Fig. 2
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Infrared spectra recorded for experiment 4a during the consecutive deposition of O2 (a) and H2O (b), over the 400–4000 cm−1 range. Top (a): no IR band is observed. The small feature around 3300 cm−1 corresponds to saturation of the water feature from crystallized water in the MCT detector. Bottom (b): ν1 + ν3 corresponds to the O–H stretching mode, ν2 to the H2O bending mode, and τ to the water libration mode. The increase in the intensity of these bands over time reflects the growth of the H2O ice thickness. For readability, only the first and last spectra are indicated in the legends.
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