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首页> 外文期刊>The Astrophysical journal >THE TRANSPARENCY OF SOLAR CORONAL ACTIVE REGIONS
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THE TRANSPARENCY OF SOLAR CORONAL ACTIVE REGIONS

机译:太阳冠状活动区的透明度

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摘要

Resonance scattering has often been invoked to explain the disagreement between the observed and predicted line ratios of Fe XVII λ15.01 to Fe XVII λ15.26 (the "3C/3D" ratio). In this process photons of λ15.01, with its much higher oscillator strength, are preferentially scattered out of the line of sight, thus reducing the observed line ratio. Recent laboratory measurements, however, have found significant inner-shell Fe XVI lines at 15.21 and 15.26 A, suggesting that the observed 3C/3D ratio results from blending. Given our new understanding of the fundamental spectroscopy, we have reexamined the original solar spectra, identifying the Fe XVI λ15.21 line and measuring its flux to account for the contribution of Fe XVI to the λ15.26 flux. Deblending brings the 3C/3D ratio into good agreement with the experimental ratio; hence, we find no need to invoke resonance scattering. Low opacity in Fe XVII λ15.01 also implies low opacity for Fe XV λ284.2, ruling out resonance scattering as the cause of the fuzziness of TRACE and SOHO-EIT 284 A images. The images must, instead, be unresolved due to the large number of structures at this temperature. Insignificant resonance scattering implies that future instruments with higher spatial resolution could resolve the active region plasma into its component loop structures.
机译:经常使用共振散射来解释Fe XVIIλ15.01与Fe XVIIλ15.26的观察到的和预测的线比率(“ 3C / 3D”比率)之间的分歧。在此过程中,具有高得多的振荡器强度的λ15.01光子优先散射到视线之外,从而降低了观察到的线比。然而,最近的实验室测量发现,在15.21和15.26 A处有明显的内壳Fe XVI线,这表明观察到的3C / 3D比是混合产生的。鉴于我们对基本光谱学有了新的认识,我们重新检查了原始太阳光谱,确定了Fe XVIλ15.21线并测量其通量,以说明Fe XVI对λ15.26通量的贡献。消融使3C / 3D比率与实验比率良好吻合;因此,我们发现不需要调用共振散射。 Fe XVIIλ15.01中的低不透明性也意味着Fe XVλ284.2中的低不透明性,排除了共振散射是TRACE和SOHO-EIT 284 A图像模糊性的原因。相反,由于在此温度下存在大量结构,因此必须无法解析图像。微不足道的共振散射意味着未来具有更高空间分辨率的仪器可以将有源区等离子体解析为其组件回路结构。

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