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首页> 外文期刊>The Astrophysical journal >YOHKOH OBSERVATIONS OF Fe XXVI X-RAY LINE EMISSION FROM SOLAR FLARES
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YOHKOH OBSERVATIONS OF Fe XXVI X-RAY LINE EMISSION FROM SOLAR FLARES

机译:太阳耀斑中Fe XXVI X射线线的YOHKOH观测

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We report on observations from the Bragg Crystal Spectrometer (BCS) on board the Japanese solar flare spacecraft Yohkoh showing Fe XXVI Lyα X-ray line emission at 1.78 A. Some 75 events over a 2 yr period between 1991 December 6 and 1993 December 31 have been analyzed. The greater sensitivity of the BCS compared with previous instruments has enabled such emission to be detected from a wider group of flares than has previously been possible. The likelihood of detecting Fe XXVI lines in a flare is found to increase sharply with the electron temperature obtained from the Fe xxv line spectrum, also observed by the BCS, and with GOES X-ray class. The width of the Lyα_1 line, measured after the impulsive stage, is greater than that determined by thermal Doppler broadening, but this is explained by the nonzero spatial extent of flares. Electron temperatures from the intensity ratio of a nearby feature due to Fe xxv dielectronic satellites and the Fe XXVI Lyα_1 line are obtained from new atomic parameters from the superstructure code, details of which are described. This revises earlier calculations that have been extensively used. Comparison of these temperatures with those from the Fe xxv spectra provides evidence for a single loose grouping of flares, with the difference between the two temperatures ranging from nearly zero to about 20 MK. A "superhot" component would seem to be more or less developed according to whether the temperature difference is large or nearly zero. Flares at both extremes are examined in detail. The gradually varying part of the 14-33 keV X-ray emission for these events, as observed by the Hard X-ray Telescope on Yohkoh, has a hardness ratio corresponding to temperatures and emission measures similar to those from Fe XXVI line ratios, pointing to a common origin for their emission. Many of the flares studied occurred in particular active regions with great magnetic complexity, although Fe XXVI flares do not seem to be a distinct class within large X-ray flares.
机译:我们报告了来自日本太阳耀斑飞船Yohkoh上的布拉格晶体光谱仪(BCS)的观测结果,显示Fe XXVILyαX射线线的发射强度为1.78A。1991年12月6日至1993年12月31日的2年期间发生了约75起事件经过分析。与以前的仪器相比,BCS的灵敏度更高,从而可以从比以前更大的火炬组中检测到这种辐射。发现从火炬中检测到的Fe XXVI线的可能性随从Fe xxv线谱获得的电子温度急剧增加,这也由BCS观察到,并且具有GOES X射线类别。在脉冲阶段之后测量的Lyα_1线的宽度大于通过热多普勒展宽确定的宽度,但这可以通过耀斑的非零空间范围来解释。根据上层结构代码的新原子参数,获取了由Fe xxv双电子卫星和Fe XXVILyα_1线引起的附近特征强度比的电子温度。这修改了已被广泛使用的早期计算。将这些温度与Fe xxv光谱中的温度进行比较,为火炬的单个松散分组提供了证据,两个温度之间的差异范围从几乎零到大约20 MK。根据温度差是大还是接近于零,“过热”成分似乎或多或少地发展了。详细研究了两种极端情况下的耀斑。用Yohkoh上的Hard X射线望远镜观察到的这些事件在14-33 keV X射线发射中逐渐变化的部分,其硬度比对应于温度和发射量,类似于Fe XXVI线比。排放到一个共同的起源。尽管在大型X射线耀斑中似乎没有Fe XXVI耀斑,但许多研究出的耀斑都发生在特定的活动区域,且磁场复杂度很高。

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