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arXiv 2103.06645astro-ph.GA
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四种低质量分子外流源的碳链分子测量

Carbon-chain molecule survey toward four low-mass molecular outflow sources

C. Zhang, Y. Wu, X. -C. Liu, Mengyao Tang, Di Li, Jarken Esimbek, S. -L. Qin

摘要:

利用紫金山天文台13.7 m射电望远镜和上海天文台65 m天马射电望远镜对IRAS 04181+2655(I 04181)、HH 211、L1524和L1598四个低质量外流源进行了碳链分子(CCM)观测。我们观察到下列烃类(C $_2$ H、C $_4$ H、c--C $_3$ H $_2$)、HC $_{\rm 2n+1}$ N(n= 1、2)、C $_{\rm n}$ S(n= 2、3)和SO、HNC、N $_2$ H $^+$。除L1598外,在所有来源中都检测到碳氢化合物和HC $_3$ N,L1598边缘检测到C $_4$ H,未检测到HC $_3$ N(J=2--1)。HC $_5$ N和CCCS仅在I 04181和L1524中检出,而SO仅在HH 211中检出。L1598的CCM检出率最低,一般认为缺乏CCM来源。在低质量恒星形成核心中,N的比值(HC $_3$ N/N(N $_2$ H $^+$))随着演化而增加。I 04181和L1524是富含碳链的恒星形成核心,可能具有温暖的碳链化学特征。在I 04181和L1524中,丰富的CCCS可以通过冲击碳链化学来解释。在HH 211中,大量的SO表明SO是由升华的S $^+$形成的。在这项研究中,我们还绘制了HNC,C $_4$ H,c-C $_3$ H $_2$和HC $_3$ N与PMO的数据。我们还发现HNC和NH $_3$分别集中在L1524 S和L1524 N中。此外,我们讨论了I 04181 SE和I 04181 W之间的化学差异。在I 04181 SE中可以看到线性烃和氰基多炔之间的共同进化。

英文摘要:

We performed a carbon-chain molecule (CCM) survey toward four low-mass outflow sources, IRAS 04181+2655 (I04181), HH211, L1524, and L1598, using the 13.7 m telescope at the Purple Mountain Observatory (PMO) and the 65 m Tian Ma Radio telescope at the Shanghai Observatory. We observed the following hydrocarbons (C$_2$H, C$_4$H, c--C$_3$H$_2$), HC$_{\rm 2n+1}$N (n=1,2), C$_{\rm n}$S (n=2,3), and SO, HNC, N$_2$H$^+$. Hydrocarbons and HC$_3$N were detected in all the sources, except for L1598, which had a marginal detection of C$_4$H and a non-detection of HC$_3$N (J=2--1). HC$_5$N and CCCS were only detected in I04181 and L1524, whereas SO was only detected in HH211. L1598 exhibits the lowest detection rate of CCMs and is generally regarded to be lacking in CCMs source. The ratio of N(HC$_3$N/N(N$_2$H$^+$)) increases with evolution in low-mass star-forming cores. I04181 and L1524 are carbon-chain-rich star-forming cores that may possibly be characterized by warm carbon-chain chemistry. In I04181 and L1524, the abundant CCCS can be explained by shocked carbon-chain chemistry. In HH211, the abundant SO suggests that SO is formed by sublimated S$^+$. In this study, we also mapped HNC, C$_4$H, c--C$_3$H$_2$, and HC$_3$N with data from the PMO. We also find that HNC and NH$_3$ is concentrated in L1524S and L1524N, respectively. Furthermore, we discuss the chemical differences between I04181SE and I04181W. The co-evolution between linear hydrocarbon and cyanopolyynes can be seen in I04181SE.

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