Adsorption and Subsequent Reaction of a Water Molecule on Silicate and Silica Cluster Anions

Abstract

We present reactions of size-selected free silicate, Mg<sub><i>l</i></sub>SiO<sub><i>m</i></sub><sup>–</sup>, and silica, Si<sub><i>n</i></sub>O<sub><i>m</i></sub><sup>–</sup>, cluster anions with a H<sub>2</sub>O molecule focusing on H<sub>2</sub>O adsorption. It was found that H<sub>2</sub>O adsorption to Mg<sub><i>l</i></sub>SiO<sub><i>m</i></sub><sup>–</sup> with <i>l</i> = 2 and 3 (<i>m</i> = 4–6) is always followed by molecular oxygen release, whereas reactivity of the clusters with <i>l</i> = 1 (<i>m</i> = 3–5) was found to be much lower. On the contrary, in the reaction of Si<sub><i>n</i></sub>O<sub><i>m</i></sub><sup>–</sup> (<i>n</i> = 3–8, 2<i>n</i> – 1 ≤ <i>m</i> ≤ 2<i>n</i> + 2), a H<sub>2</sub>O adduct is observed as a major reaction product. Larger and oxygen-rich clusters tend to exhibit higher reactivity; the rate constants of the adsorption reaction are 2 orders of magnitude larger than those of CO adsorption previously reported. DFT calculations revealed that H<sub>2</sub>O is dissociatively adsorbed on Si<sub><i>n</i></sub>O<sub><i>m</i></sub><sup>–</sup> to form two SiO<sub>3</sub>(OH) tetrahedra. The site selectivity of H<sub>2</sub>O adsorption is governed by the location of the singly occupied molecular orbital (SOMO) on Si<sub><i>n</i></sub>O<sub><i>m</i></sub><sup>–</sup>. The present findings give molecular-level insights into H<sub>2</sub>O adsorption on silica and silicate species in the interstellar environment

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