Title : Dynamics of Oxidation of a Fe2+-Bearing Aluminosilicate (Basaltic) Melt

Pub. Date : 1996 Nov 15

PMID : 8895462






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1 Dynamics of Oxidation of a Fe2+-Bearing Aluminosilicate (Basaltic) Melt Rutherford backscattering spectroscopy (RBS) and microscopy demonstrate that the approximately 1400°C oxidation of levitated droplets of a natural Fe2+-bearing aluminosilicate (basalt) melt occurs by chemical diffusion of Fe2+ and Ca2+ to the free surface of the droplet; internal oxidation of the melt results from the required counterflux of electron holes. aluminosilicate ventricular zone expressed PH domain containing 1 Homo sapiens
2 Dynamics of Oxidation of a Fe2+-Bearing Aluminosilicate (Basaltic) Melt Rutherford backscattering spectroscopy (RBS) and microscopy demonstrate that the approximately 1400°C oxidation of levitated droplets of a natural Fe2+-bearing aluminosilicate (basalt) melt occurs by chemical diffusion of Fe2+ and Ca2+ to the free surface of the droplet; internal oxidation of the melt results from the required counterflux of electron holes. aluminosilicate ventricular zone expressed PH domain containing 1 Homo sapiens