% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{Pisinaras:857192,
author = {Pisinaras, Vassilios and Panagopoulos, Andreas and
Herrmann, Frank and Bogena, Heye and Doulgeris, Charalampos
and Ilias, Andreas and Tziritis, Evangelos and Wendland,
Frank},
title = {{H}ydrologic and {G}eochemical {R}esearch at {P}inios
{H}ydrologic {O}bservatory: {I}nitial {R}esults},
journal = {Vadose zone journal},
volume = {17},
number = {1},
issn = {1539-1663},
address = {Alexandria, Va.},
publisher = {GeoScienceWorld},
reportid = {FZJ-2018-06429},
pages = {180102},
year = {2018},
abstract = {The Pinios Hydrologic Observatory (PHO) is located in the
River Pinios basin, which is one of the most productive
basins in Greece. The PHO was established to develop deep
knowledge of water balance at the river basin scale and to
improve understanding of the major hydrodynamic mechanisms
to improve hydrological modeling and ultimately sustainable
water resource management. The PHO comprises three
meteorological stations, 12 groundwater monitoring sites,
and one soil moisture monitoring site, which includes
frequency domain reflectometry sensors (SoilNet) and a
cosmic-ray neutron sensor (CRNS) probe. Although the PHO was
recently established (at the end of 2015), the preliminary
findings from data analysis are promising. Calculated
reference evapotranspiration (ETo) gradients demonstrate
differences regarding their annual cycle, total amount, and
altitude level. Moreover, climate analysis indicates
nocturnal mountain-valley winds. Groundwater level spatial
distribution indicates the dominant recharge mechanisms to
the alluvial aquifer system. These findings are also
supported by the hydrochemical data analysis (electrical
conductivity and, secondarily, NO3 distribution). Locally
elevated NO3 concentrations are attributed to agricultural
activities and call for review of the adopted farming
practices. Results from the soil moisture monitoring site
indicate a very good match between the CRNS probe and the
average SoilNet data. Future perspectives of the PHO include
geophysical surveys to accurately delineate the geometry of
the groundwater system, the expansion of groundwater and
soil moisture observation networks, and the application of
the mGROWA hydrologic model to accurately simulate the
hydrological processes in the PHO and upscale in the entire
River Pinios basin. Finally, in support of the local
farmers, we plan to develop and implement a distributed
irrigation programming protocol in the entire area of the
PHO.},
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},
UT = {WOS:000449671600001},
doi = {10.2136/vzj2018.05.0102},
url = {https://juser.fz-juelich.de/record/857192},
}