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arXiv 1902.01675astro-ph.GA
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仙后座A超新星遗迹中尘埃的质量、位置和加热

The mass, location and heating of the dust in the Cassiopeia A supernova remnant

F. D. Priestley, M. J. Barlow, I. De Looze

摘要:

我们的热尘埃排放模型加热的尘埃颗粒由同步辐射和粒子碰撞,在适当的条件下,四个不同的冲击和未冲击的气体成分的仙后座A(Cas A)超新星遗迹(SNR)。通过拟合得到的光谱能量分布(SED)所观察到的SNR尘埃通量,我们确定所需的尘埃质量在每个组件。我们发现,所观察到的SED可以再现$\sim 0.6 \, {\rm M_\odot}$的硅酸盐颗粒,其中大部分是在未经冲击的喷出物和加热的同步辐射领域。位于X射线发射反向冲击波和爆炸波区域的较温暖的尘埃有助于较短波长的红外发射,但只占总尘埃质量的一小部分。碳粒最多可以构成总尘埃质量的$\sim 25 \%$。结合气体质量的估计,我们得到的灰尘,气体质量比为每个组件,这表明在喷出物的冷凝效率高,和冲击喷出物团块中的灰尘是很好的保护,从破坏溅射在反向冲击。

英文摘要:

We model the thermal dust emission from dust grains heated by synchrotron radiation and by particle collisions, under conditions appropriate for four different shocked and unshocked gas components of the Cassiopeia A (Cas A) supernova remnant (SNR). By fitting the resulting spectral energy distributions (SEDs) to the observed SNR dust fluxes, we determine the required mass of dust in each component. We find the observed SED can be reproduced by $\sim 0.6 \, {\rm M_\odot}$ of silicate grains, the majority of which is in the unshocked ejecta and heated by the synchrotron radiation field. Warmer dust, located in the X-ray emitting reverse shock and blastwave regions, contribute to the shorter wavelength infrared emission but make only a small fraction of the total dust mass. Carbon grains can at most make up $\sim 25 \%$ of the total dust mass. Combined with estimates for the gas masses, we obtain dust-to-gas mass ratios for each component, which suggest that the condensation efficiency in the ejecta is high, and that dust in the shocked ejecta clumps is well protected from destruction by sputtering in the reverse shock.

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