17431},
pages = {L17404},
year = {2011},
note = {We thank Patrick Wunnemann from Aachen university and
Dagmar van Dusschoten of the Eco-NMR center at the IBG-3
(Forschungszentrum Julich) for their help during the MRI
measurements, and Odilia Esser for the dye analysis. Jan
Vanderborght would like to acknowledge the DFG funded
research project Multi-scale Interfaces in Unsaturated Soil
(MUSIS, FOR 1083).},
abstract = {We present results from solute transport experiments in an
evaporating composite porous medium consisting of a
cylindrical inner core with coarse sand that was surrounded
by a mantle with fine sand. Small volumes of dye and salt
tracer were applied at the surface of the fine material of
the evaporating column. The pressure head at the bottom
boundary was kept constant using a hanging water table
ensuring liquid phase continuity to top surface in both fine
and coarse material, whereby the latter was hydraulically
less conductive at these pressure conditions. Contrary to
the expectation that solute accumulation at an evaporating
surface is proportional to local cumulative evaporation,
high concentration spots developed at the surface of the
coarse material, for which IR surface temperature
measurements did not indicate higher evaporation fluxes. 3D
unsaturated flow and transport simulations and a second
tracer experiment monitored with magnetic resonance imaging
(MRI) demonstrated that preferential upward water flux in
the fine sand deeper in the column and near-surface lateral
water flow from the fine into the coarse sand in combination
with a downward diffusive flux are responsible for the local
solute accumulation. We propose that at the wet regions of a
soil surface, solute accumulation is largely decoupled from
local evaporation fluxes and strongly governed by relative
differences of the hydraulic conductivities. The possible
formation of high solute concentration spots at the surface
of coarser regions usually representing preferential flow
pathways during strong precipitation may have an
accelerating effect on the leaching of solutes. Citation:
Bechtold, M., S. Haber-Pohlmeier, J. Vanderborght, A.
Pohlmeier, T. P. A. Ferre, and H. Vereecken (2011),
Near-surface solute redistribution during evaporation,
Geophys. Res. Lett., 38, L17404, doi:10.1029/2011GL048147.},
keywords = {J (WoSType)},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Geosciences, Multidisciplinary},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000294785500001},
doi = {10.1029/2011GL048147},
url = {https://juser.fz-juelich.de/record/17431},
}