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<OAI-PMH schemaLocation=http://www.openarchives.org/OAI/2.0/ http://www.openarchives.org/OAI/2.0/OAI-PMH.xsd> <responseDate>2018-01-15T15:41:11Z</responseDate> <request identifier=oai:HAL:hal-00411933v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00411933v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:ART</setSpec> <setSpec>subject:sdu</setSpec> <setSpec>subject:sde</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:SDE</setSpec> <setSpec>collection:GM</setSpec> <setSpec>collection:GIP-BE</setSpec> <setSpec>collection:AGROPOLIS</setSpec> <setSpec>collection:INSU</setSpec> <setSpec>collection:UNIV-AG</setSpec> <setSpec>collection:B3ESTE</setSpec> <setSpec>collection:UNIV-MONTPELLIER</setSpec> </header> <metadata><dc> <publisher>HAL CCSD</publisher> <title lang=en>Physical and chemical characteristics of particles produced by laser ablation of biogenic calcium carbonate</title> <creator>Hathorne, E. C.</creator> <creator>James, R. H.</creator> <creator>Savage, P.</creator> <creator>Alard, Olivier</creator> <contributor>Géosciences Montpellier ; Université des Antilles et de la Guyane (UAG) - Institut national des sciences de l'Univers (INSU - CNRS) - Université de Montpellier (UM) - Centre National de la Recherche Scientifique (CNRS)</contributor> <description>International audience</description> <source>ISSN: 0267-9477</source> <source>EISSN: 1364-5544</source> <source>Journal of Analytical Atomic Spectrometry</source> <publisher>Royal Society of Chemistry</publisher> <identifier>hal-00411933</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00411933</identifier> <source>https://hal.archives-ouvertes.fr/hal-00411933</source> <source>Journal of Analytical Atomic Spectrometry, Royal Society of Chemistry, 2008, 23 (2), pp.240-243. 〈10.1039/b706727e〉</source> <identifier>DOI : 10.1039/b706727e</identifier> <relation>info:eu-repo/semantics/altIdentifier/doi/10.1039/b706727e</relation> <language>en</language> <subject lang=en>Plasma-mass spectrometry</subject> <subject lang=en>la-icp-ms</subject> <subject lang=en>elemental fractionation</subject> <subject lang=en>generated aerosols</subject> <subject lang=en>size distribution</subject> <subject lang=en>213 nm</subject> <subject lang=en>particulate</subject> <subject lang=en>transport</subject> <subject lang=en>glass</subject> <subject lang=en>microanalysis</subject> <subject>[SDU.STU.GC] Sciences of the Universe [physics]/Earth Sciences/Geochemistry</subject> <subject>[SDE.MCG] Environmental Sciences/Global Changes</subject> <type>info:eu-repo/semantics/article</type> <type>Journal articles</type> <description lang=en>LA-ICP-MS analysis of the chemical composition of biogenic carbonate has many applications in the environmental sciences but the characteristics of the material produced by the ablation process are largely unknown. To fill this gap, we have undertaken a study of the chemical and physical nature of particles produced by laser ablation of biogenic carbonates. SEM imaging suggests that laser ablation produces two distinct particle populations, one consisting of microsize particles and the other of nanosize particles. A 213 nm laser gives rise to a higher proportion of microsize particles than a 193 nm laser, probably because the 213 nm laser couples less completely with carbonate material. The microsize particles appear to form by photomechanical fracturing along lines of cleavage or weakness, rather than by hydrodynamic sputtering (as is generally observed for silicates). Chemical analysis of the carbonate particles suggests that little chemical fractionation of biogenic carbonates occurs during the ablation process or during transport to the plasma. This is supported by the constancy of the fractionation factor ([X/Ca](measured)/[X/Ca] true) during the course of an ablation of a carbonate standard. In contrast, changes in the fractionation factor during the first few seconds of ablation of the NIST 612 are observed for some elements. This difference in fractionation is likely to result from the different formation mechanisms of the microsize particles.</description> <date>2008</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>