Fractography of ice

descriptionPublicationkeyboard_double_arrow_right Article 01 Oct 1989 English Publisher:Springer Science and Business Media LLCJournal:Journal of Materials Science Letters, volume 8, pages 1,193-1,194 (issn: 0261-8028, eissn: 1573-4811,

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Authors: E. M. Schulson; I. Baker; C. D. Robertson; R. B. Bolon; R. J. Harnimon;

doi: 10.1007/bf01730067

Fractography of ice

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Abstract

Etude experimentale par microscopie electronique analytique. La rupture de la glace a grains fins entre −25 et −50C est une rupture transgranulaire par clivage. Les pores agissent comme sites d'initiation pour les marches de clivage

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