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arXiv 0802.2787astro-ph
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2003年10月28日富质子耀斑中3个震源的成因

On the origin of 3 seismic sources in the proton-rich flare of October 28, 2003

V. V. Zharkova, S. I. Zharkov

摘要:

本文给出了用MDI多普勒时距图技术探测到的S_1、S_2和S_3三个震源的位置、面积和可见波位移的垂直速度和水平速度。在120 μ m的数据立方体内,水平速度和波传播时间随震源略有不同。利用由硬X射线和$γ$射线发射以及由这些粒子引起的流体动力学冲击所导出的参数,将由源S1-S3的TD图所测得的动量和开始时间与由不同种类的高能粒子传递到光球的动量和开始时间进行了比较。高能质子(幂律结合准热的,或射流)被证明提供足够高的动量,并在燃烧的大气中形成流体动力学冲击,使它们能够通过更短的距离和时间被传递到光球层。然后,在源S2和S3中观测到的地震波可以用流体动力学冲击产生的动量来解释,流体动力学冲击是由混合质子束和喷流引起的,这些混合质子束和喷流几乎与硬X射线(HXR)和$γ$射线发射的第三次爆发同时发生在这些源的位置具有足点的环中。源S1中的地震波分别比第一次和第二次HXR爆发延迟4分钟和2分钟,可能与该环中发生的流体动力冲击有关,该流体动力冲击来自与这两次爆发中的任一次爆发产生的准热质子混合的具有较高能量截止的非常强大和硬的电子束的沉淀。

英文摘要:

The 3 seismic sources S1, S2 and S3 detected from MDI dopplergrams using the time-distance diagram technique are presented with the locations, areas and vertical and horizontal velocities of the visible wave displacements. Within the datacube of 120 Mm the horizontal velocities and the wave propagation times slightly vary from source to source. The momenta and start times measured from the TD diagrams in the sources S1-S3 are compared with those delivered to the photosphere by different kinds of high energy particles with the parameters deduced from hard X-ray and $γ$-ray emission as well as by the hydrodynamic shocks caused by these particles. The energetic protons (power laws combined with quasi-thermal ones, or jets) are shown to deliver momentum high enough and to form the hydrodynamic shocks deeply in a flaring atmosphere that allows them to be delivered to the photosphere through much shorter distances and times. Then the seismic waves observed in the sources S2 and S3 can be explained by the momenta produced by hydrodynamic shocks which are caused by mixed proton beams and jets occurring nearly simultaneously with the third burst of hard X-ray (HXR) and $γ$-ray emission in the loops with footpoints in the locations of these sources. The seismic wave in the source S1, delayed by 4 and 2 minutes from the first and second HXR bursts, respectively, is likely to be associated with a hydrodynamic shock occurring in this loop from precipitation of a very powerful and hard electron beam with higher energy cutoff mixed with quasi-thermal protons generated by either of these 2 bursts.

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