首页> 外文会议>Second European Workshop on Exo-Astrobiology Sep 16-19, 2002 Graz, Austria >VARIATION OF C/N AND C/H RATIOS OF TITAN'S AEROSOLS ANALOGUES
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VARIATION OF C/N AND C/H RATIOS OF TITAN'S AEROSOLS ANALOGUES

机译:钛气溶胶模拟物的C / N和C / H比值的变化

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Under the action of the solar radiations and electrons from Saturn's magnetosphere, the gaseous phase of Titan's atmosphere leads to organic aerosols production. The composition of these aerosols on Titan is still unknown, in part due to its complexity. Many experimental simulations have been performed by irradiating N_2:CH_4 gas mixtures with different energy sources in order to reproduce the chemistry of gas and paniculate phases (for a review see Ref. [2]). Even if functional groups of aerosols analogues have been determined using spectroscopy and pyrolysis, their building molecules still remain difficult to identify. However this chemical composition is a key information for Cassini-Huygens experiments in the frame of Titan's atmospheric modeling. We present the first results of the variation of C/N and C/H ratios related to different parameters of experimental simulations of Titan's atmosphere. These data will allow to constraint photochemical models, in order for them to be more realistic. Then the understanding of the mechanism of aerosols formation on Titan as a function of altitude will be easier.
机译:在土星磁层的太阳辐射和电子的作用下,土卫六大气中的气相导致产生有机气溶胶。这些气溶胶在泰坦上的成分仍然未知,部分原因是其复杂性。通过用不同的能量源照射N_2:CH_4气体混合物进行了许多实验模拟,以重现气相和颗粒相的化学性质(综述参见参考文献[2])。即使已经使用光谱学和热解法确定了气溶胶类似物的官能团,它们的结构分子仍然仍然难以鉴定。然而,在泰坦的大气模拟框架中,这种化学成分是卡西尼-惠更斯实验的关键信息。我们介绍了与泰坦大气层实验模拟的不同参数相关的C / N和C / H比变化的第一个结果。这些数据将限制光化学模型,以便使其更逼真。这样,对土卫六上气溶胶形成机理与海拔高度的函数关系的理解就会更加容易。

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