论文标题
从地球X射线反照棒上发现的巨型太阳耀斑的反向FIP效应
Inverse FIP Effects in Giant Solar Flares Found from Earth X-Ray Albedo with Suzaku/XIS
论文作者
论文摘要
我们报告了2005年9月7日(x17.0),2005年9月8日(x5.4),2005年9月9日(x6.2)和2006年12月5日(x9.0),于2005年7月7日(x17.0)发生X射线光谱结果,该结果是从X射线成像仪(XIS)上获得的。 XIS的良好能量分辨率(FWHM $ \ sim $ 100 eV)使我们能够分离许多类似线的功能并检测基础连续性发射。这些功能包括Si he $α$,si $α$,s $α$,s ly $α$,ar he $α$和ca He $α$源自太阳耀斑以及荧光AR k $α$和AR K $β$。在四个耀斑上平均的绝对元素丰度(x/h)为$ \ sim $ 2.0(CA),$ \ sim $ 0.7(si),$ \ sim $ 0.3(s)和$ \ sim $ 0.9(ar),$ 0.9(ar)在Flare Peaks附近。这种丰度模式类似于活性恒星的冠状动脉的冠状电势(i-FIP)效应,即,元素丰度随着FIP的降低而随着FIP低端的周转而降低。在耀斑期间,丰度几乎是恒定的,除了SI外,衰减阶段的$ \ sim 2 $ 2。 Si丰度的演变与I-FIP等离子体起源于色层蒸发的图片一致,然后与周围的低脂偏置材料混合。耀斑的丰度因2倍而异,与过去对太阳耀斑的观察一致。最后,我们强调的是,X射线天文学卫星(如Suzaku和Xrism)获得的地球反照率数据可以显着有助于对太阳能物理学的研究。
We report X-ray spectroscopic results for four giant solar flares occurred on 2005 September 7 (X17.0), 2005 September 8 (X5.4), 2005 September 9 (X6.2), and 2006 December 5 (X9.0), obtained from Earth albedo data with the X-ray imaging spectrometer (XIS) onboard Suzaku. The good energy resolution of the XIS (FWHM$\sim$100 eV) enables us to separate a number of line-like features and detect the underlying continuum emission. These features include Si He$α$, Si Ly$α$, S He$α$, S Ly$α$, Ar He$α$, and Ca He$α$ originating from solar flares as well as fluorescent Ar K$α$ and Ar K$β$ from the Earth atmosphere. Absolute elemental abundances (X/H) averaged over the four flares are obtained to be $\sim$2.0 (Ca), $\sim$0.7 (Si), $\sim$0.3 (S), and $\sim$0.9 (Ar) at around flare peaks. This abundance pattern is similar to those of active stars' coronae showing inverse first ionization potential (i-FIP) effects, i.e., elemental abundances decrease with decreasing FIP with a turnover at the low end of FIP. The abundances are almost constant during the flares, with an exception of Si which increases by a factor of $\sim$2 in the decay phase. The evolution of the Si abundance is consistent with a picture that the i-FIP plasma originates from the chromosphere evaporation and then mixes with the surrounding low-FIP biased materials. Flare-to-flare abundance varied by a factor of 2, agreeing with past observations of solar flares. Finally, we emphasize that Earth albedo data acquired by X-ray astronomy satellites like Suzaku and XRISM can significantly contribute to studies of solar physics.