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arXiv 2105.02454astro-ph.HEastro-ph.GA
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Gamma-ray亮活动星系核的干涉监测:测量4C +29.45的磁场强度

Interferometric Monitoring of Gamma-ray Bright AGNs: Measuring the Magnetic Field Strength of 4C +29.45

S. Kang, S. -S. Lee, J. Hodgson, J. -C. Algaba, J. W. Lee, J. -Y. Kim, J. Park, M. Kino, D. Kim, S. Trippe

摘要:

我们介绍了blazar 4C +29.45的多时期,多频率监测的结果,这是定期监测的伽马射线亮活动星系核(iMOGABA)计划的一部分-韩国甚长基线干涉测量网络(KVN)的一个关键科学计划。在2012年12月5日至2016年12月28日的4年间,在22、43、86和129 GHz同时进行了观测。我们还使用了来自15 GHz欧文斯谷射电天文台(OVRO)监测计划的其他数据。从15 GHz的光变曲线,我们估计的变化时间尺度的源在几个无线电通量增强。我们发现,在观测期间,该源经历了6次射电通量增强,变率时间尺度为9-187天,相应的变率多普勒因子为9-27。从多频同步KVN观测,我们能够获得准确的无线电频谱的源,从而更精确地测量的周转频率$ν_{\rm r}$的同步辐射自吸收(SSA)的平均值为$ν_{rm r}$ = 28.9 GHz的发射。使用射流几何假设,我们估计的发射区域的大小在周转频率。我们发现,均分磁场强度是高达两个数量级高于SSA磁场强度(0.001-0.1 G)。这与粒子主导的源是一致的。我们仔细分析了与这些估计相关的系统误差。结果表明,均布区位于SSA区的上游。

英文摘要:

We present the results of multi-epoch, multi-frequency monitoring of a blazar 4C +29.45, which was regularly monitored as part of the Interferometric Monitoring of GAmma-ray Bright Active Galactic Nuclei (iMOGABA) program - a key science program of the Korean Very long baseline interferometry Network (KVN). Observations were conducted simultaneously at 22, 43, 86, and 129 GHz during the 4 years from 5 December 2012 to 28 December 2016. We also used additional data from the 15 GHz Owens Valley Radio Observatory (OVRO) monitoring program. From the 15 GHz light curve, we estimated the variability time scales of the source during several radio flux enhancements. We found that the source experienced 6 radio flux enhancements with variability time scales of 9-187 days during the observing period, yielding corresponding variability Doppler factors of 9-27. From the multi-frequency simultaneous KVN observations, we were able to obtain accurate radio spectra of the source and hence to more precisely measure the turnover frequencies $ν_{\rm r}$ of synchrotron self-absorbed (SSA) emission with a mean value of $ν_{rm r}$ = 28.9 GHz. Using jet geometry assumptions, we estimated the size of the emitting region at the turnover frequency. We found that the equipartition magnetic field strength is up to two orders of magnitudes higher than the SSA magnetic field strength (0.001-0.1 G). This is consistent with the source being particle dominated. We performed a careful analysis of the systematic errors related to making these estimations. From the results, we concluded that the equipartition region locates upstream the SSA region.

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