corner
corner

Phys. Rev. B 53, 2155–2158 (1996)

Surface and grain-boundary amorphization: Thermodynamic melting of coesite below the glass transition temperature

Download: PDF (162 kB) Buy this article Export: BibTeX or EndNote (RIS)

W. L. Gong, L. M. Wang, and R. C. Ewing
Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131

Y. Fei
Geophysical Laboratory, Carnegie Institution of Washington, Washington, D.C. 10015

Received 14 June 1995; published in the issue dated 1 February 1996

Coesite, a high-pressure SiO2 polymorph, becomes amorphous during isothermal annealing below the glass transition temperature, Tg, at one-bar pressure. Transmission electron microscopy was used to examine this fusion process (vitrification) below Tg. The transformation is dominated by a heterogeneous nucleation-and-growth controlled process above the thermodynamic melting temperature, Tm (875 K), but below Tg (1480 K). Amorphous domains nucleate at free surfaces and grain boundaries, and the amorphous-crystalline interface propagates into the interior of the crystal. This ‘‘interface-mediated’’ amorphization (vitrification) is the same as ‘‘interface-mediated’’ melting, based on the thermodynamic, microstructural, and mechanistic aspects of the transformation. This amorphization process parallels electron-irradiation and pressure-induced amorphization in coesite. © 1996 The American Physical Society.

© 1996 The American Physical Society

URL:
http://link.aps.org/doi/10.1103/PhysRevB.53.2155
DOI:
10.1103/PhysRevB.53.2155
PACS:
61.16.Bg, 64.60.My, 64.70.Dv, 64.70.Kb