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首页> 外文期刊>The Astrophysical journal >Early Formation Of Dust In The Ejecta Of Type Ib Sn 2006jc And Temperature And Mass Of The Dust
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Early Formation Of Dust In The Ejecta Of Type Ib Sn 2006jc And Temperature And Mass Of The Dust

机译:Ib Sn 2006jc型弹射器中粉尘的早期形成以及粉尘的温度和质量

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摘要

SN 2006jc is a peculiar supernova (SN), in which the formation of dust has been confirmed at an early epoch of ~50 days after the explosion. We investigate the possibility of such an early formation of dust grains in the expanding ejecta of SN 2006jc, applying the Type Ib SN model that is developed to reproduce the observed light curve. We find that the rapid decrease of the gas temperature in SN 2006jc enables the condensation of C grains in the C-rich layer at 40-60 days after the explosion, which is followed by the condensation of silicate and oxide grains until ~200 days. The average radius of each grain species is confined to be less than 0.01 μm due to the low gas density at the condensation time. The calculated total dust mass reaches approx=1.5 M_☉, of which C dust shares 0.7 M_☉. On the other hand, based on the calculated dust temperature, we show that the dust species and mass evaluated to reproduce the spectral energy distribution observed by AKARI and MAGNUM at day 200 are different from those obtained by the dust formation calculations; the dust species contributing to the observed flux are hot C and FeS grains with masses of 5.6 × 10~4 and 2.0 × 10~(-3) M_☉, respectively, although we cannot defy the presence of a large amount of cold dust such as silicate and oxide grains up to 0.5 M_☉. One of the physical processes responsible for the difference between calculated and evaluated masses of C and FeS grains could be considered to be the destruction of small-sized clusters by energetic photons and electrons prevailing within the ejecta at the earlier epoch.
机译:SN 2006jc是奇特的超新星(SN),在爆炸后约50天的早期就确认了尘埃的形成。我们使用发展为重现观察到的光曲线的Ib型SN模型,研究了SN 2006jc扩张喷口中尘埃颗粒如此早期形成的可能性。我们发现,SN 2006jc中气体温度的快速下降使爆炸后40-60天的C富碳层中的C晶粒凝结,随后硅酸盐和氧化物晶粒的凝结直到约200天。由于凝结时的气体密度低,每个晶粒的平均半径被限制为小于0.01μm。计算出的总粉尘质量达到约= 1.5M_☉,其中C灰尘共享0.7M_☉。另一方面,根据计算得出的粉尘温度,我们表明,为重现AKARI和MAGNUM在200天时观察到的光谱能量分布而评估的粉尘种类和质量与通过粉尘形成计算获得的粉尘种类和质量有所不同。尽管我们不能抗拒大量冷尘的存在,但有助于观测通量的粉尘种类分别是质量为5.6×10〜4和2.0×10〜(-3)M_☉的热C和FeS晶粒。高达0.5M_☉的硅酸盐和氧化物颗粒。造成C和FeS晶粒质量与估算质量之间差异的物理过程之一,可以被认为是较早时期喷出的高能光子和电子破坏了小型团簇。

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