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@ARTICLE{Senbayram:203165,
author = {Senbayram, Mehmet and Bol, Roland and Dixon, Liz and
Fisher, Andrew and Stevens, Carly and Quinton, John and
Fangueiro, David},
title = {{P}otential use of rare earth oxides as tracers of organic
matter in grassland},
journal = {Journal of plant nutrition and soil science},
volume = {178},
number = {2},
issn = {1436-8730},
address = {Weinheim},
publisher = {Wiley-VCH},
reportid = {FZJ-2015-05170},
pages = {288 - 296},
year = {2015},
abstract = {Tracing organic matter (OM) in soil is challenging, because
runoff and leaching processes are interrelated and have
multiple sources. Therefore, multiple tracers with low
background concentrations such as rare earth element oxides
(REOs) are necessary to delineate the origin of sources of
the organic materials in groundwater, rivers or in
catchments. The main objective of this study was to examine
the potential use of REOs as a tracer in various forms of OM
(1) whole slurry, (2) solid, and (3) liquid phase of cattle
slurry after mechanical separation. A laboratory experiment
was carried out using five REOs (La, Gd, Sm, Pr, and Nd
oxides) mixed directly into soil or mixed with various
fractions of cattle slurry and then applied to the soil
surface. In the additional grassland experiment, Gd oxide
was spiked with soil and cattle slurry and then applied to
the soil surface. The mineral N in the liquid phase (urine)
of the slurry in the grassland experiment was labelled with
15N urea (16 $atom\%).$ In the laboratory experiment,
results showed that the five REOs concentration of soil in
0–1 cm soil section after the rainfall simulation was
still up to 20 times more than the background values. In
1–2 cm soil section, the concentration of only Gd (two
fold higher) and La oxides $(50\%$ higher) were
significantly higher than the soil background values.
Therefore, we hypothesized that Gd and La oxides were
associated also with relatively finer organic particles in
slurry, thus 1–2 cm soil section were enriched with these
oxides. The five REOs concentration below 2 cm soil depth
were similar to the background values in all treatments. In
line with the laboratory experiment, Gd concentrations in
the deeper soil layers (2–4 and 4–8 cm) in the grassland
experiment were not significantly affected by any treatment.
Both in grassland and laboratory experiment, solid phase of
the slurry (dung) was collected from the soil surface after
rainfall simulation. Here, about $56\%$ of REOs were
measured on the solid phase of the slurry which indicates
the strong binding potential of REOs on slurry OM. The
present novel study, where REO tagged slurry was uniquely
tested to study geochemical cycle of organic fertilizers,
clearly highlighted the potential for their use as
multiple-tracers of (animal derived-) OM in agricultural
soils.},
cin = {IBG-3},
ddc = {570},
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:000352570800015},
doi = {10.1002/jpln.201400465},
url = {https://juser.fz-juelich.de/record/203165},
}