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DUST IN A TYPE Ia SUPERNOVA PROGENITOR: SPITZER SPECTROSCOPY OF KEPLER'S SUPERNOVA REMNANT

机译:Ia型超新星祖先的粉尘:开普勒超新星遗骸的斯皮策光谱

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Characterization of the relatively poorly understood progenitor systems of Type Ia supernovae is of great importance in astrophysics, particularly given the important cosmological role that these supernovae play. Kepler's supernova remnant, the result of a Type Ia supernova, shows evidence for an interaction with a dense circumstellar medium (CSM), suggesting a single-degenerate progenitor system. We present 7.5-38 μm infrared (IR) spectra of the remnant, obtained with the Spitzer Space Telescope, dominated by emission from warm dust. Broad spectral features at 10 and 18 μm, consistent with various silicate particles, are seen throughout. These silicates were likely formed in the stellar outflow from the progenitor system during the asymptotic giant branch stage of evolution, and imply an oxygen-rich chemistry. In addition to silicate dust, a second component, possibly carbonaceous dust, is necessary to account for the short-wavelength Infrared Spectrograph and Infrared Array Camera data. This could imply a mixed chemistry in the atmosphere of the progenitor system. However, non-spherical metallic iron inclusions within silicate grains provide an alternative solution. Models of collisionally heated dust emission from fast shocks (1000?km?s–1) propagating into the CSM can reproduce the majority of the emission associated with non-radiative filaments, where dust temperatures are ~80-100?K, but fail to account for the highest temperatures detected, in excess of 150?K. We find that slower shocks (a few hundred?km?s–1) into moderate density material (n 0 ~ 50-250?cm–3) are the only viable source of heating for this hottest dust. We confirm the finding of an overall density gradient, with densities in the north being an order of magnitude greater than those in the south.
机译:Ia型超新星的相对较不了解的祖先系统的表征在天体物理学中非常重要,特别是考虑到这些超新星在宇宙学中的重要作用。开普勒的超新星残骸是Ia型超新星的结果,它显示了与密集的星际介质(CSM)相互作用的证据,这表明了单个退化的祖细胞系统。我们介绍了使用Spitzer空间望远镜获得的残留物的7.5-38μm红外(IR)光谱,其中主要是来自温暖尘埃的发射。整个过程中都可以看到与各种硅酸盐颗粒一致的10和18μm宽光谱特征。这些硅酸盐很可能是在演化的渐近大分支阶段从祖先系统的恒星流出物中形成的,这意味着富含氧的化学物质。除了硅酸盐粉尘外,还需要第二种成分(可能是碳粉尘)来说明短波红外光谱仪和红外阵列相机数据。这可能暗示了祖细胞大气中的化学混合。但是,硅酸盐晶粒内的非球形金属铁夹杂物提供了另一种解决方案。传播到CSM中的快速震动(> 1000?km?s–1)产生的碰撞加热粉尘排放模型可以再现与非辐射丝相关的大部分排放,粉尘温度约为80-100?K,但失败考虑到检测到的最高温度超过150?K。我们发现,对中等密度材料(n 0〜50-250?cm–3)的较慢的冲击(几百?km?s–1)是这种最热尘埃唯一可行的加热源。我们确认发现整体密度梯度,北部的密度比南部的密度大一个数量级。

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