Abstract
1128 The structure and physicochemical properties of silicate and magmatic melts are currently described mostly within the scope of a model representing the structure of melts as an ensemble of silicon–oxygen structural units Q n (where n is the number of bridging oxygen atoms). The concentrations of these structural units depend on the composition and temperature and can be experimentally determined from Raman spec� tra or calculated by means of thermodynamic simula� tions [1–3].
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