论文标题
2006年爆发后,RS Ophiuchi的硅酸盐灰尘的上升和下降
Rise and fall of silicate dust in RS Ophiuchi following the 2006 eruption
论文作者
论文摘要
我们介绍了对档案中的档案烈性光谱仪(IRS)观察的分析,对2006年爆发后大约7个月开始,几次获得的复发性nova rs ophiuchi。这些数据显示原子发射线,吸收频段,由于光谱SIO和众所周知的Silicate Silicate Dust,以及$ 9.7.7.7.7 $ $ 18.7.7 $ 18.7.7 $ 18.7.7 $ 18.7.7.7 $ 18.7.7.7 $ MON。在次级恒星的风中产生的灰尘发射是由尘土模型拟合的,以减少范围$ 1.0-1.7 \ times10^{ - 7} $ M $ _ {\ odot} $ yr $^{ - 1} $。硅酸盐特征的轮廓与在孤立的晚期恒星和一些尘土飞扬的共生二进制环境中所看到的特征相似,尽管较长的波长特征在$ 17 \,μ$ m,,而不是通常的$ 18 \,μ$ m,表示特殊的谷物特性。灰尘特征是可变的,在爆发期间,在2008年至2009年的爆发期间,该系统处于静态状态时。这种差异归因于紫外产量的变化和积聚磁盘的改革,尽管红色巨人次要恒星的质量损失率下降也可能发挥作用。在2021年爆发后,进一步的观察可以得出明确的结论。
We present an analysis of archival Spitzer InfraRed Spectrograph (IRS) observations of the recurrent nova RS Ophiuchi obtained on several occasions, beginning about 7 months after the outburst in 2006. These data show atomic emission lines, absorption bands due to photospheric SiO, and the well known silicate dust features at $9.7\,μ$m and $18\,μ$m. The dust emission, arising in the wind of the secondary star, is fitted by Dusty models for mass-loss rates in the range $1.0-1.7\times10^{-7}$M$_{\odot}$yr$^{-1}$. The silicate features are similar in profile to those seen in circumstellar environments of isolated late-type stars and some dusty symbiotic binaries, although the longer wavelength feature peaks at $17\,μ$m,, instead of the usual $18\,μ$m, indicating peculiar grain properties. The dust features are variable, appearing stronger in 2006-2007 during outburst than in 2008-2009 when the system was in the quiescent state. This variability is attributed to changes in the ultraviolet output and the reformation of the accretion disk, although a decline in the mass-loss rate of the red giant secondary star could also play a role. Further observations, in the aftermath of the 2021 eruption, could provide a definitive conclusion.