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@ARTICLE{Vonberg:155364,
author = {Vonberg, David and Hofmann, Diana and Vanderborght, Jan and
Lelickens, Anna and Köppchen, Stephan and Pütz, Thomas and
Burauel, Peter and Vereecken, Harry},
title = {{A}trazine {S}oil {C}ore {R}esidue {A}nalysis from an
{A}gricultural {F}ield 21 {Y}ears after {I}ts {B}an},
journal = {Journal of environmental quality},
volume = {43},
number = {4},
issn = {0047-2425},
address = {Madison, Wis.},
publisher = {ASA [u.a.]},
reportid = {FZJ-2014-04533},
pages = {1450 -},
year = {2014},
abstract = {Atrazine
(2-chloro-4-ethylamino-6-isopropylamino-1,3,5-triazine)
groundwater monitoring in the Zwischenscholle aquifer in
western Germany revealed concentrations exceeding the
threshold value of 0.1 μg L−1 and increasing
concentration trends even 20 yr after its ban. Accordingly,
the hypothesis was raised that a continued release of bound
atrazine residues from the soil into the Zwischenscholle
aquifer in combination with the low atrazine degradation in
groundwater contributes to elevated atrazine in groundwater.
Three soil cores reaching down to the groundwater table were
taken from an agricultural field where atrazine had been
applied before its ban in 1991. Atrazine residues were
extracted from eight soil layers down to 300 cm using
accelerated solvent extraction and analyzed using liquid
chromatography–tandem mass spectrometry. Extracted
atrazine concentrations ranged between 0.2 and 0.01 μg
kg−1 for topsoil and subsoil, respectively. The extracted
mass from the soil profiles represented $0.07\%$ of the
applied mass, with $0.01\%$ remaining in the top layer. A
complete and instantaneous remobilization of atrazine
residues and vertical mixing with the groundwater body below
would lead to atrazine groundwater concentrations of 0.068
μg L−1. Considering the area where atrazine was applied
in the region and assuming instantaneous lateral mixing in
the Zwischenscholle aquifer would result in a mean
groundwater concentration of 0.002 μg L−1. A conservative
estimation suggests an atrazine half-life value of about 2
yr for the soil zone, which significantly exceeds highest
atrazine half-lives found in the literature (433 d for
subsurface soils). The long-term environmental behavior of
atrazine and its metabolites thus needs to be reconsidered.},
cin = {IBG-3},
ddc = {333.7},
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:000339273000035},
doi = {10.2134/jeq2013.12.0497},
url = {https://juser.fz-juelich.de/record/155364},
}