Growth of larger hydrocarbons in the ionosphere of titan.
Growth of larger hydrocarbons in the ionosphere of titan.
复制标题
较大的碳氢化合物在泰坦电离层中生长。
DOI:
10.1002/chem.200800524
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发表时间:
2008
期刊:
影响因子:
--
通讯作者:
J. Roithová
中科院分区:
文献类型:
--
作者:
C. L. Ricketts;D. Schröder;C. Alcaraz;J. Roithová
Among the many fascinating results of the Cassini–Huygens mission, the mass spectrum of the ionosphere of Titan has attracted considerable attention. In brief, the ionosphere was found to be surprisingly complex, consisting of hydrocarbon ions CmHn + as well as nitrogen-containing ions CnHnNo + with mass-to-charge ratios up to the probe#s limit of m/z 100; even much heavier components have been proposed. While the formation of CmHn compounds with m 7 is reasonably well understood, routes to larger hydrocarbons are less obvious. Moreover, most of the present models rely on condensation reactions of CmHn + ions with unsaturated precursors such as acetylene, whereas methane, as the major hydrocarbon in the atmosphere of Titan, only plays a minor role in the subsequent growth processes. Here, we report carbon carbon (C C) coupling reactions of methane with medium-sized CmHn 2+ dications leading to larger hydrocarbon molecules. Despite low steady-state concentrations of the dicationic intermediates, kinetic modeling allows predictions about the larger hydrocarbon species present in the ionosphere of Titan, thereby rationalizing the results from the Cassini–Huygens mission which consideration of monocations only cannot explain. The activation of methane poses a particular challenge and usually involves energetic conditions or metal catalysis. Under the conditions of the Titan atmosphere (low temperatures and pressures), small hydrocarbon ions can indeed react with methane, but the rate constants decrease with size, and so far reaction 1 involves the largest CmHn + ion reacting with methane under thermal conditions.