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@PHDTHESIS{Jonard:132075,
author = {Jonard, Francois},
title = {{S}oil water content estimation using ground-based active
and passive microwave remote sensing: ground-penetrating
radar and radiometer},
school = {Université catholique de Louvain (Belgium)},
type = {Dr.},
address = {Louvain-la-Neuve (Belgium)},
publisher = {UCL},
reportid = {FZJ-2013-01314},
pages = {181 p.},
year = {2012},
note = {Université catholique de Louvain (Belgium), Diss., 2012},
abstract = {Soil water content is widely recognized as a key component
of the water, energy and carbon cycles and knowledge of its
spatiotemporal distribution is in particular needed for
developing optimal and sustainable environmental and
agricultural management strategies. In that context, we
analyzed and further developed advanced groundpenetrating
radar (GPR) and microwave radiometry techniques for
high-resolution mapping and monitoring of shallow soil water
content at the field scale. First, far-field ultra-wideband
GPR and L-band radiometer were used for mapping soil water
content over two test sites with bare soils and the results
were compared to reference ground truths. For GPR, soil
water content was derived from full-wave inversion focusing
on the surface reflection while for radiometer a radiative
transfer model was used. Both techniques provided relatively
good results, especially for reconstructing spatial moisture
patterns in relation to topography and forced conditions
(differential irrigation and soil tilth). Nevertheless,
absolute estimates were subject to inherent discrepancies
that were attributed to the different characterization
scales and local variability. Second, we addressed the
roughness modeling problem. For GPR, we combined the
full-wave GPR model with a roughness model derived from the
Kirchhoff scattering theory. Laboratory experiments showed
that this approach performs well for roughness amplitudes
reaching up to one fourth the wavelength. For the
radiometer, we used an empirical equation which requires
calibrating ground truths. This approach was successfully
validated in field conditions. Finally, GPR and radiometer
measurements were performed over a sand box subject to
hydrostatic equilibrium with a range of water table depths.
For each technique, all measurements were aggregated in an
inversion scheme to reconstruct the vertical water content
profiles, which were constrained using the van Genuchten
water retention equation. The results were in close
agreement with reference timedomain reflectometry
measurements. Our results open promising research and
application perspectives for the joint use of active and
passive microwave remote sensing for soil moisture
retrieval. In that respect, we addressed new avenues for
characterizing crop canopies and water-stress related
phenomena.},
keywords = {Dissertation (GND)},
cin = {IBG-3},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {246 - Modelling and Monitoring Terrestrial Systems: Methods
and Technologies (POF2-246)},
pid = {G:(DE-HGF)POF2-246},
typ = {PUB:(DE-HGF)11},
url = {https://juser.fz-juelich.de/record/132075},
}