arXivDaily arXiv每日学术速递 周一至周五更新
arXiv 0909.3280astro-ph.GAastro-ph.EP
收藏

远红外原行星气体盘

Protoplanetary gas disks in the far infrared

Javier R. Goicoechea, Bruce Swinyard

摘要:

年轻原行星盘的物理和化学条件为行星形成设定了边界条件。虽然尘埃盘中的尘埃相对容易被检测为远红外光度“过量”超过预期的光球发射,但对气相的了解要少得多。似乎很清楚,从大质量光学厚盘(富含气体的结构,其中只有约1%的总质量以尘埃的形式存在)到几乎没有气体的纤细碎片盘的突然转变发生在约10^7年,到那时,至少大部分巨行星必须形成。事实上,这些行星大部分是气态的,因此它们必须在气盘消散之前聚集起来。因此,在不同的演化阶段的盘气体含量的光谱研究是至关重要的。来自丰富气藏的远红外水蒸气线和原子精细结构线(例如,[OI] 63 μ m、[SI] 56 μ m、[SiIII] 34 μ m)是圆盘中气体的稳健示踪剂。赫歇尔上的光谱仪将探测到其中一些朝向最近的、最年轻的和更大质量的原行星盘的线。然而,根据模型,赫歇尔将无法达到所需的灵敏度,以(1)检测在更演化和更脆弱的transamational磁盘中的气体残留,这些磁盘可能形成行星,(2)检测银河系中最多恒星(M型和较冷的矮星)周围质量较小的原行星盘的气体排放。两者都是SPICA/SAFARI的独特目标。此外,SAFARI将能够探测到~44和~ 62 μ m的水冰远红外模式,从而允许在许多原行星系统中观察水冰,并充分探索其对行星形成和演化的影响。

英文摘要:

The physical and chemical conditions in young protoplanetary disks set the boundary conditions for planet formation. Although the dust in disks is relatively easily detected as a far-IR photometric ``excess'' over the expected photospheric emission, much less is known about the gas phase. It seems clear that an abrupt transition from massive optically thick disks (gas-rich structures where only ~1% of the total mass is in the form of dust) to tenuous debris disks almost devoid of gas occurs at ~10^7 years, by which time the majority of at least the giant planets must have formed. Indeed, these planets are largely gaseous and thus they must assemble before the gas disk dissipates. Spectroscopic studies of the disk gas content at different evolutive stages are thus critical. Far-IR water vapor lines and atomic fine structure lines from abundant gas reservoirs (e.g., [OI]63um, [SI]56um, [SiII]34um) are robust tracers of the gas in disks. Spectrometers on board Herschel will detect some of these lines toward the closest, youngest and more massive protoplanetary disks. However, according to models, Herschel will not reach the required sensitivity to (1) detect the gas residual in more evolved and tenuous transational disks that are potentially forming planets and (2) detect the gas emission from less massive protoplanetary disks around the most numerous stars in the Galaxy (M-type and cooler dwarfs). Both are unique goals for SPICA/SAFARI. Besides, SAFARI will be able to detect the far-IR modes of water ice at ~44 and ~62um, and thus allow water ice to be observed in many protoplanetary systems and fully explore its impact on planetary formation and evolution.

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。

↑