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    <titleInfo>
      <title>Spatial and temporal changes of soil C after establishment of a pasture on a long-term cultivated vertisol</title>
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      <namePart type="family">Chevallier</namePart>
      <namePart type="given">Tiphaine</namePart>
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    <name type="personnal">
      <namePart type="family">Voltz</namePart>
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      <namePart type="family">Blanchart</namePart>
      <namePart type="given">Eric</namePart>
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    <name type="personnal">
      <namePart type="family">Chotte</namePart>
      <namePart type="given">Jean-Luc</namePart>
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      <namePart type="family">Eschenbrenner</namePart>
      <namePart type="given">Vincent</namePart>
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    <name type="personnal">
      <namePart type="family">Mahieu</namePart>
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    <name type="personnal">
      <namePart type="family">Albrecht</namePart>
      <namePart type="given">Alain</namePart>
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        <roleTerm type="text">auteur</roleTerm>
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    <abstract>In 1991 in Martinique (F.W.I.), a Digitaria decumbens pasture was established on a vertisol that had supported a market-gardening culture for more than 10 years. Organic matter stock restoration was investigated by measuring carbon contents (C contents) and carbon/nitrogen (C/N) ratios each year from 1992 to 1997. Relations between and soil properties (particle-size distribution, soil depth) and C contents were studied. Furthermore, geostatistical analyses of C contents were realised in order to characterise the C storgae in soil at plot scale. The increase of C contents from 1992 (Y0) to 1997 (Y5) was 5 g C/(kg soil) in the topsoil (0-10 cm) and 2.5 g C/kg soil, or 7.5 Mg C/ha, in the 0-30-cm layer. The intensity of organic C storage had a spatial pattern, although the C/N ratio remained homogeneous across the plot. However, there was no correlation between the C increase and the particle-size distribution or the depth of the soil. In the topsoil, the local variability of the C contents increased with time until 1995 and then there was a gradually spreading of this local variability. Plant-cover distribution and physical structure of vertisol could explain the evolution of spatial structure of the soil C content. (Résumé d'auteur)</abstract>
    <targetAudience authority="marctarget">specialized</targetAudience>
    <subject authority="local">
      <topic>PATURAGE</topic>
      <topic>SOL CULTIVE</topic>
      <topic>SOL DEGRADE</topic>
      <topic>STOCK ORGANIQUE</topic>
      <topic>CARBONE ORGANIQUE</topic>
      <topic>RAPPORT C/N</topic>
      <topic>VARIATION INTERANNUELLE</topic>
      <topic>GEOSTATISTIQUE</topic>
    </subject>
    <subject authority="local">
      <geographic>MARTINIQUE</geographic>
    </subject>
    <classification authority="local">068PEDAPP</classification>
    <classification authority="local">076AGRO</classification>
    <relatedItem type="host">
      <titleInfo>
        <title>Geoderma</title>
      </titleInfo>
      <part>
        <detail type="volume">
          <number>94</number>
        </detail>
        <extent unit="pages">
          <list> 43-58</list>
        </extent>
      </part>
      <originInfo>
        <dateIssued>2000</dateIssued>
      </originInfo>
      <identifier type="issn">0016-7061</identifier>
    </relatedItem>
    <identifier type="uri">https://www.documentation.ird.fr/hor/fdi:010021104</identifier>
    <identifier type="doi">10.1016/S0016-7061(99)00064-6</identifier>
    <identifier type="issn">0016-7061</identifier>
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      <url usage="primary display" access="object in context">https://www.documentation.ird.fr/hor/fdi:010021104</url>
      <url access="row object">https://horizon.documentation.ird.fr/exl-doc/pleins_textes/pleins_textes_7/b_fdi_53-54/010021104.pdf</url>
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      <recordCreationDate encoding="w3cdtf">2000-04-17</recordCreationDate>
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        <languageTerm authority="iso639-2b">fre</languageTerm>
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