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Evidence for Nb2+ and Ta3+ in silicate melts under highly reducing conditions: A XANES study
-
Camille Cartier
,
Maud Boyet
Published/Copyright:
September 30, 2015
Abstract
Niobium (Nb) K-edge and tantalum (Ta) LIII-edge XANES spectra were acquired at the part-permillion concentration level in silicate glasses quenched from chondritic melts equilibrated at 5 GPa and under moderately to highly reducing conditions (IW-1, IW-4.5, IW-7.9). Standard materials have also been analyzed for Nb and Ta, and the data were used to construct the calibration curves of E0 (threshold energy) vs. valence. Under moderately reducing conditions our results are consistent with niobium and tantalum being mainly pentavalent in the silicate melts as also suggested by previous studies. We do not exclude that at IW-1, a small fraction of Nb and Ta could be reduced, leading to a mean formal valence slightly lower than five. At IW-4.5, Ta is mainly in the form Ta3+, and at IW-7.9, Ta appears to be Ta1+, whereas Nb is divalent (Nb2+). The possibility for Nb and Ta to be present in reduced forms has implications for the behavior of the two elements during the processes of differentiation on planetary bodies formed in the reduced parts of the early Solar System. Element partitioning is a function of size and valence, and our results show that high field strength elements could be reduced, which could change their chemical affinity. This may also be important for the Earth and Moon formation and early differentiation, as exemplified by the “Nb paradox.”
Received: 2015-2-11
Accepted: 2015-4-14
Published Online: 2015-9-30
Published in Print: 2015-10-1
© 2015 by Walter de Gruyter Berlin/Boston
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- Phosphoran olivine overgrowths: Implications for multiple impacts to the Main Group pallasite parent body
- Diffusion of phosphorus in olivine and molten basalt
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- U-Th baddeleyite geochronology and its significance to date the emplacement of silica undersaturated magmas
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