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JWST/NIRCam 散射光盘 GTO 2780 项目:HD 10647、HD 32297、HD 61005、HD 107146 和 HD 181327 碎片盘系统的全波段日冕仪成像

The JWST/NIRCam Scattered Light Disks GTO 2780 program: panchromatic coronagraphic imaging of the HD 10647, HD 32297, HD 61005, HD 107146, and HD 181327 debris disk systems

András Gáspár, Jarron M. Leisenring, Schuyler Grace Wolff, Kellen Lawson, George H. Rieke, Dingshan Deng, Marcia J. Rieke, Antranik A. Sefilian, Charles Beichman, Joshua B. Lovell, John Krist, Marie Ygouf, Jorge Llop-Sayson, Geoffrey Bryden, Christopher C. Stark, Christine H. Chen

arXiv 2608.27437首次发表:更新:

AI 中文总结

该研究利用 JWST/NIRCam 日冕仪观测五个明亮碎片盘系统,补充短波长数据,揭示水冰分布、散射特性及尘埃组成,还发现 MIRI 图像中心聚集度更高的现象。

AI 中文摘要

碎片盘由岩石、巨砾、星子及其碰撞产生的尘埃组成,是成熟行星系统中最易观测到的组成部分,也可作为有价值的诊断工具,用于研究行星动力学相互作用和矿物成分。从光学波段到射电波段观测,每个波段都能揭示尘埃群的独特信息,其中光学和近红外观测对微米级粒子表面散射的光特别敏感。本文呈现 JWST/NIRCam GTO 项目 2780 的成果,该项目计划使用 NIRCam 日冕仪,通过六个滤镜观测五个此前在光学波段被确认异常明亮的盘系统:HD 10647、HD 32297、HD 61005、HD 107146 和 HD 181327。NIRCam 数据补充了这些系统此前更短波长的图像,以高分辨率和信噪比揭示了盘及受辐射力作用的微小粒子延伸晕的散射光。所有系统均显示出水冰存在的证据,不过水冰的径向分布可能存在差异,且往往在晕中表现出更强的特征。在可分析的两个案例中,盘的散射相位函数类似太阳系尘埃的行为,且晕中存在前向散射增强的证据,与晕由微小粒子组成的结论一致。两个系统的 MIRI 图像比更短波长的图像更集中于中心,表明被拖拽的更大粒子发挥了作用。

英文摘要

Debris disks, composed of rocks, boulders, planetesimals, and the dust produced in their collisions, present the most readily observable components of mature planetary systems. They also serve as valuable diagnostic tools, enabling studies of planetary dynamical interactions and mineral compositions. Observed from optical to radio wavelengths, each band reveals unique information about the dust populations. Optical and near-infrared observations are specifically sensitive to light scattered off the surfaces of the micron-sized particles. Here, we present results from the JWST/NIRCam GTO program 2780, designed to observe five disk systems previously identified to be exceptionally bright at optical wavelengths (HD 10647, HD 32297, HD 61005, HD 107146, and HD 181327) with six filters using the NIRCam coronagraphs. The NIRCam data complement previous shorter-wavelength images of these same systems. They reveal scattered light from the disks and from the extended halos of tiny grains under the influence of radiative forces, at high resolution and signal to noise. All the systems show evidence for water ice, although it can have differing radial distributions and tends to show stronger signatures in the halos. In the two cases we could analyze, the scattering phase function in the disks resembles the behavior of dust in the Solar System with evidence for enhanced forward scattering in the halos, consistent with the latter being composed of tiny grains. MIRI images for two systems are more centrally concentrated than the shorter wavelength ones, suggesting a role for dragged-in larger grains.

Comments52 pages, 42 figures, accepted for publication in ApJ

DOI:10.3847/1538-4357/ae9d6f

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