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arXiv 1903.01232astro-ph.GA
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模拟星际云中的硫损耗

Modeling Sulfur Depletion in Interstellar Clouds

Jacob C. Laas, Paola Caselli

摘要:

星际硫元素从气相中的耗尽一直是天体化学模型面临的一个反复出现的挑战。观测表明,在星际分子云的整个扩散和半透明阶段,硫相对于其宇宙值保持相对非耗尽状态,但其气相成分不能解释这种宇宙值对高密度环境的影响。我们试图解决这个问题,通过模拟星际云从其原始状态的扩散原子云的分子环境的密度高得多,使用气体/颗粒天体化学的演变。代码和增强的硫反应网络。一个共同的气体/粮食反应网络已经系统地更新和大大扩展了以前的点燃的基础上。和模型,重点放在粮食化学和过程。一个简单的模型被用来对由此产生的网络更新进行基准测试,并将模型的结果与文献中的典型天文观测结果进行比较。我们的新的气体/颗粒模型是能够再现元素消耗的硫,硫可以从气相中耗尽两个数量级,这个过程可能会发生在暗云条件下,如果云的化学年龄至少为1百万年。由此产生的颗粒上含硫物质的混合物涵盖了所有最常见的化学元素(H/C/N/O),与彗星环境中观察到的分子没有什么不同。值得注意的是,这种混合物不像所有其他现有的天体化学物质那样仅仅由H2S主导。模型尽管我们的物理模型相对简单,但大多数已知的气相含硫分子丰度在稠密条件下都能准确再现,但预计它们不会是硫的主要分子汇。我们的模型预测,大部分缺失的硫是以谷物上捕获的有机硫物质的形式存在。

英文摘要:

The elemental depletion of interstellar sulfur from the gas phase has been a recurring challenge for astrochemical models. Observations show that sulfur remains relatively non-depleted with respect to its cosmic value throughout the diffuse and translucent stages of an interstellar molecular cloud, but its gas-phase constituents cannot account for this cosmic value towards higher-density environments. We have attempted to address this issue by modeling the evolution of an interstellar cloud from its pristine state as a diffuse atomic cloud to a molecular environment of much higher density, using a gas/grain astrochem. code and an enhanced sulfur reaction network. A common gas/grain reaction network has been systematically updated and greatly extended based on previous lit. and models, with a focus on the grain chemistry and processes. A simple model was used to benchmark the resulting network updates, and the results of the model were compared to typical astronomical observations sourced from the literature. Our new gas/grain model is able to reproduce the elemental depletion of sulfur, whereby sulfur can be depleted from the gas-phase by two orders of magnitude, and this process may occur under dark cloud conditions if the cloud has a chemical age of at least 1 Myrs. The resulting mix of sulfur-bearing species on the grain ranges across all the most common chemical elements (H/C/N/O), not dissimilar to the molecules observed in cometary environments. Notably, this mixture is not dominated simply by H2S, unlike all other current astrochem. models. Despite our relatively simple physical model, most of the known gas-phase S-bearing molecular abundances are accurately reproduced under dense conditions, however they are not expected to be the primary molecular sinks of sulfur. Our model predicts that most of the missing sulfur is in the form of organo-sulfur species trapped on grains.

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