% IMPORTANT: The following is UTF-8 encoded. This means that in the presence
% of non-ASCII characters, it will not work with BibTeX 0.99 or older.
% Instead, you should use an up-to-date BibTeX implementation like “bibtex8” or
% “biber”.
@ARTICLE{FernndezBayo:135016,
author = {Fernández-Bayo, Jesus D. and Saison, Carine and Voltz,
Marc and Disko, Ulrich and Hofmann, Diana and Berns, Anne
E.},
title = {{C}hlordecone fate and mineralisation in a tropical soil
(andosol) microcosm under aerobic conditions},
journal = {The science of the total environment},
volume = {463-464},
issn = {0048-9697},
address = {Amsterdam [u.a.]},
publisher = {Elsevier Science},
reportid = {FZJ-2013-03020},
pages = {395 - 403},
year = {2013},
abstract = {Chlordecone is a persistent organochlorine insecticide
that, even decades after its ban, poses a threat to the
environment and human health. Nevertheless, its
environmental fate in soils has scarcely been investigated,
and elementary data on its degradation and behaviour in soil
are lacking. The mineralisation and sorption of chlordecone
and the formation of possible metabolites were evaluated in
a tropical agricultural andosol. Soil microcosms with two
different soil horizons (S-A and S-B) were incubated for 215
days with 14C-chlordecone. At five different times (1, 33,
88, 150 and 215 days) the extractability of 14C-chlordecone
was analysed. Mineralisation was monitored using 14CO2 traps
of NaOH. The appearance of metabolites was studied using
thin layer and gas chromatography techniques. At the end of
the experiment, the water soluble 14C-activity was $2\%$ of
the remaining 14C-chlordecone for S-A and $8\%$ for S-B.
Only $12\%$ of the remaining activity was non extractable
and more than $80\%$ remained extractable with organic
solvents. For the first time to our knowledge, a significant
mineralisation of chlordecone was measured in a microcosm
under aerobic conditions $(4.9\%$ for S-A and $3.2\%$ for
S-B of the initial 14C-activity). The drastically lower
emission of 14CO2 in sterilised microcosms indicated the
biological origin of chlordecone mineralisation in the
non-sterilised microcosms. No metabolites could be detected
in the soil extracts. The mineralisation rate of chlordecone
decreased by one order of magnitude throughout the
incubation period. Thus, the chlordecone content in the soil
remained large. This study confirms the existence of
chlordecone degrading organisms in a tropical andosol. The
reasons why their activity is restricted should be
elucidated to allow the development of bioremediation
approaches. Possible reasons are a heterogeneous
distribution a chlordecone between sub-compartments with
different microbial activities or a degradation of
chlordecone by co-metabolic processes controlled by a
limited supply of nutrients.},
cin = {IBG-3},
ddc = {333.7},
cid = {I:(DE-Juel1)IBG-3-20101118},
pnm = {245 - Chemicals in the Environment (POF2-245)},
pid = {G:(DE-HGF)POF2-245},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000325831200046},
doi = {10.1016/j.scitotenv.2013.06.044},
url = {https://juser.fz-juelich.de/record/135016},
}