Abstract
When hydrogen, nitrogen and CO are exposed to amorphous iron silicate surfaces at temperatures between 500-900 K a carbonaceous coating forms via Fischer-Tropsch type reactions. Under normal circumstances such a coating would impede or stop further reaction. However, we find that this coating is a better catalyst than the amorphous iron silicates that initiate these reactions. Formation of a self-perpetuating catalytic coating on grain surfaces could explain the rich deposits of macromolecular carbon found in primitive meteorites and would imply that protostellar nebulae should be rich in organic material. © 2008 International Astronomical Union.
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Nuth, J. A., Johnson, N. M., & Manning, S. (2008). A self-perpetuating catalyst for the production of complex organic molecules in protostellar nebulae. In Proceedings of the International Astronomical Union (Vol. 4, pp. 403–408). https://doi.org/10.1017/S1743921308022047
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