Thermochemical equilibrium calculations of high-temperature O2 generation on the early Earth: Giant asteroid impact on land
Earth’s atmosphere is composed primarily of N2 and O2. The origin of free O2 in the early Earth’s atmosphere is still subject of considerable debate.1 Theoretical models suggest that the initial form of free O2 in the atmosphere has been oceanic H2O. Recent computation modeling has suggested that a...
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| Format: | Article |
| Language: | English |
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Serbian Chemical Society
2003-01-01
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| Series: | Journal of the Serbian Chemical Society |
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| Online Access: | http://www.doiserbia.nb.rs/img/doi/0352-5139/2003/0352-51390302097P.pdf |