Interstellar H adsorption and H2 formation on the crystalline (010) forsterite surface: a B3LYP-D2* periodic study
Articolo
Data di Pubblicazione:
2014
Abstract:
The physisorption/chemisorption of atomic hydrogen on a slab model of the Mg 2 SiO 4 forsterite (010)
surface mimicking the interstellar dust particle surface has been modeled using a quantum mechanical
approach based on periodic B3LYP-D2* density functional calculations (DFT) combined with flexible
polarized Gaussian type basis sets, which allows a balanced description of the hydrogen/surface
interactions for both minima and activated complexes. Physisorption of hydrogen is barrierless, very
weak and occurs either close to surface oxygen atoms or on Mg surface ions. The contribution of
dispersion interactions accounts for almost half of the adsorption energy. Both the hydrogen adsorption
energy and barrier to hydrogen jump between equivalent surface sites are overestimated compared to
experimental results meant to simulate the interstellar conditions in the laboratory. The hydrogen atom
exclusively chemisorbs at the oxygen site of the forsterite (010) surface, forming a SiOH surface group
and its spin density being entirely transferred to the neighboring Mg ion. Barrier for chemisorption
allows rapid attachment of H at the surface at 100 K, but prevents the same process from occurring at
10 K. From this H-chemisorbed state, the second hydrogen chemisorption mainly occurs on the
neighboring Mg ion, thus forming a Mg–H surface group, giving rise to a surface species stabilized by
favorable electrostatic interactions between the OH H–Mg pair. The formation of molecular hydrogen
at the (010) forsterite surface adopting a Langmuir–Hinshelwood mechanism takes place either starting
from two physisorbed H atoms with an almost negligible kinetic barrier through a spin–spin coupling
driven reaction or from two chemisorbed H atoms with a barrier surmountable even at T higher than
10 K. We also suggest that a nanosized model of the interstellar dust built from a replica of the forsterite
unit cell is able to adsorb half the energy released by the H 2 formation by increasing its temperature by
about 50 K which could then radiate in about 0.02 s.
Tipologia CRIS:
03A-Articolo su Rivista
Elenco autori:
Javier Navarro-Ruiz;Mariona Sodupe;Piero Ugliengo;Albert Rimola
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