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@ARTICLE{Siebers:916964,
author = {Siebers, Nina and Kruse, Jens and Jia, Yunsheng and
Lennartz, Bernd and Koch, Stefan},
title = {{L}oss of subsurface particulate and truly dissolved
phosphorus during various flow conditions along a tile
drain–ditch–brook continuum},
journal = {The science of the total environment},
volume = {866},
issn = {0048-9697},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2023-00230},
pages = {161439 -},
year = {2023},
abstract = {Subsurface losses of colloidal and truly dissolved
phosphorus (P) from arable land can cause ecological damage
to surface water. To gain deeper knowledge about subsurface
particulate P transport from inland sources to brooks, we
studied an artificially drained lowland catchment (1550 ha)
in north-eastern Germany. We took daily samples during the
winter discharge period 2019/2020 at different locations,
i.e., a drain outlet, ditch, and brook, and analyzed them
for total P (TPunfiltered), particulate P >750 nm (TP>750
nm), colloidal P (TPcolloids), and truly dissolved P (truly
DP) during baseflow conditions and high flow events. The
majority of TPunfiltered in the tile drain, ditch, and brook
was formed by TP>750 nm (54 to 59 $\%),$ followed by truly
DP (34 to 38 $\%)$ and a small contribution of TPcolloids (5
to 6 $\%).$ During flow events, 63 to 66 $\%$ of
TPunfiltered was present as particulate P (TP>750 nm +
TPcolloids), whereas during baseflow the figure was 97 to 99
$\%;$ thus, truly DP was almost negligible (1 to 3 $\%$ of
TPunfiltered) during baseflow. We also found that colloids
transported in the water samples have their origin in the
water-extractable nanocolloids (0.66 to 20 nm) within the C
horizon, which are mainly composed of clay minerals. Along
the flow path there is an agglomeration of P-bearing
nanocolloids from the soil, with an increasing importance of
iron(III) (hydr)oxides over clay particles. Event flow
facilitated the transport of greater amounts of larger
particles (>750 nm) through the soil matrix. However, the
discharge did not exhaust colloid mobilization and colloidal
P was exported through the tile-drainage system during the
complete runoff period, even under baseflow conditions.
Therefore, it is essential that the impact of rainfall
intensity and pattern on particulate P discharge be
considered more closely so that drainage management can be
adjusted to achieve a reduced P export from agricultural
land.},
cin = {IBG-3},
ddc = {610},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {2173 - Agro-biogeosystems: controls, feedbacks and impact
(POF4-217)},
pid = {G:(DE-HGF)POF4-2173},
typ = {PUB:(DE-HGF)16},
pubmed = {36623669},
UT = {WOS:000921740300001},
doi = {10.1016/j.scitotenv.2023.161439},
url = {https://juser.fz-juelich.de/record/916964},
}