论文标题
VEGA长达十年的磁监测
A decade-long magnetic monitoring of Vega
论文作者
论文摘要
目标。在VEGA表面检测到的非常弱的磁场,在A和B光谱类型的弱磁星的广泛种群中检测到。我们在这里为通过研究该原型恒星的田间几何形状的长期稳定性来收集有关这种磁性起源的更多线索。方法。我们将收集的光谱数据作为长期运动的一部分,在2008年至2018年之间进行了2,000多个观察结果。使用从整个时间序列中提取的各种子集,我们重建了大型表面磁场的几个地图。结果。我们确认偏振信号是根据$ \ sim 0.68 $ d期调制的,我们将其解释为恒星旋转期。表面磁场在复杂的几何形状中组织。我们证实存在先前报道的Vega的非常局部的极性磁斑,径向场强度约为-5 g。我们表明,恒星的表面也被偶极子覆盖,极强度接近9 g,偶极子倾斜度接近90^\ circ $。两种磁性结构在十年中都非常稳定。可用的数据表明,较小的磁斑可能不限于极性区域,尽管重建的可靠性差并不能使我们对它们的时间演变牢固地得出结论。
Aims. The very weak magnetic field detected at the surface of Vega hints at a widespread population of weakly magnetic stars of A and B spectral types. We contribute here to gather more clues about the origin of this magnetism by investigating the long-term stability of the field geometry of this prototypical star. Methods. We use spectropolarimetric data collected as part of a long-term campaign, with more than 2,000 observations spread between 2008 and 2018. Using various sub-sets extracted from the whole time series, we reconstruct several maps of the large-scale surface magnetic field. Results. We confirm that the polarimetric signal is modulated according to a $\sim 0.68$ d period, which we interpret as the stellar rotation period. The surface magnetic field is organized in a complex geometry. We confirm the existence of a very localized, polar magnetic spot previously reported for Vega, with a radial field strength of about -5 G. We show that the surface of the star is also covered by a dipole, with a polar strength close to 9 G and a dipole obliquity close to $90^\circ$. Both magnetic structures are remarkably stable over one decade. The available data suggest that smaller-scale magnetic spots may not be limited to the polar region, although the poor reliability of their reconstruction does not allow us to firmly conclude about their temporal evolution.