Theoretical infrared signature of OH defects in Fe3+, Cr3+ and Al3+-doped enstatite

This is a Preprint and has not been peer reviewed. The published version of this Preprint is available: https://doi.org/10.1007/s00269-024-01289-2. This is version 2 of this Preprint.

Add a Comment

You must log in to post a comment.


Comments

There are no comments or no comments have been made public for this article.

Downloads

Download Preprint

Authors

Etienne Balan, Jannick Ingrin

Abstract

The infrared spectroscopic properties of selected defects involving one proton and one nearby M3+ (M=Al, Cr, Fe) substitution in orthoenstatite are investigated by first- principles calculations. Based on the theoretical results, the absorption bands experimentally observed on synthetic samples with high crystalline quality and low doping levels can be assigned to specific defect configurations. Most of them correspond to Mg vacancies at M2 sites locally compensated by one proton and one M3+ cation at a nearby M1 site. This confirms that the M3+ + H+ = 2 Mg2+ exchange mechanism is the dominant hydrogen incorporation mechanism at the lowest concentration levels in doped enstatite. At higher concentration levels, more complex incorporation mechanisms could become dominant in Al-bearing samples.

DOI

https://doi.org/10.31223/X5411C

Subjects

Mineral Physics

Keywords

NAMs, infrared spectroscopy, OH defects

Dates

Published: 2024-06-08 08:24

Last Updated: 2024-07-22 21:41

Older Versions
License

CC BY Attribution 4.0 International