Fate of nitrogen applied in different fertilizers to the surface of a calcareous soil in Syria

cg.contactc.j.pilbeam@reading.ac.uken_US
cg.contributor.centerInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.contributor.centerUniversity of Reading - UORen_US
cg.contributor.funderUniversity of Reading - UORen_US
cg.contributor.projectCommunication and Documentation Information Services (CODIS)en_US
cg.contributor.project-lead-instituteInternational Center for Agricultural Research in the Dry Areas - ICARDAen_US
cg.coverage.countrySYen_US
cg.coverage.regionWestern Asiaen_US
cg.date.embargo-end-dateTimelessen_US
cg.identifier.doihttps://dx.doi.org/10.1023/A:1016376313823en_US
cg.isijournalISI Journalen_US
cg.issn1385-1314en_US
cg.journalNutrient Cycling in Agroecosystemsen_US
cg.subject.agrovocureaen_US
cg.subject.agrovocdenitrificationen_US
cg.subject.agrovocammonium nitrateen_US
cg.subject.agrovocammonium sulphateen_US
cg.subject.agrovocvolatilizationen_US
cg.volume52en_US
dc.contributorHutchison, Den_US
dc.creatorPilbeam, C Jen_US
dc.date.accessioned2023-09-13T17:45:00Z
dc.date.available2023-09-13T17:45:00Z
dc.description.abstract15N-labelled ammonium sulphate or15N-labelled urea were each applied in solutionat a rate of 30 kg N ha-1 to the surface of 20soil cores (52 mm internal diameter × 100 mm deep)located on a field experiment at the ICARDA station,Tel Hadya, Syria. Recovery of 15N-label in theammonium, nitrate, organic and/or urea-N pools in thesoil was measured on days 0, 1, 2, 5 and 13 afterapplication. Total recovery of 15N was initially100%, but by day 13 after application it had declinedto 51% with urea and 73% with ammonium sulphate.Ammonium nitrate labelled either as ammonium or asnitrate was also applied to the soil surface of 8other cores at the same time. 15N recovery in thefour soil N pools was measured only on day 12 afterapplication. Total recovery of 15N-label was 75%with labelled ammonium and 57% with labelled nitrate.Volatilization of ammonia from this calcareous soil(pH 8.1) is one probable mechanism of N loss fromammonium and urea fertilizers: with nitrate bothleaching beyond the base of the core (i.e. 100 mm) and denitrification were responsible for Nlosses. These large losses of N immediately afterapplication have implications for fertilizermanagement practices.en_US
dc.formatPDFen_US
dc.identifierhttps://mel.cgiar.org/dspace/limiteden_US
dc.identifier.citationC J Pilbeam, D Hutchison. (30/9/1998). Fate of nitrogen applied in different fertilizers to the surface of a calcareous soil in Syria. Nutrient Cycling in Agroecosystems, 52, pp. 55-60.en_US
dc.identifier.statusTimeless limited accessen_US
dc.identifier.urihttps://hdl.handle.net/20.500.11766/68666
dc.languageenen_US
dc.publisherSpringer (part of Springer Nature)en_US
dc.sourceNutrient Cycling in Agroecosystems;52,(1998) Pagination 55-60en_US
dc.subjectfertilizer recoveryen_US
dc.subject15n fertilizeren_US
dc.titleFate of nitrogen applied in different fertilizers to the surface of a calcareous soil in Syriaen_US
dc.typeJournal Articleen_US
dcterms.available1998-09-30en_US
dcterms.extent55-60en_US
mel.impact-factor3.1en_US

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