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@ARTICLE{Mander:172326,
author = {Mander, Ülo and Well, Reinhard and Weymann, Daniel and
Soosaar, Kaido and Maddison, Martin and Kanal, Arno and
Lõhmus, Krista and Truu, Jaak and Augustin, Jürgen and
Tournebize, Julien},
title = {{I}sotopologue {R}atios of {N} $_{2}$ {O} and {N} $_{2}$
{M}easurements {U}nderpin the {I}mportance of
{D}enitrification in {D}ifferently {N}-{L}oaded {R}iparian
{A}lder {F}orests},
journal = {Environmental science $\&$ technology},
volume = {48},
number = {20},
issn = {0013-936X},
address = {Columbus, Ohio},
publisher = {American Chemical Society},
reportid = {FZJ-2014-05809},
pages = {11910 - 11918},
year = {2014},
abstract = {Known as biogeochemical hotspots in landscapes, riparian
buffer zones exhibit considerable potential concerning
mitigation of groundwater contaminants such as nitrate, but
may in return enhance the risk for indirect N2O emission.
Here we aim to assess and to compare two riparian grey alder
forests in terms of gaseous N2O and N2 fluxes and dissolved
N2O, N2, and NO3- in the near-surface groundwater. We
further determine for the first time isotopologue ratios of
N2O dissolved in the riparian groundwater in order to
support our assumption that it mainly originated from
denitrification. The study sites, both situated in Estonia,
north-eastern Europe, receive contrasting N loads from
adjacent uphill arable land. Whereas N2O emissions were
rather small at both sites, average gaseous N2-to-N2O ratios
inferred from closed-chamber measurements and He-O
laboratory incubations were almost four times smaller for
the heavily loaded site. In contrast, groundwater parameters
were less variable among sites and between landscape
positions. Campaign-based average 15N site preferences of
N2O (SP) in riparian groundwater ranged between 11 and 44
‰. Besides the strong prevalence of N2 emission over N2O
fluxes and the correlation pattern between isotopologue and
water quality data, this comparatively large range
highlights the importance of denitrification and N2O
reduction in both riparian grey alder stands.},
cin = {IBG-3},
ddc = {050},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {246 - Modelling and Monitoring Terrestrial Systems: Methods
and Technologies (POF2-246) / 255 - Terrestrial Systems:
From Observation to Prediction (POF3-255)},
pid = {G:(DE-HGF)POF2-246 / G:(DE-HGF)POF3-255},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000343640900021},
doi = {10.1021/es501727h},
url = {https://juser.fz-juelich.de/record/172326},
}