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Chlordecone fate and mineralisation in a tropical soil (andosol) microcosm under aerobic conditions

Authors :
Marc Voltz
Jesús D. Fernández-Bayo
Ulrich Disko
Diana Hofmann
Anne E. Berns
Carine Saison
Institut National de la Recherche Agronomique (INRA)
Laboratoire d'étude des Interactions Sol - Agrosystème - Hydrosystème (UMR LISAH)
Institut de Recherche pour le Développement (IRD)-Institut National de la Recherche Agronomique (INRA)-Centre international d'études supérieures en sciences agronomiques (Montpellier SupAgro)-Institut national d’études supérieures agronomiques de Montpellier (Montpellier SupAgro)
Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)-Institut national d'enseignement supérieur pour l'agriculture, l'alimentation et l'environnement (Institut Agro)
Forschungszentrum Jülich GmbH | Centre de recherche de Juliers
Helmholtz-Gemeinschaft = Helmholtz Association
National Program of Human Resource Mobility of the Spanish Ministry of Education [I-D + I 2008-2011]
French Research Agency (ANR-CES)
French National Research Agency [CESA-004]
ANR-08-CESA-0004,CHLORDEXCO,Pollution des sols et des eaux par la chlordécone aux antilles, conséquences sur la contamination des cultures et des organismes dulçaquicoles(2008)
Source :
Science of the Total Environment, Science of the Total Environment, Elsevier, 2013, 463, pp.395-403. ⟨10.1016/j.scitotenv.2013.06.044⟩
Publication Year :
2013
Publisher :
Elsevier BV, 2013.

Abstract

International audience; 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 C-14-chlordecone. At five different times (1, 33, 88, 150 and 215 days) the extractability of C-14-chlordecone was analysed. Mineralisation was monitored using (CO2)-C-14 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 C-14-activity was 2% of the remaining C-14-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 C-14-activity). The drastically lower emission of (CO2)-C-14 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. (C) 2013 Elsevier B.V. All rights reserved.

Details

ISSN :
00489697 and 18791026
Database :
OpenAIRE
Journal :
Science of The Total Environment
Accession number :
edsair.doi.dedup.....c4433ff40b1f44318136e1a051061b0d