Related Experiment Video
Updated: Apr 23, 2026

Atom Probe Tomography Analysis of Exsolved Mineral Phases
Published on: October 25, 2019
The α-β phase transition in volcanic cristobalite
David E Damby1, Edward W Llewellin2, Claire J Horwell3
1Department of Earth Sciences, Durham University, South Road, Durham DH1 3LE, UK ; Institute of Hazard, Risk and Resilience, Durham University, South Road, Durham DH1 3LE, UK ; Department of Earth and Environmental Sciences, Ludwig-Maximilians-Universität München, Munich 80333, Germany.
Volcanic cristobalite, containing aluminum and sodium, transitions between alpha and beta phases at a lower temperature than synthetic cristobalite. This finding impacts respiratory hazard assessments of volcanic ash.
Area of Science:
- Mineralogy and Materials Science
- Geochemistry
- Crystallography
Background:
- Cristobalite is prevalent in volcanic ash from dome-forming eruptions.
- Understanding volcanic cristobalite is crucial for assessing respiratory hazards.
- Al3+ and Na+ substitutions in volcanic cristobalite affect its crystal structure and phase transitions.
Purpose of the Study:
- To investigate the dynamics and energy changes of the alpha-beta phase transition in volcanic cristobalite.
- To compare the transition behavior of volcanic cristobalite with synthetic cristobalite.
Main Methods:
- X-ray powder diffraction with simultaneous in situ heating.
- Differential scanning calorimetry.
Main Results:
- Volcanic cristobalite has a larger cell volume than synthetic cristobalite at ambient temperature.
- Volcanic cristobalite exhibits lower thermal expansion and a lower alpha-beta transition temperature (~473 K) compared to synthetic cristobalite (>543 K).
- The transition displays a hysteresis loop, with coexisting alpha and beta phases, indicating varying transition temperatures among crystals.
Conclusions:
- The presence of Al3+ and Na+ defects influences the phase transition behavior of volcanic cristobalite.
- The unique properties of volcanic cristobalite, including its transition temperature and diffraction pattern, can lead to ambiguity in phase identification.
- These findings are important for accurately assessing the health risks associated with inhaling volcanic ash.
Related Concept Videos
Phase Transitions: Sublimation and Deposition
Phase Transitions: Melting and Freezing
Phase Transitions: Vaporization and Condensation
Phase Transitions
Phase Transitions
Phase Changes
A substance melts or freezes at a temperature called its melting point and boils or condenses at its boiling point. These temperatures depend on pressure. High pressure favors the denser form of the substance, so typically, high pressure...

