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@ARTICLE{Jablonowski:13003,
author = {Jablonowski, N. D. and Hamacher, G. and Martinazzo, R. and
Langen, U. and Köppchen, S. and Hofman, D. and Burauel, P.},
title = {{M}etabolism and {P}ersistence of {A}trazine in {S}everal
{F}ield {S}oils with {D}ifferent {A}trazine {A}pplication
{H}istories},
journal = {Journal of agricultural and food chemistry},
volume = {58},
issn = {0021-8561},
address = {Washington, DC [u.a.]},
publisher = {American Chemical Society (ACS)},
reportid = {PreJuSER-13003},
pages = {12869 - 12877},
year = {2010},
note = {Record converted from VDB: 12.11.2012},
abstract = {To assess the potential occurrence of accelerated herbicide
degradation in soils, the mineralization and persistence of
(14)C-labeled and nonlabeled atrazine was evaluated over 3
months in two soils from Belgium (BS, atrazine-treated
1973-2008; BC, nontreated) and two soils from Germany (CK,
atrazine-treated 1986-1989; CM, nontreated). Prior to the
experiment, accelerated solvent extraction of bulk field
soils revealed atrazine (8.3 and 15.2 μg kg(-1)) in BS and
CK soils and a number of metabolites directly after field
sampling, even in BC and CM soils without previous atrazine
treatment, by means of LC-MS/MS analyses. For atrazine
degradation studies, all soils were incubated under
different moisture conditions $(50\%$ maximum soil
water-holding capacity (WHC(max))/slurried conditions). At
the end of the incubation, the (14)C-atrazine mineralization
was high in BS soil (81 and $83\%)$ and also unexpectedly
high in BC soil (40 and $81\%),$ at $50\%$ WHC(max) and
slurried conditions, respectively. In CK soil, the
(14)C-atrazine mineralization was higher (10 and $6\%)$ than
in CM soil (4.7 and $2.7\%),$ but was not stimulated by
slurried conditions. The results revealed that atrazine
application history dramatically influences its degradation
and mineralization. For the incubation period, the amount of
extractable atrazine, composed of residues from freshly
applied atrazine and residues from former field
applications, remained significantly greater (statistical
significance = 99.5 and $99.95\%)$ for BS and CK soils,
respectively, than the amount of extractable atrazine in the
bulk field soils. This suggests that (i) mostly freshly
applied atrazine is accessible for a complex microbial
community, (ii) the applied atrazine is not completely
mineralized and remains extractable even in adapted soils,
and (iii) the microbial atrazine-mineralizing capacity
strongly depends on atrazine application history and appears
to be conserved on long time scales after the last
application.},
keywords = {Agriculture / Atrazine: analysis / Atrazine: metabolism /
Bacteria: metabolism / Biodegradation, Environmental /
Herbicides: analysis / Herbicides: metabolism / Soil:
analysis / Soil Microbiology / Soil Pollutants: analysis /
Soil Pollutants: metabolism / Herbicides (NLM Chemicals) /
Soil (NLM Chemicals) / Soil Pollutants (NLM Chemicals) /
Atrazine (NLM Chemicals) / J (WoSType)},
cin = {IBG-3},
ddc = {630},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {Terrestrische Umwelt},
pid = {G:(DE-Juel1)FUEK407},
shelfmark = {Agriculture, Multidisciplinary / Chemistry, Applied / Food
Science $\&$ Technology},
typ = {PUB:(DE-HGF)16},
pubmed = {pmid:21121649},
UT = {WOS:000285236400042},
doi = {10.1021/jf103577j},
url = {https://juser.fz-juelich.de/record/13003},
}