论文标题
中年IA Supernova Remnant G344.7-0.1中的元素分层
Element Stratification in the Middle-Aged Type Ia Supernova Remnant G344.7-0.1
论文作者
论文摘要
尽管它们的重要性,但对IA型超新星(SNE IA)的详细理解仍然难以捉摸。超新星残留物(SNR)中元素分布的X射线测量为理解SNE IA的爆炸和核合成机制提供了重要的线索。但是,要观察年轻SNR的X射线射击中的整个弹出质量,这是一项挑战,因为中央喷射可能还没有被反向冲击加热。在这里,我们介绍了IA SNR G344.7-0.1型的200多公斤Chandra观察结果,其年龄足够大,足以使SNR中心达到SNR中心,提供了一个机会来调查整个喷射质量的分布。我们揭示了重型元件的明确分层,其中央弹出物的中央峰分布被中等质量元素(IMES:SI,S,AR CA)包围,具有弧形的结构。 Fe K发射的质心能量在富含铁的中部地区比富含IME的区域略低,这表明最近对Fe弹出的冲击热了。这些结果与标准SN IA模型的预测一致,在爆炸的白矮人的内部合成了较重的元素。但是,我们发现,相对于SNR的几何中心,Fe K发射的峰位置略有偏移到西方。这种明显的不对称可能是由于环境介质的不均匀密度分布,这与我们对环境分子和中性气体的无线电观察一致。
Despite their importance, a detailed understanding of Type Ia supernovae (SNe Ia) remains elusive. X-ray measurements of the element distributions in supernova remnants (SNRs) offer important clues for understanding the explosion and nucleosynthesis mechanisms for SNe Ia. However, it is challenging to observe the entire ejecta mass in X-rays for young SNRs, because the central ejecta may not have been heated by the reverse shock yet. Here we present over 200 kilosecond Chandra observations of the Type Ia SNR G344.7-0.1, whose age is old enough for the reverse shock to have reached the SNR center, providing an opportunity to investigate the distribution of the entire ejecta mass. We reveal a clear stratification of heavy elements with a centrally peaked distribution of the Fe ejecta surrounded by intermediate-mass elements (IMEs: Si, S, Ar Ca) with an arc-like structure. The centroid energy of the Fe K emission is marginally lower in the central Fe-rich region than in the outer IME-rich regions, suggesting that the Fe ejecta were shock-heated more recently. These results are consistent with the prediction for standard SN Ia models, where the heavier elements are synthesized in the interior of an exploding white dwarf. We find, however, that the peak location of the Fe K emission is slightly offset to the west with respect to the geometric center of the SNR. This apparent asymmetry is likely due to the inhomogeneous density distribution of the ambient medium, consistent with our radio observations of the ambient molecular and neutral gas.