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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>2018-01-15T15:41:38Z</responseDate> <request identifier=oai:HAL:hal-00408605v1 verb=GetRecord metadataPrefix=oai_dc>http://api.archives-ouvertes.fr/oai/hal/</request> <GetRecord> <record> <header> <identifier>oai:HAL:hal-00408605v1</identifier> <datestamp>2018-01-11</datestamp> <setSpec>type:COMM</setSpec> <setSpec>subject:spi</setSpec> <setSpec>collection:CNRS</setSpec> <setSpec>collection:LCVN</setSpec> <setSpec>collection:GM</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>Effect of stress gradient at the vicinity of a crack tip on ionic diffusion in silicate glasses : an AFM study</title> <creator>Celarie, F.</creator> <creator>Ciccotto, Matteo</creator> <creator>George, Matthieu</creator> <creator>Marliere, Christian</creator> <contributor>Laboratoire des colloïdes, verres et nanomatériaux (LCVN) ; Université Montpellier 2 - Sciences et Techniques (UM2) - Centre National de la Recherche Scientifique (CNRS)</contributor> <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>Fractography of glasses an ceramics V</source> <source>The Fifth Conference on the Fractography of Glasses and Ceramics</source> <coverage>Rochester, United States</coverage> <contributor>James R. Varner J.; Quinn G.; Wightman M.</contributor> <publisher>wiley</publisher> <identifier>hal-00408605</identifier> <identifier>https://hal.archives-ouvertes.fr/hal-00408605</identifier> <source>https://hal.archives-ouvertes.fr/hal-00408605</source> <source>James R. Varner J.; Quinn G.; Wightman M. The Fifth Conference on the Fractography of Glasses and Ceramics, Jun 2006, Rochester, United States. wiley, pp.35, 2007</source> <language>en</language> <subject lang=en>stress gradient</subject> <subject lang=en>silicate glasse</subject> <subject lang=en>AFM study</subject> <subject lang=en>Ionic Diffusion</subject> <subject lang=en>Soda−lime−silica Glass</subject> <subject lang=en>Crack Growth</subject> <subject lang=en>Atomic Force Microscopy</subject> <subject>PACS: 62.20.Mk; 66.30.-h; 68.03.Cd; 68.37.Ps</subject> <subject>[SPI.MAT] Engineering Sciences [physics]/Materials</subject> <type>info:eu-repo/semantics/conferenceObject</type> <type>Conference papers</type> <description lang=en>The slow advance of a crack in sodo-silicate glasses was studied at nanometer scale by in-situ atomic force microscopy (AFM) in a well-controlled atmosphere (N2 and H2O). An enhanced diffusion of sodium ions in the stress-gradient field at the sub-micrometric vicinity of the crack tip was revealed through several effects: growth of nodules in height images, changes in the AFM tip–sample energy dissipation as detected in phase images. Ex-situ chemical micro-analyses completed the AFM measurements. The nodules patterns revealed a dewetting phenomenon evidenced by “breath figures”, i.e. analog to the fogging that occurs when a vapour condenses onto a 'cold' surface [D. Beysens et al., Phys. Rev. Let. 57, 1433 (1986)]. These experimental results were explained by a two-step process: i) a fast migration of sodium ions towards the fracture surfaces as proposed by Langford et al. [J. Mat. Res. 6, 1358 (1991)], ii) a slow backwards diffusion of the cations as evidenced in these AFM experiments (typical time: few minutes). Measurements of the diffusion coefficient of that relaxing process were done at room temperature. Our results strengthen the theoretical concept of a near-surface structural relaxation due to the stress-gradient at the vicinity of the crack tip. Raman and SIMS studies revealed that nodules – for samples studied after exposition to common air - are preferentially covered by an organic overlayer of a carboxylate salt with a long aliphatic chain. The catalytic role of sodium ions in that chemical process is suspected.</description> <date>2006-06-09</date> </dc> </metadata> </record> </GetRecord> </OAI-PMH>