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@ARTICLE{Jadoon:3546,
author = {Jadoon, K. Z. and Slob, E. C. and Vanclooster, M. and
Vereecken, H. and Lambot, S.},
title = {{U}niqueness and {S}tability {A}nalysis of
{H}ydrogeophysical {I}nversion for {T}ime-{L}apse
{G}round-{P}enetrating {R}adar {E}stimates of {S}hallow
{S}oil {H}ydraulic {P}roperties},
journal = {Water resources research},
volume = {44},
issn = {0043-1397},
address = {Washington, DC},
publisher = {AGU},
reportid = {PreJuSER-3546},
pages = {W09421},
year = {2008},
note = {This work was supported by the Forschungszentrum Julich
GmbH (Germany), Fonds National de la Recherche Scientifique
(FNRS) and Universite Catholique de Louvain (Belgium), and
Delft University of Technology (Netherlands). The authors
are grateful to Marc Grasmueck, Niklas Linde, an anonymous
reviewer, and Fred Day-Lewis for their constructive comments
for improving the manuscript.},
abstract = {[1] Precise measurement of soil hydraulic properties at
field scales is one of the prerequisites to simulate
subsurface flow and transport processes, which is crucial in
many research and engineering areas. In our study, we
numerically analyze uniqueness and stability for integrated
hydrogeophysical inversion of time-lapse, off-ground
ground-penetrating radar (GPR) data in estimating the
unsaturated soil hydraulic properties. In the inversion,
hydrodynamic modeling based on the one-dimensional (1-D)
Richards equation is used to physically constrain a
full-waveform radar electromagnetic model. Synthetic GPR
data, in terms of 3-D multilayered media Green's functions,
were generated for three different textured soils (coarse,
medium, and fine) and assuming different infiltration
events. Inversion was performed iteratively to estimate
three key soil hydraulic parameters (alpha,n, and K-s) of
the Mualem-van Genuchten model using the global multilevel
coordinate search optimization algorithm. For the coarse-
and medium-textured soils, inversions converged to the
actual solution for all scenarios. For the fine soil,
estimation errors occurred, mainly because of the higher
attenuation of the electromagnetic waves in such a soil
(high electric conductivity). The procedure appeared to be
generally stable with respect to possible errors in the
hydrodynamic and petrophysical model parameterization.
However, we found that particular attention should be given
to an accurate estimation of the saturated water content and
infiltration flux for real field applications. The results
from our numerical experiments suggest that, in theory, the
proposed method is promising for the noninvasive
identification of the shallow soil hydraulic properties at
the field scale with a high spatial resolution.},
keywords = {J (WoSType)},
cin = {ICG-4 / JARA-ENERGY / JARA-SIM},
ddc = {550},
cid = {I:(DE-Juel1)VDB793 / $I:(DE-82)080011_20140620$ /
I:(DE-Juel1)VDB1045},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Environmental Sciences / Limnology / Water Resources},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000259399900003},
doi = {10.1029/2007WR006639},
url = {https://juser.fz-juelich.de/record/3546},
}