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

Katsuda, Satoru, Ohno, Masanori, Mori, Koji, Beppu, Tatsuhiko, Kanemaru, Yoshiaki, Tashiro, Makoto S., Terada, Yukikatsu, Sato, Kosuke, Morita, Kae, Sagara, Hikari, Ogawa, Futa, Takahashi, Haruya, Murakami, Hiroshi, Nobukawa, Masayoshi, Tsunemi, Hiroshi, Hayashida, Kiyoshi, Matsumoto, Hironori, Noda, Hirofumi, Nakajima, Hiroshi, Ezoe, Yuichiro, Tsuboi, Yohko, Maeda, Yoshitomo, Yokoyama, Takaaki, Narukage, Noriyuki

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.

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