Fig. 2: Unpolarised FTIR spectra of omphacite (Obn112 sample).
From: Molecular hydrogen in minerals as a clue to interpret ∂D variations in the mantle

In the Fourier Transform Infra Red (FTIR) spectra, the 2800–5500 cm−1 range show main peaks in the 3000–3800 cm−1 range corresponding to OH and molecular H2O (stretching). Secondary peaks in the 3800–6000 cm−1 interval correspond to molecular H2 (4100 cm−1), Si-OH (4470 cm−1), and molecular water (5200 cm−1). A comparison between unheated and heated samples (500 and 600 °C) shows decreasing intensity of the peak at 4100 cm−1 with increasing temperature. The widening of the peak with increasing H2 content is due to overlapping with two smaller peaks at 4200 and 3950 cm−1. Note that the low intensity of the band at 5200 cm−1 related to molecular water indicates negligible fluid inclusion contributions.