<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/10.1111/sum.12198">
    <dct:isReferencedBy>IMPACT4SOIL</dct:isReferencedBy>
    <dct:isReferencedBy>OpenAire</dct:isReferencedBy>
    <dct:isReferencedBy>Flore (Florence Research Repository)</dct:isReferencedBy>
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    <dct:isReferencedBy>Crossref</dct:isReferencedBy>
    <dct:isReferencedBy>Microsoft Academic Graph</dct:isReferencedBy>
    <dct:isReferencedBy>CNR ExploRA</dct:isReferencedBy>
    <dct:isPartOf>Soil Use and Management</dct:isPartOf>
    <dct:license>Open Access</dct:license>
    <dct:created>2015-07-31</dct:created>
    <dct:available>2024-02-20</dct:available>
    <dct:available>2016-09-07</dct:available>
    <dc:description>Abstract&lt;p&gt;Crop and land management practices affect both the quality and quantity of soil organic matter (SOM) and hence are driving forces for soil organic carbon (SOC) sequestration. The objective of this study was to assess the long&#65506;&#65408;&#65424;term effects of tillage, fertilizer application and crop rotation onSOCin an agricultural area of southern Norway, where a soil fertility and crop rotation experiment was initiated in 1953 and a second experiment on tillage practices was initiated in 1983. The first experiment comprised 6&#65506;&#65408;&#65424;yr crop rotations with cereals only and 2&#65506;&#65408;&#65424;yr cereal and 4&#65506;&#65408;&#65424;yr grass rotations with recommended (base) and more than the recommended (above base) fertilizer application rates; the second experiment dealt with autumn&#65506;&#65408;&#65424;ploughed (conventional&#65506;&#65408;&#65424;till) plots and direct&#65506;&#65408;&#65424;drilled plots (no&#65506;&#65408;&#65424;till). Soil samples at 0&#65506;&#65408;&#65427;10 and 10&#65506;&#65408;&#65427;30&#65474;&#65440;cm depths were collected in autumn 2009 and analysed for their C and N contents. The quality ofSOMin the top layer was determined by13C solid&#65506;&#65408;&#65424;stateNMRspectroscopy. TheSOCstock did not differ significantly because of rotation or fertilizer application types, even after 56&#65474;&#65440;yr. However, the no&#65506;&#65408;&#65424;till system showed a significantly higherSOCstock than the conventional&#65506;&#65408;&#65424;till system at the 0&#65506;&#65408;&#65427;10&#65474;&#65440;cm depth after the 26&#65474;&#65440;yr of experiment, but it was not significantly different at the 10&#65506;&#65408;&#65427;30&#65474;&#65440;cm depth. In terms of quality,SOMwas found to differ by tillage type, rate of fertilizer application and crop rotation. The no&#65506;&#65408;&#65424;till system showed an abundance of O&#65506;&#65408;&#65424;alkyl C, while conventional&#65506;&#65408;&#65424;till system indicated an apparently indirect enrichment in alkyl C, suggesting a more advanced stage ofSOMdecomposition. The long&#65506;&#65408;&#65424;term quantitative and qualitative effects onSOMsuggest that adopting a no&#65506;&#65408;&#65424;tillage system and including grass in crop rotation and farmyard manure in fertilizer application may contribute to preserve soil fertility and mitigate climate change.&lt;/p&gt;</dc:description>
    <dc:subject>Fertilizer application</dc:subject>
    <dc:subject>2. Zero hunger</dc:subject>
    <dc:subject>Crop rotation, fertilizer application, soil organic carbon (SOC), soil organic matter (SOM), tillage, NMR spectroscopy.</dc:subject>
    <dc:subject>NMR spectroscopy</dc:subject>
    <dc:subject>Crop rotation</dc:subject>
    <dc:subject>Soil organic matter (SOM)</dc:subject>
    <dc:subject>13. Climate action</dc:subject>
    <dc:subject>Soil organic carbon (SOC)</dc:subject>
    <dc:subject>0401 agriculture, forestry, and fisheries</dc:subject>
    <dc:subject>04 agricultural and veterinary sciences</dc:subject>
    <dc:subject>15. Life on land</dc:subject>
    <dc:subject>Tillage</dc:subject>
    <dc:creator rdf:resource="https://orcid.org/0000-0003-0405-2038"/>
    <dc:creator>Shrestha, B. M., Singh, B. R., Forte, C., CERTINI, GIACOMO, </dc:creator>
    <dc:date>2015-07-31</dc:date>
    <dc:type>journalpaper</dc:type>
    <dct:abstract>Abstract&lt;p&gt;Crop and land management practices affect both the quality and quantity of soil organic matter (SOM) and hence are driving forces for soil organic carbon (SOC) sequestration. The objective of this study was to assess the long&#65506;&#65408;&#65424;term effects of tillage, fertilizer application and crop rotation onSOCin an agricultural area of southern Norway, where a soil fertility and crop rotation experiment was initiated in 1953 and a second experiment on tillage practices was initiated in 1983. The first experiment comprised 6&#65506;&#65408;&#65424;yr crop rotations with cereals only and 2&#65506;&#65408;&#65424;yr cereal and 4&#65506;&#65408;&#65424;yr grass rotations with recommended (base) and more than the recommended (above base) fertilizer application rates; the second experiment dealt with autumn&#65506;&#65408;&#65424;ploughed (conventional&#65506;&#65408;&#65424;till) plots and direct&#65506;&#65408;&#65424;drilled plots (no&#65506;&#65408;&#65424;till). Soil samples at 0&#65506;&#65408;&#65427;10 and 10&#65506;&#65408;&#65427;30&#65474;&#65440;cm depths were collected in autumn 2009 and analysed for their C and N contents. The quality ofSOMin the top layer was determined by13C solid&#65506;&#65408;&#65424;stateNMRspectroscopy. TheSOCstock did not differ significantly because of rotation or fertilizer application types, even after 56&#65474;&#65440;yr. However, the no&#65506;&#65408;&#65424;till system showed a significantly higherSOCstock than the conventional&#65506;&#65408;&#65424;till system at the 0&#65506;&#65408;&#65427;10&#65474;&#65440;cm depth after the 26&#65474;&#65440;yr of experiment, but it was not significantly different at the 10&#65506;&#65408;&#65427;30&#65474;&#65440;cm depth. In terms of quality,SOMwas found to differ by tillage type, rate of fertilizer application and crop rotation. The no&#65506;&#65408;&#65424;till system showed an abundance of O&#65506;&#65408;&#65424;alkyl C, while conventional&#65506;&#65408;&#65424;till system indicated an apparently indirect enrichment in alkyl C, suggesting a more advanced stage ofSOMdecomposition. The long&#65506;&#65408;&#65424;term quantitative and qualitative effects onSOMsuggest that adopting a no&#65506;&#65408;&#65424;tillage system and including grass in crop rotation and farmyard manure in fertilizer application may contribute to preserve soil fertility and mitigate climate change.&lt;/p&gt;</dct:abstract>
    <dc:title>Long-Term Effects Of Tillage, Nutrient Application And Crop Rotation On Soil Organic Matter Quality Assessed By Nmr Spectroscopy</dc:title>
    <dc:identifier>10.1111/sum.12198</dc:identifier>
    <dct:references>https://doi.org/10.1111/sum.12198</dct:references>
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