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@ARTICLE{Deiana:59377,
author = {Deiana, R. and Cassiani, G. and Kemna, A. and Villa, A. and
Bruno, V. and Bagliani, A.},
title = {{A}n experiment of non-invasive characterization of the
vadose zone via water injection and cross-hole time-lapse
geophysical monitoring},
journal = {Near surface geophysics},
volume = {5},
issn = {1569-4445},
address = {Houten},
publisher = {EAGE},
reportid = {PreJuSER-59377},
pages = {183 - 194},
year = {2007},
note = {Record converted from VDB: 12.11.2012},
abstract = {The characterization of the vadose zone, i.e. the part of
the subsurface above the water table, is a challenging task.
This zone is difficult to access with direct methods without
causing major disturbance to the natural in-situ conditions.
Hence the increasing use of geophysical methods capable of
imaging the water presence in the vadose zone, such as
ground-penetrating radar (GPR) and electrical resistivity
tomography (ERT). This type of monitoring can be applied
both to processes of natural infiltration and to artificial
injection (tracer) tests, by collecting multiple data sets
through time (time-lapse mode). We present the results of a
water-injection experiment conducted at a test site in
Gorgonzola, east of Milan (Italy). The site is characterized
by Quaternary sand and gravel sediments that house an
extensive unconfined aquifer, potentially subject to
pollution from industrial and agricultural sources. ERT and
GPR profiles were acquired in 2D cross-hole configuration
and time-lapse mode over a period of several days preceding
and following the injection of 3.5 m(3) of fresh water in a
purpose-excavated trench. A 3D model of the water- infi
Itrati on experiment was calibrated against the time-lapse
cross-hole data, particularly focusing on the ability of the
model to reproduce the vertical motion of the centre of mass
of the injected water as imaged by GPR and ERT. This model
calibration provided an estimate of the isotropic hydraulic
conductivity of the sediments in the range of 5-10 m/d.
However, all isotropic models overpredict the measured
excess of moisture content, caused by water injection, as
imaged by GPR. The calibration of anisotropic models for the
vertical hydraulic conductivity, with the horizontal
hydraulic conductivity determined by direct measurement,
also leads to a good fit of the sinking of the centre of
mass, with a better mass balance in comparison with field
data. The information derived from the experiment is key to
a quantitative assessment of aquifer vulnerability to
pollutants infiltrating from the surface.},
keywords = {J (WoSType)},
cin = {ICG-4},
ddc = {550},
cid = {I:(DE-Juel1)VDB793},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Geochemistry $\&$ Geophysics},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000247099200004},
url = {https://juser.fz-juelich.de/record/59377},
}