论文标题

用Orbyts量化SN 2012AW和IPTF14HL的灰尘

Quantifying the dust in SN 2012aw and iPTF14hls with ORBYTS

论文作者

Niculescu-Duvaz, Maria, Barlow, M. J., Dunn, W., Bevan, A., Ahmed, Omar, Arkless, David, Barker, Jon, Bartolotta, Sidney, Brockway, Liam, Browne, Daniel, Esmail, Ubaid, Garner, Max, Guz, Wiktoria, King, Scarlett, Kose, Hayri, Lampstaes-Capes, Madeline, Magen, Joseph, Morrison, Nicole, Oo, Kyaw, Paik, Balvinder, Primrose, Joanne, Quick, Danny, Radeka, Anais, Rodney, Anthony, Sandeman, Eleanor, Sheikh, Fawad, Stansfield, Camron, Symister, Delayne, Taylor, Joshua, Wilshere, William, Wesson, R., De Looze, I., Clayton, G. C., Krafton, K., Matsuura, M.

论文摘要

核心溢出的超新星(CCSNE)可能能够产生大量的灰尘,有强有力的证据表明,射水量可以在长时间内显着生长。 CCSNE的宽发射线中的红蓝色不对称可以使用蒙特卡洛辐射转移代码damocles建模,以确定喷射尘埃质量。为了促进更轻松地使用Damocles,我们提出了运行Damocles的TKINTER图形用户界面(GUI)。高中生对GUI进行了测试,这是年轻的Twinkle学生(Orbyts)计划的原始研究的一部分,他们用它测量了两种IIP CCSNE:SN 2012AW和IPTF14HL的两个时代形成的尘埃质量,表明许多人可以为科学进步做出重大贡献。贝叶斯方法用于量化我们模型参数的不确定性。从1863 H $α$ profile of SN 2012AW的当天存在红色散射翼,我们能够将灰尘成分限制为大的(半径$>0.1μ$ M)硅酸盐晶粒,灰尘质量为$ 6.0^{+21.9} _ { - 3.6} _ { - 3.6}} \ times10^\ times10^{-4} m_ \ odot $。从SN 2012AW的第1158 h $α$ profile从一天开始,我们发现灰尘质量为$ 3.0^{+14} _ { - 2.5} \ times10^{ - 4} $ m $ _ \ odot $。对于IPTF14HL,我们发现了一天的1170尘埃质量为8.1 $^{+81} _ { - 7.6} \ times10^{ - 5} $ M $ _ {\ odot} $,用于由50%无律碳和50%天文学硅酸盐组成的粉尘组成。爆炸后1000天,SN 2012AW和IPTF14HL的灰尘比SN 1987a少,这表明SN 1987a可能比其他类型IIP形成更大的灰尘块。

Core-collapse supernovae (CCSNe) are potentially capable of producing large quantities of dust, with strong evidence that ejecta dust masses can grow significantly over extended periods of time. Red-blue asymmetries in the broad emission lines of CCSNe can be modelled using the Monte Carlo radiative transfer code DAMOCLES, to determine ejecta dust masses. To facilitate easier use of DAMOCLES, we present a Tkinter graphical user interface (GUI) running DAMOCLES. The GUI was tested by high school students as part of the Original Research By Young Twinkle Students (ORBYTS) programme, who used it to measure the dust masses formed at two epochs in two Type IIP CCSNe: SN 2012aw and iPTF14hls, demonstrating that a wide range of people can contribute significantly to scientific advancement. Bayesian methods were used to quantify uncertainties on our model parameters. From the presence of a red scattering wing in the day 1863 H$α$ profile of SN 2012aw, we were able to constrain the dust composition to large (radius $>0.1 μ$m) silicate grains, with a dust mass of $6.0^{+21.9}_{-3.6}\times10^{-4} M_\odot$. From the day 1158 H$α$ profile of SN 2012aw, we found a dust mass of $3.0^{+14}_{-2.5}\times10^{-4}$ M$_\odot$. For iPTF14hls, we found a day 1170 dust mass of 8.1 $^{+81}_{-7.6}\times10^{-5}$ M$_{\odot}$ for a dust composition consisting of 50% amorphous carbon and 50% astronomical silicate. At 1000 days post explosion, SN 2012aw and iPTF14hls have formed less dust than SN 1987A, suggesting that SN 1987A could form larger dust masses than other Type IIP's.

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