Published October 2019
| Version v1
Journal article
Stishovite formation at very low pressures in soda-lime glass
- 1. Department of Materials Science and Engineering, University of California Los Angeles, Los Angeles, CA 90095 (United States)
- 2. Hysitron, Inc., Minneapolis, MN 55344 (United States)
- 3. Department of Mechanical and Aerospace Engineering, University of California Los Angeles, Los Angeles, CA 90095 (United States)
Description
We show for the first time that amorphous soda-lime glass undergoes polymorphic transformation to its densest crystalline stishovite phase at only ~5 GPa of pressure and room temperature, by uniaxially compressing the soda-lime glass nanopillars of 500 nm diameter and observing the post-deformed pillars under transmission electron microscopy. This contrasts with the recent shock-compression experiments of amorphous fused silica glass plates which report a pressure threshold of 34 GPa for stishovite formation. Our findings support recent dislocation dynamics simulations on W pillars which show that small domain size acts as a proxy for high temperature, thereby reducing the pressure threshold.
Additional details
Identifiers
- DOI
- 10.1016/j.scriptamat.2019.06.005;
- PII
- S1359646219303379;
Publishing Information
- Journal Title
- Scripta Materialia
- Journal Volume
- 171
- Journal Page Range
- p. 6-9
- ISSN
- 1359-6462
- CODEN
- SCMAF7
INIS
- Country of Publication
- United Kingdom
- Country of Input or Organization
- International Atomic Energy Agency (IAEA)
- INIS RN
- 55043202
- Subject category
- S36: MATERIALS SCIENCE;
- Descriptors DEI
- COMPUTERIZED SIMULATION; DISLOCATIONS; GLASS; PLATES; SILICA; SODIUM CARBONATES; STISHOVITE; TRANSMISSION ELECTRON MICROSCOPY
- Descriptors DEC
- ALKALI METAL COMPOUNDS; CARBON COMPOUNDS; CARBONATES; CRYSTAL DEFECTS; CRYSTAL STRUCTURE; ELECTRON MICROSCOPY; LINE DEFECTS; MICROSCOPY; MINERALS; OXIDE MINERALS; OXYGEN COMPOUNDS; SIMULATION; SODIUM COMPOUNDS
Optional Information
- Copyright
- Copyright (c) 2019 Acta Materialia Inc. Published by Elsevier Ltd. All rights reserved.