论文标题

部分可观测时空混沌系统的无模型预测

Grain Growth in the Dust Ring with Crescent around Very Low Mass Star ZZ Tau IRS with JVLA

论文作者

Hashimoto, Jun, Liu, Hauyu Baobab, Dong, Ruobing, Liu, Beibei, Muto, Takayuki

论文摘要

在原星磁盘(例如年轻恒星周围的新月形)中,尘埃环的方位角不对称通常被解释为尘埃陷阱,因此是地球和行星形成的理想位置。这种尘埃陷阱是否有效地促进了非常低的质量恒星周围磁盘中的行星形成(VLM; $ \ lyssim $ 0.2〜 $ M_ \ odot $)是值得商式的,因为此类系统中的动态增长时间范围很长。为了研究这种系统中的谷物生长,我们使用Karl G. Jansky在VLM Star Zz〜tau〜irs周围使用了新月形的粉尘环,以厘米波长非常大的阵列(JVLA)。围绕Zz〜tau〜IRS检测到明显的信号。为了估计新月中的最大晶粒尺寸($ a _ {\ rm max} $),我们将观察到的光谱能分布(SED)与辐射传输计算预测的各种$ a _ {\ rm max} $值的SED进行了比较。我们发现$ a _ {\ rm max} \ gtrsim $ 〜1〜mm和$ \ sillsim $ 〜60〜 $μ$ m分别在新月和环上,尽管我们的建模工作依赖于不确定的灰尘特性。我们的结果表明,相对于亚微米大小的星际培养基,在Zz〜tau〜IRS磁盘中发生了晶粒的生长。带有MM大小卵石的新月形的行星形成可能比通过卵石积聚方案在具有亚毫米大小的卵石的其他区域进行效率更高。

The azimuthal asymmetries of dust rings in protoplanetary disks such as a crescent around young stars are often interpreted as dust traps, and thus as ideal locations for planetesimal and planet formations. Whether such dust traps effectively promote planetesimal formation in disks around very-low-mass stars (VLM; a mass of $\lesssim$0.2~$M_\odot$) is debatable, as the dynamical and grain growth timescales in such systems are long. To investigate grain growth in such systems, we studied the dust ring with crescent around the VLM star ZZ~Tau~IRS using the Karl G. Jansky Very Large Array (JVLA) at centimeter wavelengths. Significant signals were detected around ZZ~Tau~IRS. To estimate the maximum grain size ($a_{\rm max}$) in the crescent, we compared the observed spectral energy distribution (SED) with SEDs for various $a_{\rm max}$ values predicted by radiative transfer calculations. We found $a_{\rm max} \gtrsim$~1~mm and $\lesssim$~60~$μ$m in the crescent and ring, respectively, though our modeling efforts rely on uncertain dust properties. Our results suggest that grain growth occurred in the ZZ~Tau~IRS disk, relative to sub-micron-sized interstellar medium. Planet formation in crescent with mm-sized pebbles might proceed more efficiently than in other regions with sub-millimeter-sized pebbles via pebble accretion scenarios.

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