CH(+) Destruction by Reaction with H: Computing Quantum Rates To Model Different Molecular Regions in the
S Bovino1, T Grassi1, F A Gianturco2,3
1Institut für Astrophysik Georg-August-Universität , Friedrich-Hund Platz 1, 37077 Göttingen, Germany.
The Journal of Physical Chemistry. A
|June 11, 2015
Summary
This study analyzes interstellar carbon chemistry, finding that CH(+) destruction primarily occurs above 100 K. Differences in low-temperature experiments are less relevant for interstellar medium conditions.
Area of Science:
- Astrochemistry
- Interstellar Medium Chemistry
- Quantum Chemistry
Background:
- The carbon chemistry of the interstellar medium (ISM) is crucial for understanding molecular formation.
- CH(+) is a key ion in ISM carbon chemistry, but its abundance is not fully understood.
- Existing experimental and theoretical data on CH(+) destruction rates show discrepancies.
Purpose of the Study:
- To compute accurate ab initio reactive cross sections for a key ionic reaction in ISM carbon chemistry.
- To determine CH(+) destruction rates across a range of temperatures.
- To model the impact of these rates on CH(+) abundance in various ISM environments.
Main Methods:
- Quantum mechanical calculations to compute ab initio reactive cross sections.
- Numerical modeling to obtain CH(+) destruction rates.
- Incorporation of new rates into a complex chemical network using the krome package.
- Solving coupled, first-order kinetics equations to model CH(+) abundance evolution.
Main Results:
- Computed CH(+) destruction rates show good agreement with existing experiments.
- Differences between calculations and low-temperature experiments are linked to collinear approaches and nonadiabatic crossing.
- CH(+) destruction is significant at temperatures above 100 K in astrochemical environments.
- A slight decrease in initial oxygen abundance may lead to higher CH(+) abundances.
Conclusions:
- Low-temperature experimental discrepancies have minimal impact on CH(+) abundance in typical ISM conditions.
- Other chemical processes dominate CH(+) destruction at lower temperatures relevant to ISM.
- A revised understanding of CH(+) destruction and formation pathways may resolve discrepancies in astrochemical models.
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