2012
DOI: 10.1016/j.agee.2012.07.005
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Analysis of environmental and farming factors of soil contamination by a persistent organic pollutant, chlordecone, in a banana production area of French West Indies

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Cited by 56 publications
(63 citation statements)
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“…This K oc value is consistent with the reported range in the literature of 2500 to 20,000 cm 3 g -1 (Woignier et al, 2012) and indicates that CLD sorption on the soil is mainly controlled by hydrophobic interactions with soil organic carbon (Cabidoche et al, 2009;Levillain et al, 2012;Li et al, 2012), while inorganic soil components like clay minerals play a relatively minor role, which produces a limited mobility of CLD in soils (Fernandez-Bayo et al, 2013a;. The sorption of SDZ in the same (Kaldenkirchen-Hülst) soil was described in an earlier study (Zarfl, 2008 (Kasteel et al, 2010).…”
Section: Adsorption Of Cld and Sdz On Mwcnts And Soilsupporting
confidence: 81%
“…This K oc value is consistent with the reported range in the literature of 2500 to 20,000 cm 3 g -1 (Woignier et al, 2012) and indicates that CLD sorption on the soil is mainly controlled by hydrophobic interactions with soil organic carbon (Cabidoche et al, 2009;Levillain et al, 2012;Li et al, 2012), while inorganic soil components like clay minerals play a relatively minor role, which produces a limited mobility of CLD in soils (Fernandez-Bayo et al, 2013a;. The sorption of SDZ in the same (Kaldenkirchen-Hülst) soil was described in an earlier study (Zarfl, 2008 (Kasteel et al, 2010).…”
Section: Adsorption Of Cld and Sdz On Mwcnts And Soilsupporting
confidence: 81%
“…These soils have high organic carbon contents compared to nitisols, in the range 2 to 6 %; pH in water is between 5 and 6; and cation exchange capacity ranges between 10 and 29 meq %g. They also have a high infiltration capacity with saturated hydraulic conductivity greater than 60 mm h −1 (Cabidoche et al 2009;Levillain et al 2012). Andosols contain amorphous clay, allophane, which has a completely different microstructure than the phyllosilicate microstructure of classical crystalline clays found in nitisols.…”
Section: Soil Samplesmentioning
confidence: 97%
“…Nowadays, CLD is still present in soils, especially in the densely cultivated areas from south of Basse-Terre (Guadeloupe) (Cabidoche et al, 2009). Although, Fernández-Bayo et al (2013) showed the existence of CLD degrading organisms in a tropical soil (andosol) microcosm under aerobic conditions, CLD undergoes no significant or quick biotic or abiotic degradation (Dolfing et al, 2012;Levillain et al, 2012). Driven by the water cycle, CLD in soils is progressively transferred to aquatic ecosystems (Coat et al, 2011) and also in the food web because of its high K oc (Soil Organic Carbon Water Partitioning Coefficient) (15849 L/Kg), K ow (Octanol-Water Partition Coefficient) (4.5-6.0) and its affinity for lipids (Cabidoche and Lesueur-Jannoyer, 2012;Clostre et al, 2013;Sterrett and Boss, 1977;UNEP, 2005;US-EPA, 2008).…”
Section: Introductionmentioning
confidence: 99%