% 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{Bol:851053,
author = {Bol, Roland and Gruau, Gerard and Mellander, Per-Erik and
Dupas, Rémi and Bechmann, Marianne and Skarbøvik, Eva and
Bieroza, Magdalena and Djodjic, Faruk and Glendell, Miriam
and Jordan, Philip and Van der Grift, Bas and Rode, Michael
and Smolders, Erik and Verbeeck, Mieke and Gu, Sen and
Klumpp, Erwin and Pohle, Ina and Fresne, Maelle and
Gascuel-Odoux, Chantal},
title = {{C}hallenges of {R}educing {P}hosphorus {B}ased {W}ater
{E}utrophication in the {A}gricultural {L}andscapes of
{N}orthwest {E}urope},
journal = {Frontiers in Marine Science},
volume = {5},
issn = {2296-7745},
address = {Lausanne},
publisher = {Frontiers Media},
reportid = {FZJ-2018-04766},
pages = {276},
year = {2018},
abstract = {In this paper, we outline several recent insights for the
priorities and challenges for future research for reducing
phosphorus (P) based water eutrophication in the
agricultural landscapes of Northwest Europe. We highlight
that new research efforts best be focused on headwater
catchments as they are a key influence on the initial
chemistry of the larger river catchments, and here many
management interventions are most effectively made. We
emphasize the lack of understanding on how climate change
will impact on P losses from agricultural landscapes.
Particularly, the capability to disentangle current and
future trends in P fluxes, due to climate change itself,
from climate driven changes in agricultural management
practices and P inputs. Knowing that, future climatic change
trajectories for Western Europe will accelerate the release
of the most bioavailable soil P. We stress the ambiguities
created by the large varieties of sources and
storage/transfer processes involved in P emissions in
landscapes and the need to develop specific data treatment
methods or tracers able to circumvent them, thereby helping
catchment managers to identify the ultimate P sources that
most contribute to diffuse P emissions. We point out that
soil and aqueous P exist not only in various chemical forms,
but also in range of less considered physical forms e.g.
dissolved, nanoparticulate, colloidal and other
particulates, all affected differently by climate as well as
other environmental factors, and require bespoke mitigation
measures. We support increased high resolution monitoring of
headwater catchments, to help verify not only the
effectiveness of catchments mitigation strategies, but add
research data to develop new water quality models (e.g.
those include Fe-P interactions) and can deal with climate
and land use change effects within an uncertainty framework.
We finally conclude that there is a crucial need for more
integrative research efforts to deal with our incomplete
understanding of the mechanisms and processes associated
with the identification of critical source areas, P
mobilization, delivery and biogeochemical processing, as
otherwise even high-intensity and high-resolution research
efforts will only reveal an incomplete picture of the full
global impact of the terrestrial derived P on downstream
aquatic and marine ecosystems.},
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:000457365500001},
doi = {10.3389/fmars.2018.00276},
url = {https://juser.fz-juelich.de/record/851053},
}