<?xml version="1.0"?>
<oai_dc:dc xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:title>Spatial and temporal changes of soil C after establishment of a pasture on a long-term cultivated vertisol (Martinique)</dc:title>
  <dc:creator>/Chevallier, Tiphaine</dc:creator>
  <dc:creator>Voltz, M.</dc:creator>
  <dc:creator>/Blanchart, Eric</dc:creator>
  <dc:creator>/Chotte, Jean-Luc</dc:creator>
  <dc:creator>/Eschenbrenner, Vincent</dc:creator>
  <dc:creator>Mahieu, M.</dc:creator>
  <dc:creator>/Albrecht, Alain</dc:creator>
  <dc:subject>PATURAGE</dc:subject>
  <dc:subject>SOL CULTIVE</dc:subject>
  <dc:subject>SOL DEGRADE</dc:subject>
  <dc:subject>STOCK ORGANIQUE</dc:subject>
  <dc:subject>CARBONE ORGANIQUE</dc:subject>
  <dc:subject>RAPPORT C/N</dc:subject>
  <dc:subject>VARIATION INTERANNUELLE</dc:subject>
  <dc:subject>GEOSTATISTIQUE</dc:subject>
  <dc:description>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. (R&#xE9;sum&#xE9; d'auteur)</dc:description>
  <dc:date>2000</dc:date>
  <dc:type>text</dc:type>
  <dc:identifier>https://www.documentation.ird.fr/hor/fdi:010021104</dc:identifier>
  <dc:identifier>fdi:010021104</dc:identifier>
  <dc:identifier>Chevallier Tiphaine, Voltz M., Blanchart Eric, Chotte Jean-Luc, Eschenbrenner Vincent, Mahieu M., Albrecht Alain. Spatial and temporal changes of soil C after establishment of a pasture on a long-term cultivated vertisol (Martinique). 2000, 94,  43-58</dc:identifier>
  <dc:language>EN</dc:language>
  <dc:coverage>MARTINIQUE</dc:coverage>
</oai_dc:dc>
