arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 0906.3699astro-ph.GAastro-ph.SR
收藏

CO同位素体的光解离和化学:星际云和星周盘的应用

The photodissociation and chemistry of CO isotopologues: applications to interstellar clouds and circumstellar disks

R. Visser, E. F. van Dishoeck, J. H. Black

摘要:

目标。在从星际云到原行星盘的许多天体物理环境中,紫外光离解是CO的一种重要破坏机制。这项工作的目的是更好地了解该过程的深度依赖性和同位素选择性本质。方法.我们提出了一个光解模型的基础上,最近的光谱数据从文献中,这使我们能够计算深度依赖性和同位素选择性的光解速率在更高的精度比以前的工作。该模型包括自屏蔽、相互屏蔽和原子分子氢屏蔽,并且是第一个包括稀有同位素体C17 O和13 C17 O的模型。我们把它耦合到一个简单的化学网络来分析扩散和半透明云,光子占主导地位的地区,和拱星盘中的CO丰度。结果在未衰减的星际辐射场中,光解离速率为2.6 e-10 s^-1,比目前采用的数值高出30%。当温度高于100 K时,增加激发温度或多普勒宽度可使光解速率和同位素选择性降低三倍。该模型再现了对扩散云和PDR观测到的柱密度,并对扩散云中N(12 CO)/N(13 CO)比值的增强和降低提供了解释。C17 O和13 C17 O的光解离分别与C18 O和13 C18 O的光解离显示出几乎完全相同的深度依赖性,因此17 O和18 O相对于16 O被同等地分馏。这支持了最近的假设,即太阳星云中的CO光解是陨石中异常的17 O和18 O丰度的原因。

英文摘要:

Aims. Photodissociation by UV light is an important destruction mechanism for CO in many astrophysical environments, ranging from interstellar clouds to protoplanetary disks. The aim of this work is to gain a better understanding of the depth dependence and isotope-selective nature of this process. Methods. We present a photodissociation model based on recent spectroscopic data from the literature, which allows us to compute depth-dependent and isotope-selective photodissociation rates at higher accuracy than in previous work. The model includes self-shielding, mutual shielding and shielding by atomic and molecular hydrogen, and it is the first such model to include the rare isotopologues C17O and 13C17O. We couple it to a simple chemical network to analyse CO abundances in diffuse and translucent clouds, photon-dominated regions, and circumstellar disks. Results. The photodissociation rate in the unattenuated interstellar radiation field is 2.6e-10 s^-1, 30% higher than currently adopted values. Increasing the excitation temperature or the Doppler width can reduce the photodissociation rates and the isotopic selectivity by as much as a factor of three for temperatures above 100 K. The model reproduces column densities observed towards diffuse clouds and PDRs, and it offers an explanation for both the enhanced and the reduced N(12CO)/N(13CO) ratios seen in diffuse clouds. The photodissociation of C17O and 13C17O shows almost exactly the same depth dependence as that of C18O and 13C18O, respectively, so 17O and 18O are equally fractionated with respect to 16O. This supports the recent hypothesis that CO photodissociation in the solar nebula is responsible for the anomalous 17O and 18O abundances in meteorites.

机构、总结、中文摘要均由AI分析而来,可能存在错误,请以论文正文为准。

↑