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@ARTICLE{Bircher:279885,
author = {Bircher, S. and Andreasen, M. and Vuollet, J. and
Vehviläinen, J. and Rautiainen, K. and Jonard, F. and
Weihermüller, L. and Zakharova, E. and Wigneron, J.-P. and
Kerr, Y. H.},
title = {{S}oil moisture sensor calibration for organic soil surface
layers},
journal = {Geoscientific instrumentation, methods and data systems
discussions},
volume = {5},
number = {2},
issn = {2193-0872},
address = {Göttingen},
publisher = {Copernicus Publ.},
reportid = {FZJ-2015-07761},
pages = {447 - 493},
year = {2015},
abstract = {This paper's objective is to present generic calibration
functions for organic surface layers derived for the soil
moisture sensors Decagon ECH2O 5TE and Delta-T ThetaProbe
ML2x, using material from northern regions, mainly from the
Finish Meteorological Institute's Arctic Research Center in
Sodankylä and the study area of the Danish Center for
Hydrology HOBE. For the Decagon 5TE sensor such a function
is currently not reported in literature. Data were compared
with measurements from underlying mineral soils including
laboratory and field measurements. Shrinkage and charring
during drying were considered. For both sensors all field
and lab data showed consistent trends. For mineral layers
with low soil organic matter (SOM) content the validity of
the manufacturer's calibrations was demonstrated. Deviating
sensor outputs in organic and mineral horizons were
identified: for the Decagon 5TE apparent relative
permittivities at a given moisture content decreased for
increased SOM content, which was attributed to an increase
of bound water in organic materials with large surface areas
compared to the studied mineral soils. ThetaProbe
measurements from organic horizons showed stronger
non-linearity in the sensor response and signal saturation
in the high level data. The derived calibration fit
functions between sensor response and volumetric water
content hold for samples spanning a wide range of humus
types with differing SOM characteristics. This strengthens
confidence in their validity under various conditions,
rendering them highly suitable for large-scale applications
in remote sensing and land surface modeling studies.
Agreement between independent Decagon 5TE and ThetaProbe
time series from an organic surface layer at the Sodankylä
site was significantly improved when the here proposed fit
functions were used. Decagon 5TE data also well-reflected
precipitation events. Thus, Decagon 5TE network data from
organic surface layers at the Sodankylä and HOBE sites are
based on the here proposed natural log fit. The newly
derived ThetaProbe fit functions should be used for
hand-held applications only, but in that case proof of value
for the acquisition of instantaneous large-scale soil
moisture estimates.},
cin = {IBG-3},
ddc = {550},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {255 - Terrestrial Systems: From Observation to Prediction
(POF3-255)},
pid = {G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
doi = {10.5194/gid-5-447-2015},
url = {https://juser.fz-juelich.de/record/279885},
}