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arXiv 0807.1447astro-ph
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低质量原恒星IRAS 16293-2422的干涉研究:小尺度有机化学

An interferometric study of the low-mass protostar IRAS 16293-2422: small scale organic chemistry

S. E. Bisschop, J. K. Jorgensen, T. L. Bourke, S. Bottinelli, E. F. van Dishoeck

摘要:

目的:根据低质量年轻天体IRAS 16293-2422 A和B中复杂有机物的空间分布和激发条件,研究它们之间的化学关系。研究方法:用亚毫米波阵列进行了5“× 3”分辨率的干涉观测,揭示了HNCO,CH_3CN,CH_2CO,CH_3CHO和C_2 H_5 OH的发射线。当检测到足够数量的线时,从旋转图确定旋转温度。结果:紧凑的发射检测到所有物种在这里研究。对于HNCO和CH 3CN,其主要来自源A,CH 2CO和C2 H5 OH对于两种源具有相当的强度,并且CH 3CHO仅来自源B。HNCO、CH_3CN和CH_3CHO的旋转温度>200 K。(u,v)-能见度资料显示HNCO也有扩展冷辐射。结论:这里研究的分子丰度与高质量YSO中发现的分子丰度非常相似。因此,高质量和低质量天体之间的化学反应似乎与光度和云质量无关。在A源和B源之间可以看到更大的丰度差异。相对于CH 3OH的HNCO丰度朝向A高约4倍,这可能是由于与B相比,源A中的初始OCN-冰丰度更高。此外,并非所有含氧物质都是共存的。与CH 3CHO相比,CH 2CO和C2 H5 OH的不同空间行为表明,颗粒表面上的氢化反应不足以解释所观察到的气相丰度。CH 3CHO的选择性破坏可能导致源A中这些物质的反符合。这些结果说明了功率的干涉相比,单盘数据在测试化学模型。

英文摘要:

Aims: To investigate the chemical relations between complex organics based on their spatial distributions and excitation conditions in the low-mass young stellar objects IRAS 16293-2422 A and B. Methods: Interferometric observations with the Submillimeter Array have been performed at 5''x3'' resolution revealing emission lines of HNCO, CH3CN, CH2CO, CH3CHO and C2H5OH. Rotational temperatures are determined from rotational diagrams when a sufficient number of lines are detected. Results: Compact emission is detected for all species studied here. For HNCO and CH3CN it mostly arises from source A, CH2CO and C2H5OH have comparable strength for both sources and CH3CHO arises exclusively from source B. HNCO, CH3CN and CH3CHO have rotational temperatures >200 K. The (u,v)-visibility data reveal that HNCO also has extended cold emission. Conclusions: The abundances of the molecules studied here are very similar within factors of a few to those found in high-mass YSOs. Thus the chemistry between high- and low-mass objects appears to be independent of luminosity and cloud mass. Bigger abundance differences are seen between the A and B source. The HNCO abundance relative to CH3OH is ~4 times higher toward A, which may be due to a higher initial OCN- ice abundances in source A compared to B. Furthermore, not all oxygen-bearing species are co-existent. The different spatial behavior of CH2CO and C2H5OH compared with CH3CHO suggests that hydrogenation reactions on grain-surfaces are not sufficient to explain the observed gas phase abundances. Selective destruction of CH3CHO may result in the anti-coincidence of these species in source A. These results illustrate the power of interferometric compared with single dish data in terms of testing chemical models.

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