Abstract
The α/β-phase-transition of cristobalite (SiO2) shows a stable and reproducible hysteresis loop with phase coexistence on both slopes. The transition proceeds as a function of temperature rather than isothermally. The non-thermally-activated (athermal) behaviour is analogous to martensitic transformations in metals and alloys, and similar to the hysteresis of ferroics in an applied field. The observations suggest that self-pinning by coherency-strain is the cause of the \"thermal’ hysteresis of non-quenchable structure phase transitions. -from Author
Dokumententyp: | Zeitschriftenartikel |
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Fakultät: | Geowissenschaften > Department für Geo- und Umweltwissenschaften > Kristallographie und Materialwissenschaft |
Themengebiete: | 500 Naturwissenschaften und Mathematik > 550 Geowissenschaften, Geologie |
Sprache: | Englisch |
Dokumenten ID: | 18605 |
Datum der Veröffentlichung auf Open Access LMU: | 10. Mrz. 2014, 14:11 |
Letzte Änderungen: | 29. Apr. 2016, 09:15 |