What is it about?
This research focuses on the effect of aluminium on the atomic structure and the physical properties of silicate melts, and of glasses formed by their rapid cooling. We studied how aluminium enters in the melt atomic structure, and how this changes its disorder. We relate this to the ability of the melt to flow, with aluminium playing an important role during the exchanges of chemical bonds required to allow the melt to flow.
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Why is it important?
Aluminium plays a central role in geologic and industrial silicate melts and glasses. For instance, they represent the magmas erupted during volcanic eruptions at Earth surface. They further are used to manufacture various glass products such as handheld device screens or car windshields. Understanding the effect of aluminium on the atomic structure and the physical properties of glasses and melts will help manufacturing glasses less prone to fracture, for instance. It also will allow us to better understand how the mobility of magmas changes in volcanoes as a function of the magma cristallisation history.
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This page is a summary of: The role of Al3+ on rheology and structural changes in sodium silicate and aluminosilicate glasses and melts, Geochimica et Cosmochimica Acta, February 2014, Elsevier,
DOI: 10.1016/j.gca.2013.11.010.
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