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Published on: June 5, 2014
Molecular dynamics simulations of CO2 formation in interstellar ices
C Arasa1, M C van Hemert, E F van Dishoeck
1Gorlaeus Laboratories, Leiden Institute of Chemistry, Leiden University, P.O. Box 9502, 2300 RA Leiden, The Netherlands.
The formation of carbon dioxide (CO2) ice in interstellar space is explored. Molecular dynamics simulations reveal that while CO2 can form, the HOCO complex is a more probable product, especially when CO is not deep within the ice.
Area of Science:
- Astrochemistry
- Computational Chemistry
- Interstellar Ice Formation
Background:
- Carbon dioxide (CO2) ice is abundant in interstellar ices, alongside water (H2O) and carbon monoxide (CO).
- The precise formation pathways for CO2 ice in interstellar environments remain incompletely understood.
- Ultraviolet (UV) photodissociation of H2O is a known process in space that can generate reactive species.
Purpose of the Study:
- To investigate the formation routes of CO2 ice via UV photodissociation of CO-H2O ice mixtures.
- To determine the relative probabilities of CO2 formation versus other products like the HOCO complex.
- To compare theoretical findings with experimental data on CO2 ice formation pathways.
Main Methods:
- Molecular dynamics simulations were performed on CO-H2O ice systems at 10 K.
- Simulations focused on the ultraviolet photodissociation of H2O and subsequent reactions with CO.
- Different ice surface models were employed to assess the influence of the ice environment.
Main Results:
- The reaction between CO and OH radicals (from H2O photodissociation) can form CO2 ice.
- The HOCO complex is found to be a more probable product than CO2, with a formation probability of (3.00 ± 0.07) × 10(-2) compared to (3.6 ± 0.7) × 10(-4) for CO2.
- CO2 formation is highly dependent on the initial position of CO within the ice; deeper locations favor CO2.
- The HOCO complex is stabilized in the ice, hindering further conversion to CO2.
- The HCO van der Waals complex can form from the reaction of CO with H atoms produced by H2O photodissociation.
Conclusions:
- The reaction of OH with CO is a plausible, though not the most probable, route to CO2 ice formation.
- The formation of the HOCO complex is a significant competing pathway.
- The initial location of CO within interstellar ice structures is a critical factor influencing CO2 ice production.
- Alternative pathways, such as the reaction of photogenerated H atoms with CO, can lead to HCO ice formation.
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