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    <titleInfo>
      <title>Chlordecone retention in the fractal structure of volcanic clay</title>
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    <abstract>Chlordecone (CHLD), a soil and foodstuff pollutant, as well as an environmentally persistent organochlorine insecticide, was used intensively in banana fields. The chlordecone uptake of three crops was measured for two types of polluted soils: allophanic and non-allophanic. The uptake is lower for allophanic soils even if their chlordecone content is higher than with non-allophanic soils. The fractal structure of the allophane aggregates was characterized at the nanoscale by small angle X-rays scattering, pore size distribution and transmission electron microscopy. We showed that clay microstructures should be an important physico-chemical factor governing the fate of chlordecone in the environment. Allophanic clays result in two counterintuitive findings: higher contaminant trappings yet lower contaminant availability. We propose that this specific, tortuous structure, along with its associated low accessibility, partly explains the low availability of chlordecone confined in allophanic soils. Capsule The fractal and tortuous microstructure of allophane clay favours the chlordecone retention in soils and disfavours the crop uptake.</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject>
      <topic>Chlordecone</topic>
      <topic>Allophanic clay</topic>
      <topic>Fractal microstructure</topic>
      <topic>SAXS</topic>
      <topic>Plant uptake</topic>
    </subject>
    <subject authority="local">
      <geographic>MARTINIQUE</geographic>
    </subject>
    <classification authority="local">068</classification>
    <classification authority="local">021</classification>
    <classification authority="local">076</classification>
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      <titleInfo>
        <title>Journal of Hazardous Materials</title>
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      <part>
        <detail type="volume">
          <number>241</number>
        </detail>
        <extent unit="pages">
          <list> 224-230</list>
        </extent>
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      <originInfo>
        <dateIssued>2012</dateIssued>
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      <identifier type="issn">0304-3894</identifier>
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    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010058848</identifier>
    <identifier type="doi">10.1016/j.jhazmat.2012.09.034</identifier>
    <identifier type="issn">0304-3894</identifier>
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      <recordCreationDate encoding="w3cdtf">2013-03-06</recordCreationDate>
      <recordChangeDate encoding="w3cdtf">2017-08-23</recordChangeDate>
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