Abstract
The escape rate of nitrogen from Mars is calculated to be 2.3×10 5 s −1 for low solar flux conditions and 8.9×10 5 s −1 for high solar flux conditions. The major source of energetic atoms is dissociative recombination of ground state and vibrationally excited N 2 + ions. The measured 15 N/ 14 N isotope ratio can be reproduced by postulating an early dense atmosphere during which little differentiation occurred.
Original language | American English |
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Pages (from-to) | 9027-9032 |
Journal | Journal of Geophysical Research: Space Physics |
Volume | 88 |
Issue number | A11 |
DOIs | |
State | Published - Jan 1 1983 |
Keywords
- nitrogen escape
- Mars
Disciplines
- Physics
- The Sun and the Solar System