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arXiv 1506.04564astro-ph.EP
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AU Microscopii碎片盘的碰撞模拟

Collisional modelling of the AU Microscopii debris disc

Ch. Schüppler, T. Löhne, A. V. Krivov, S. Ertel, J. P. Marshall, S. Wolf, M. C. Wyatt, J. -C. Augereau, S. A. Metchev

摘要:

空间分辨的AU Mic碎片盘是最著名和研究最多的碎片盘之一。我们的目标是全面了解尘埃的生产和动态的光盘对象与深入的碰撞建模,包括恒星辐射和微粒力。我们的模型进行了比较,一套观测数据的热和散射光发射,范围从ALMA径向表面亮度分布在1.3毫米的偏振测量可见。大部分的数据都可以用一个外缘在40天文单位左右的微行星带和随后由恒星风向内输送的尘埃来重现。一个低的动力学激发的星子与偏心率高达0.03是优选的。星子带的径向宽度不能被严格限制。5au和17au宽的带,以及44au宽的带与观测结果一致。所有的模型都显示出表面密度分布随着与恒星距离的增加而增加,这是从观测中推断出来的。最好的模型是假设恒星的质量损失率超过太阳的50倍。虽然SED和ALMA轮廓的形状被很好地再现,但模型更强烈地偏离散射光数据。观测结果显示,在投影距离<40天文单位时,圆盘的颜色比模型预测的更蓝,偏振度也更低。这个问题可以通过不规则形状的尘埃颗粒来缓解,这些尘埃颗粒具有与所使用的米氏球不同的散射特性。从少数选定的粉尘材料的测试,我们得到的硅酸盐,碳和冰的中等孔隙度的混合物的偏好。我们解决的起源未解决的中央过量排放检测ALMA,并表明它不能单独从一个额外的内部带干。相反,它应该至少部分来自中央恒星的色球层。

英文摘要:

The spatially resolved AU Mic debris disc is among the most famous and best-studied debris discs. We aim at a comprehensive understanding of the dust production and the dynamics of the disc objects with in depth collisional modelling including stellar radiative and corpuscular forces. Our models are compared to a suite of observational data for thermal and scattered light emission, ranging from the ALMA radial surface brightness profile at 1.3mm to polarisation measurements in the visible. Most of the data can be reproduced with a planetesimal belt having an outer edge at around 40au and subsequent inward transport of dust by stellar winds. A low dynamical excitation of the planetesimals with eccentricities up to 0.03 is preferred. The radial width of the planetesimal belt cannot be constrained tightly. Belts that are 5au and 17au wide, as well as a broad 44au-wide belt are consistent with observations. All models show surface density profiles increasing with distance from the star as inferred from observations. The best model is achieved by assuming a stellar mass loss rate that exceeds the solar one by a factor of 50. While the SED and the shape of the ALMA profile are well reproduced, the models deviate from the scattered light data more strongly. The observations show a bluer disc colour and a lower degree of polarisation for projected distances <40au than predicted by the models. The problem may be mitigated by irregularly-shaped dust grains which have scattering properties different from the Mie spheres used. From tests with a handful of selected dust materials, we derive a preference for mixtures of silicate, carbon, and ice of moderate porosity. We address the origin of the unresolved central excess emission detected by ALMA and show that it cannot stem from an additional inner belt alone. Instead, it should derive, at least partly, from the chromosphere of the central star.

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