Structural transformation in Ni-bearing Na2Si2O5 glass and melt

Physics

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Chemical Composition, Glass, Melts (Crystal Growth), Nickel Compounds, Pressure Effects, Absorption Spectroscopy, Fine Structure, Geochemistry, Mathematical Models, X Ray Spectroscopy

Scientific paper

The coordination environment around Ni at minor concentration levels (2 wt. % NiO) in Na2Si2O5 glass and melt (293-1250K) has been investigated by Ni K-edge X-ray Absorption Fine Structure (XAFS) spectroscopy. X-ray Absorption Near Edge Structure (XANES) spectra indicate that both Ni IV and Ni V occur in the glass, whereas Ni IV is dominant in the melt. The average anharmonic Ni-O distances derived from XAFS spectra of the glass at 293 K and the melt above 1150 K are 2.00 (+/- 0.02) and 1.97 (+/- 0.02) A, respectively. The Ni-O distance in the glass is consistent with a mixture of Ni IV and Ni V whereas that in the melt is consistent with dominantly Ni V, suggesting a Ni-coordination change during glass melting. This major change in Ni coordination indicates significant reorganization of the melt during quenching and crystallization. These observations for a compositionally- simple melt/glass system may help explain the enrichment of Ni in early-formed igneous materials. They also suggest the possiblity of a pressure-induced coordination change around Ni in the mantle which may influence geochemical modeling of the deep Earth.

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