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The structure of MgO-SiO2 glasses at elevated pressure
Martin Wilding1, Malcolm Guthrie, Shinji Kohara
1Institute of Mathematical and Physical Sciences, Aberystwyth University, Aberystwyth, UK. mbw@aber.ac.uk
Magnesium silicate glasses reveal structural changes under high pressure, with increased Mg-O coordination and Si-O bond connectivity. This research aids understanding of planetary formation processes.
Area of Science:
- Geophysics
- Materials Science
- Mineral Physics
Background:
- The magnesium silicate system is crucial for understanding planetary formation.
- Neutron diffraction provides insights into the structure of glasses and liquids.
Purpose of the Study:
- To investigate structural changes in magnesium silicate glass under high pressure.
- To develop a method for accurate structural characterization of compressed glass.
Main Methods:
- In situ neutron diffraction at high pressure (up to 8.6 GPa).
- Development of a method for calculating the total structure factor, S(Q).
- Reverse Monte Carlo (RMC) simulations for structural analysis.
Main Results:
- Observed changes in chemical ordering with increasing pressure.
- Increased magnesium-oxygen (Mg-O) coordination number.
- Distortion of the local magnesium ion environment and increased Si-O bond connectivity.
Conclusions:
- High pressure induces significant structural modifications in magnesium silicate glass.
- The findings contribute to understanding the behavior of silicate liquids under planetary conditions.
- The study provides a framework for analyzing structure-dependent properties in related materials.
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