首页> 外文期刊>The Astrophysical journal >MAGNETAR GIANT FLARES IN MULTIPOLAR MAGNETIC FIELDS. I. FULLY AND PARTIALLY OPEN ERUPTIONS OF FLUX ROPES
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MAGNETAR GIANT FLARES IN MULTIPOLAR MAGNETIC FIELDS. I. FULLY AND PARTIALLY OPEN ERUPTIONS OF FLUX ROPES

机译:多极磁场中的磁巨光晕。 I.完全和部分开放的磁通量喷发

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We propose a catastrophic eruption model for the enormous energy release of magnetars during giant flares, in which a toroidal and helically twisted flux rope is embedded within a force-free magnetosphere. The flux rope stays in stable equilibrium states initially and evolves quasi-statically. Upon the loss of equilibrium, the flux rope cannot sustain the stable equilibrium states and erupts catastrophically. During the process, the magnetic energy stored in the magnetosphere is rapidly released as the result of destabilization of global magnetic topology. The magnetospheric energy that could be accumulated is of vital importance for the outbursts of magnetars. We carefully establish the fully open fields and partially open fields for various boundary conditions at the magnetar surface and study the relevant energy thresholds. By investigating the magnetic energy accumulated at the critical catastrophic point, we find that it is possible to drive fully open eruptions for dipole-dominated background fields. Nevertheless, it is hard to generate fully open magnetic eruptions for multipolar background fields. Given the observational importance of the multipolar magnetic fields in the vicinity of the magnetar surface, it would be worthwhile to explore the possibility of the alternative eruption approach in multipolar background fields. Fortunately, we find that flux ropes may give rise to partially open eruptions in the multipolar fields, which involve only partial opening of background fields. The energy release fractions are greater for cases with central-arcaded multipoles than those with central-caved multipoles that emerged in background fields. Eruptions would fail only when the centrally caved multipoles become extremely strong.
机译:我们提出了一个巨大的爆发过程,用于在巨大的耀斑中释放出巨大的电磁波能量,其中环形和螺旋扭曲的通量绳嵌入无力的磁层中。通量绳最初保持稳定的平衡状态,并准静态地发展。一旦失去平衡,通量绳就无法维持稳定的平衡状态,并突然爆发。在此过程中,由于整体磁拓扑结构的不稳定,迅速释放了磁层中存储的磁能。可以累积的磁层能量对于爆发电磁波至关重要。我们仔细地建立了磁表面上各种边界条件的完全开放场和部分开放场,并研究了相关的能量阈值。通过研究在关键灾难点积累的磁能,我们发现有可能驱动以偶极子为主的背景场的完全开放爆发。然而,很难为多极背景场产生完全开放的磁爆发。考虑到磁极表面附近的多极磁场的观测重要性,有必要探讨在多极背景场中使用替代喷发方法的可能性。幸运的是,我们发现通量绳可能会在多极场中引起部分开放的喷发,这仅涉及背景场的部分开放。具有中心拱形多极的情况下的能量释放分数要大于出现在背景场中的具有中心凹形多极的情况。仅当中央塌陷的多极变得极强时,喷发才会失败。

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