利用 SMT 进行的亚利桑那州分子 ISM 勘测:整个星系中 CO(2-1)/CO(1-0) 线比的变化

Ryan P. Keenan, Daniel P. Marrone, Garrett K. Keating
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引用次数: 0

摘要

一氧化碳(CO(1-0))的 J=1$\rightarrow$0 光谱线是分子气体的典型示踪线。不过,CO(2-1)经常被用来代替它,因为假设高能量线可以用来推断 CO(1-0) 光度和分子气体质量。CO(2-1)的使用取决于对CO(2-1)和CO(1-0)光度之比r21的了解。在这里,我们给出了122个星系的r21综合测量值,这些星系的恒星质量从10$^9$到10$^{11.5}$ M$_\odot$,恒星形成率(SFRs)从0.08到35 M$_\odot$/年。我们发现r21与恒星形成率、恒星形成率表面密度、恒星形成效率以及与恒星形成主序(SFMS)的距离之间存在很强的趋势。我们证明了恒定r21的假设会给星系种群研究中的分子气体趋势带来偏差,并演示了这是如何影响重要星系比例关系的恢复的,包括肯尼卡特-施密特定律以及SFMS偏移和恒星形成效率之间的关系。我们提供了一个处方,它考虑到了r21作为SFR函数的变化,当只有一条线可用时,可以用来在CO(2-1)和CO(1-0)之间进行转换。我们的处方与AMISS和文献样本的r21变化相匹配,可用于从CO(2-1)观测中得出更精确的气体质量。
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The Arizona Molecular ISM Survey with the SMT: Variations in the CO(2-1)/CO(1-0) Line Ratio Across the Galaxy Population
The J=1$\rightarrow$0 spectral line of carbon monoxide (CO(1-0)) is the canonical tracer of molecular gas. However, CO(2-1) is frequently used in its place, following the assumption that the higher energy line can be used to infer the CO(1-0) luminosity and molecular gas mass. The use of CO(2-1) depends on a knowledge of the ratio between CO(2-1) and CO(1-0) luminosities, r21. Here we present galaxy-integrated r21 measurements for 122 galaxies spanning stellar masses from 10$^9$ to 10$^{11.5}$ M$_\odot$ and star formation rates (SFRs) from 0.08 to 35 M$_\odot$/yr. We find strong trends between r21 and SFR, SFR surface density, star formation efficiency, and distance from the star formation main sequence (SFMS). We show that the assumption of a constant r21 can introduce biases into the molecular gas trends in galaxy population studies and demonstrate how this affects the recovery of important galaxy scaling relations, including the Kennicutt-Schmidt law and the relation between SFMS offset and star formation efficiency. We provide a prescription which accounts for variations in r21 as a function of SFR and can be used to convert between CO(2-1) and CO(1-0) when only one line is available. Our prescription matches variations in r21 for both AMISS and literature samples and can be used to derive more accurate gas masses from CO(2-1) observations.
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