Abstract
A model is developed for determining molecular internal energies after O(3P) + SO2(X,1A1) collisions in the Direct Simulation Monte Carlo (DSMC) method in order to improve modeling of the hyperthermal interactions occurring in the upper atmosphere of Io. Molecular Dynamics/Quasi-Classical Trajectory (MD/QCT) studies are conducted to generate post-collision SO2 and post-dissociation SO internal energy distributions as a function of initial SO2 internal energy and relative collision velocity, which are found to be an improvement over the baseline Larsen-Borgnakke (LB) method that often predicts unphysical internal energies above the dissociation energy for non-reacting collisions and under-predicts post-dissociation SO internal energy. An approach for sampling from the MD/QCT-based internal energy distributions in DSMC is developed and DSMC simulations are then conducted for a time-dependent thermal nonequilibrium heat bath using both the MD/QCT-based distributions and the LB model. When only SO2-O collisions are considered, noticeable differences are observed for post-collisional SO2 and SO internal temperatures.
Original language | English (US) |
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Pages (from-to) | 33-44 |
Number of pages | 12 |
Journal | Chemical Physics |
Volume | 443 |
DOIs | |
State | Published - Oct 31 2014 |
Externally published | Yes |
Keywords
- Direct Simulation Monte Carlo
- Planetary simulations
- Post-collision energy distributions
- Quasi-Classical Trajectories
- Thermochemical nonequilibrium
ASJC Scopus subject areas
- General Physics and Astronomy
- Physical and Theoretical Chemistry