| タイトル | Lightning and Mass Independent Oxygen Isotopic Fractionation in Nebular Silicates |
| 著者（英） | Nuth, Joseph A. |
| 著者所属（英） | NASA Goddard Space Flight Center |
| 発行日 | 2009-07-05 |
| 言語 | eng |
| 内容記述 | Lightning has long been postulated as the agent of Chondru|e formation in the solar nebula, but it may have an additional role to play as well. Lightning bolts of almost any scale will both vaporize dust and liberate oxygen atoms that will then interact with both nebular gases as well as the refractory silicate vapor as it re-condenses. Such processes should result in the addition of the heavy oxygen isotopes to the growing silicate grains while the light oxygen-16 becomes part of the gas phase water. This process will proceed to some extent throughout the history of any turbulent nebula and will result in the gradual increase of O-16 in the gas phase and in a much larger relative increase in the O-17 and O-18 content of the nebular dust. Laboratory experiments have demonstrated the production of such "heavy oxygen enriched", non-mass-dependently-fractionated dust grains in a high voltage discharge in a hydrogen rich gas containing small quantities of silane, pentacarbonyl iron and oxygen. |
| NASA分類 | Lunar and Planetary Science and Exploration |
| 権利 | No Copyright |
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