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@ARTICLE{Jablonowski:976,
author = {Jablonowski, N. D. and Koeppchen, S. and Hofmann, D. and
Schaeffer, A. and Burauel, P.},
title = {{S}patial {D}istribution and {C}haracterization of
{L}ong-{T}erm {A}ged 14{C}-{L}abeled {A}trazine {R}esidues
in {S}oil},
journal = {Journal of agricultural and food chemistry},
volume = {56},
number = {20},
issn = {0021-8561},
address = {Washington, DC [u.a.]},
publisher = {American Chemical Society (ACS)},
reportid = {PreJuSER-976},
pages = {9548 - 9554},
year = {2008},
note = {We gratefully acknowledge the help and assistance of the
laboratory co-workers, namely Ms. Anita Steffen and Ms.
Jessica Bausch, for sample preparation, and Mr. Gfinter
Henkelmann, LfL Munich, for the lysimeter soil. Sincere
thanks are due to Mr. M. Michulitz, Ms. H. Lippert, and Ms.
N. Merki, Forschungszentrum Julich (ZCH), for
physicochemical analysis.},
abstract = {The long-term behavior of the herbicide atrazine and its
metabolites in the environment is of continued interest in
terms of risk assessment and soil quality monitoring.
Aqueous desorption, detection, and quantification of
atrazine and its metabolites from an agriculturally used
soil were performed 22 years after the last atrazine
application. A lysimeter soil containing long-term aged
atrazine for >20 years was subdivided into 10 and 5 cm
layers (at the lysimeter bottom: soil 0-50 and 50-55 cm;
fine gravel 55-60 cm depth, implemented for drainage
purposes) to identify the qualitative and quantitative
differences of aged (14)C-labeled atrazine residues
depending on the soil profile and chemico-physical
conditions of the individual soil layers. Deionized water
was used for nonexhaustive cold water shaking extraction of
the soil. With increasing soil depth, the amount of
previously applied (14)C activity decreased significantly
from $8.8\%$ to $0.7\%$ at 55-60 cm depth whereas the
percentage of desorbed (14)C residues in each soil layer
increased from $2\%$ to $6\%$ of the total (14)C activity in
the sample. The only metabolite detectable by means of
LC-MS/MS was 2-hydroxyatrazine while most of the residual
(14)C activity was bound to the soil and was not desorbed.
The amount of desorbed 2-hydroxyatrazine decreased with
increasing soil depth from $21\%$ to $10\%$ of the total
desorbed (14)C residue fraction. The amount of (14)C
residues in the soil layers correlated well with the carbon
content in the soil and in the aqueous soil extracts ( p
value = 0.99 and 0.97, respectively), which may provide
evidence of the binding behavior of the aged atrazine
residues on soil carbon. The lowest coarse layer (55-60 cm)
showed increased residual (14)C activity leading to the
assumption that most (14)C residues were leached from the
soil column over time.},
keywords = {Atrazine: chemistry / Atrazine: metabolism /
Biodegradation, Environmental / Carbon Radioisotopes:
analysis / Chromatography, Liquid / Herbicides: chemistry /
Herbicides: metabolism / Soil: analysis / Soil Pollutants:
chemistry / Soil Pollutants: metabolism / Tandem Mass
Spectrometry / Carbon Radioisotopes (NLM Chemicals) /
Herbicides (NLM Chemicals) / Soil (NLM Chemicals) / Soil
Pollutants (NLM Chemicals) / Atrazine (NLM Chemicals) / J
(WoSType)},
cin = {ICG-4 / ZCH},
ddc = {630},
cid = {I:(DE-Juel1)VDB793 / I:(DE-Juel1)ZCH-20090406},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Agriculture, Multidisciplinary / Chemistry, Applied / Food
Science $\&$ Technology},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:18808141},
UT = {WOS:000260102500033},
doi = {10.1021/jf8017832},
url = {https://juser.fz-juelich.de/record/976},
}