首页> 外文期刊>Astronomy and astrophysics >Long-term activity and outburst of comet C/2013 A1 (Siding Spring) from narrow-band photometry and long-slit spectroscopy
【24h】

Long-term activity and outburst of comet C/2013 A1 (Siding Spring) from narrow-band photometry and long-slit spectroscopy

机译:窄带光度法和长缝光谱学对彗星C / 2013 A1(侧板弹簧)的长期活动和爆发

获取原文
           

摘要

We present a unique data set of more than one year’s worth of regular observations of comet C/2013 A1(Siding Spring) taken with TRAPPIST, along with low-resolution spectra obtained with the ESO/VLT FORS 2 instrument. The comet made a close approach to Mars on October 19, 2014, and was then observed by many space-borne and ground-based telescopes. We followed the evolution of the OH, NH, CN, C_(3) , and C_(2) production rates as well as the Afρ parameter, a proxy for the dust production. We detected an outburst two weeks after perihelion, with gas and dust production rates increased by a factor of five within a few days. By modelling the shape of the CN and C_(2) radial profiles, we determined that the outburst happened on November 10 around 15:30 UT ( ± 5 h) and measured a gas expansion velocity of 1.1 ± 0.2 km?s ~(-1) . We used a thermal evolution model to reproduce the activity pattern and outburst. Our results are consistent with the progressive formation of a dust mantle explaining the shallow dependence of gas production rates, which may be partially blown off during the outburst. We studied the evolution of gas composition, using various ratios such as CN/OH, C_(2) /OH, or C_(3) /OH, which showed little or no variation with heliocentric distance, including at the time of the outburst. This indicates a relative level of homogeneity of the nucleus composition.
机译:我们提供了一个独特的数据集,其中包括用TRAPPIST进行的对C / 2013 A1(春季板壁)彗星的定期观测,以及使用ESO / VLT FORS 2仪器获得的低分辨率光谱的常规观测值。彗星于2014年10月19日接近火星,随后被许多星载和地基望远镜观测到。我们跟踪了OH,NH,CN,C_(3)和C_(2)生产率以及Afρ参数(粉尘产生的替代指标)的演变过程。我们在近日点攻击后两周发现爆发,几天内气体和粉尘产生率增加了五倍。通过对CN和C_(2)径向剖面的形状进行建模,我们确定爆发发生在11月10日UT 15:30(±5 h)左右,并且测得的气体膨胀速度为1.1±0.2 km?s〜(- 1)。我们使用热演化模型来再现活动模式和爆发。我们的结果与粉尘罩的逐步形成是一致的,这说明了瓦斯产生速率的依赖性很弱,在爆发期间可能被部分吹散。我们使用各种比率(例如CN / OH,C_(2)/ OH或C_(3)/ OH)研究了气体成分的演变,这些比率随日心距的变化很小,甚至没有变化,包括在爆发时。这表明核组成的相对均质性。

著录项

相似文献

  • 外文文献
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号