<rdf:RDF xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:dct="http://purl.org/dc/terms/" xmlns:rdf="http://www.w3.org/1999/02/22-rdf-syntax-ns#">
  <rdf:Description rdf:about="https://doi.org/10.1016/j.geoderma.2011.06.014">
    <dct:isReferencedBy>IMPACT4SOIL</dct:isReferencedBy>
    <dct:isReferencedBy>OpenAire</dct:isReferencedBy>
    <dct:isReferencedBy>HAL INRAE</dct:isReferencedBy>
    <dct:isReferencedBy>Crossref</dct:isReferencedBy>
    <dct:isReferencedBy>Microsoft Academic Graph</dct:isReferencedBy>
    <dct:isPartOf>Geoderma</dct:isPartOf>
    <dct:license>Closed Access</dct:license>
    <dct:created>2011-07-23</dct:created>
    <dct:available>2020-05-29</dct:available>
    <dc:description>article i nfo Under long-term cultivation, greater accumulations of soil organic matter (SOM) and phosphorus (P) are found in the surface soil layer under no-till (NT) versus mouldboard ploughing (MP) practices. Our objective was to evaluate the effects of NT and MP practices on concomitant SOM and P distribution and sorption characteristics among water-stable aggregates and non-aggregated particles. The study was conducted in Quebec, Canada, as part of a long-term corn and soybean rotation experiment (established since 1992) on a clay loam soil of the St-Blaise series (Dark Grey Gleysol). Soil samples were collected in the fall of 2007 in the 0-5 cm layer from plots under NT and MP receiving 35 kg P ha -1 and 160 kg N ha -1 . Samples were separated into three water-stable aggregate-sized classes (macro, 2000-250 &#956;m; meso, 250-180 &#956;m; micro, 180- 53 &#956;m) and (silt+clay)-sized particles (b53 &#956;m) using wet-sieving. Macro aggregates made up 60.2 and 48.5% of total soil weight under NT and MP, respectively. In wet-sieved soils from NT plots, water-extractable P (Pw) concentration increased in the order (silt+clay)-sized particlesbmicro-bmeso-bmacro-aggregates; under MP, micro-, meso-, and macro-aggregate fractions had the same Pw concentration, while the (silt+clay)- sized particles showed the lowest Pw concentration. The hierarchy observed among aggregate-sized classes</dc:description>
    <dc:subject>2. Zero hunger</dc:subject>
    <dc:subject>ORGANIC CARBON</dc:subject>
    <dc:subject>[SDV.EE] Life Sciences [q-bio]/Ecology, environment</dc:subject>
    <dc:subject>SOL ARGILO-LIMONEUX</dc:subject>
    <dc:subject>MOULDBOARD PLOUGHING</dc:subject>
    <dc:subject>SOIL AGGREGATION</dc:subject>
    <dc:subject>0401 agriculture, forestry, and fisheries</dc:subject>
    <dc:subject>NO TILL</dc:subject>
    <dc:subject>04 agricultural and veterinary sciences</dc:subject>
    <dc:subject>PHOSPHORUS DYNAMICS</dc:subject>
    <dc:subject>15. Life on land</dc:subject>
    <dc:subject>6. Clean water</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0002-7192-955x"/>
    <dc:creator>Aim&#233; J. Messiga, Aim&#233; J. Messiga, Noura Ziadi, Denis A. Angers, Christian Morel, L&#233;on-E. Parent, </dc:creator>
    <dc:date>2011-09-01</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>article i nfo Under long-term cultivation, greater accumulations of soil organic matter (SOM) and phosphorus (P) are found in the surface soil layer under no-till (NT) versus mouldboard ploughing (MP) practices. Our objective was to evaluate the effects of NT and MP practices on concomitant SOM and P distribution and sorption characteristics among water-stable aggregates and non-aggregated particles. The study was conducted in Quebec, Canada, as part of a long-term corn and soybean rotation experiment (established since 1992) on a clay loam soil of the St-Blaise series (Dark Grey Gleysol). Soil samples were collected in the fall of 2007 in the 0-5 cm layer from plots under NT and MP receiving 35 kg P ha -1 and 160 kg N ha -1 . Samples were separated into three water-stable aggregate-sized classes (macro, 2000-250 &#956;m; meso, 250-180 &#956;m; micro, 180- 53 &#956;m) and (silt+clay)-sized particles (b53 &#956;m) using wet-sieving. Macro aggregates made up 60.2 and 48.5% of total soil weight under NT and MP, respectively. In wet-sieved soils from NT plots, water-extractable P (Pw) concentration increased in the order (silt+clay)-sized particlesbmicro-bmeso-bmacro-aggregates; under MP, micro-, meso-, and macro-aggregate fractions had the same Pw concentration, while the (silt+clay)- sized particles showed the lowest Pw concentration. The hierarchy observed among aggregate-sized classes</dct:abstract>
    <dc:title>Tillage Practices Of A Clay Loam Soil Affect Soil Aggregation And Associated C And P Concentrations</dc:title>
    <dc:identifier>10.1016/j.geoderma.2011.06.014</dc:identifier>
    <dct:references>https://doi.org/10.1016/j.geoderma.2011.06.014</dct:references>
  </rdf:Description>
</rdf:RDF>