通过散射诱导极化探测 IRS 48 系统中带有适度尘埃落定的湍流涡旋

Haifeng 海峰 Yang 杨, M. Fern'andez-L'opez, Zhi-Yun Li, I. Stephens, L. Looney, Zheyu Lin, Rachel E. Harrison
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摘要

我们利用 ALMA 波段 7(870 μm)的高分辨(亚)毫米偏振观测,研究了过渡盘 Oph IRS 48 中的新月形尘埃陷阱。尘埃偏振图显示了与尘埃散射引起的偏振相一致的模式。偏振通量与总通量之间存在相对位移,这是了解该系统中尘埃尺度高度的关键。我们建立了偏振观测模型,重点关注尘埃尺度高度的影响。我们发现,倾角引起的偏振和新月中辐射各向异性引起的偏振之间的相互作用决定了观测到的偏振;各向异性由沿中平面的尘埃光学深度控制,而尘埃光学深度又由垂直方向上的尘埃尺度高度决定。我们发现,尘粒既不可能完全沉降,也不可能与气体充分混合。在完全沉降的情况下,总通量和偏振通量之间的径向位移很小,而在充分混合的情况下,新月的外部(径向)边缘会产生一种方位角模式,而这种模式是观测不到的。我们的最佳模型的气体-尘埃尺度高度比为 2,可以再现总通量和偏振通量之间的径向位移和方位位移。我们推断有效湍流 α 参数约为 0.0001-0.005。由散射引起的偏振现象使我们得以深入了解 IRS 48 系统中尘埃沉降程度适中的湍流漩涡,这在其他情况下是很难实现的。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Turbulent Vortex with Moderate Dust Settling Probed by Scattering-induced Polarization in the IRS 48 System
We investigate the crescent-shaped dust trap in the transition disk Oph IRS 48 using well-resolved (sub)millimeter polarimetric observations at ALMA Band 7 (870 μm). The dust polarization map reveals patterns consistent with dust-scattering-induced polarization. There is a relative displacement between the polarized flux and the total flux, which holds the key to understanding the dust scale heights in this system. We model the polarization observations, focusing on the effects of dust scale heights. We find that the interplay between the inclination-induced polarization and the polarization arising from radiation anisotropy in the crescent determines the observed polarization; the anisotropy is controlled by the dust optical depth along the midplane, which is, in turn, determined by the dust scale height in the vertical direction. We find that the dust grains can be neither completely settled nor well mixed with the gas. The completely settled case produces little radial displacement between the total and polarized flux, while the well-mixed case produces an azimuthal pattern in the outer (radial) edge of the crescent that is not observed. Our best model has a gas-to-dust scale height ratio of 2 and can reproduce both the radial displacement and the azimuthal displacement between the total and polarized flux. We infer an effective turbulence α parameter of approximately 0.0001–0.005. The scattering-induced polarization provides insight into a turbulent vortex with a moderate level of dust settling in the IRS 48 system, which is hard to achieve otherwise.
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