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在泰坦的高层大气中形成氨(NH3)和甲胺(CH2NH)。

Formation of NH3 and CH2NH in Titan's upper atmosphere.

机构信息

Department of Planetary Sciences, University of Arizona, Tucson, AZ 85721, USA.

出版信息

Faraday Discuss. 2010;147:31-49; discussion 83-102. doi: 10.1039/c004787m.

Abstract

The large abundance of NH3 in Titan's upper atmosphere is a consequence of coupled ion and neutral chemistry. The density of NH3 is inferred from the measured abundance of NH4+. NH3 is produced primarily through reaction of NH2 with H2CN, a process neglected in previous models. NH2 is produced by several reactions including electron recombination of CH2NH2+. The density of CH2NH2+ is closely linked to the density of CH2NH through proton exchange reactions and recombination. CH2NH is produced by reaction of N(2D) and NH with ambient hydrocarbons. Thus, production of NH3 is the result of a chain of reactions involving non-nitrile functional groups and the large density of NH3 implies large densities for these associated molecules. This suggests that amine and imine functional groups may be incorporated as well in other, more complex organic molecules.

摘要

土卫六上层大气中大量的氨是离子与中性化学耦合的结果。NH3 的密度是根据测量得到的 NH4+的丰度推断出来的。NH3 主要通过 NH2 与 H2CN 的反应产生,而这一过程在以前的模型中被忽略了。NH2 是通过包括 CH2NH2+的电子复合反应等几种反应产生的。CH2NH2+的密度与 CH2NH 密切相关,通过质子交换反应和复合反应实现。CH2NH 是由 N(2D)和 NH 与周围碳氢化合物反应生成的。因此,NH3 的生成是一系列涉及非腈官能团的反应的结果,而大量的 NH3 意味着这些相关分子的密度也很大。这表明,胺和亚胺官能团也可能与其他更复杂的有机分子一起被包含在内。

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