论文标题
六月epsilon ophiuchids Meteoroid流和300p/catalina的表征
Characterization of the June epsilon Ophiuchids meteoroid stream and the comet 300P/Catalina
论文作者
论文摘要
在2019年之前,六月的Epsilon Ophiuchids(JEO)被称为较小的未经证实的流星淋浴,其活动通常被认为是明亮的火球。在2019年6月观察到了一场意外的活动,这甚至增加了与波多黎各附近小行星2019年MO的影响有关的可能性。早期报告还指出了淋浴与300p/catalina彗星轨道的相似性。我们旨在分析JEO Meteoroids的轨道,发射光谱和物质强度,以提供此流的表征,识别其母体对象,并评估其与影响的小行星2019 MO的联系。我们的分析基于22种JEO流星轨道的样本以及加那利群岛和智利的AMOS网络观察到的4个发射光谱。使用轨道相似性D标准以及彗星300p和JEO流的轨道的向后积分的组合评估了与潜在母体的链接。我们确认了源自JEO流中的一群流星体的意外群的报道。 JEO流星体具有较低的材料强度,其特征是脆弱的彗星体,并且表现出多孔结构的迹象。与所有其他测得的彗星流相比,发射光谱显示铁含量略有增加,但通常与原始的软骨组成一致。进一步的动态分析表明,JEO流很可能起源于300p/catalina彗星,并且在过去的1000年内形成。在较长的时间尺度上,由于彗星的湍流轨道演化,流中的流星体移至混沌轨道。我们的结果还表明,6月22日小行星2019年MO的影响与JEO活动无关。
Prior to 2019, the June epsilon Ophiuchids (JEO) were known as a minor unconfirmed meteor shower with activity that was considered typically moderate for bright fireballs. An unexpected bout of enhanced activity was observed in June 2019, which even raised the possibility that it was linked to the impact of the small asteroid 2019 MO near Puerto Rico. Early reports also point out the similarity of the shower to the orbit of the comet 300P/Catalina. We aim to analyze the orbits, emission spectra, and material strengths of JEO meteoroids to provide a characterization of this stream, identify its parent object, and evaluate its link to the impacting asteroid 2019 MO. Our analysis is based on a sample of 22 JEO meteor orbits and four emission spectra observed by the AMOS network at the Canary Islands and in Chile. The link to potential parent objects was evaluated using a combination of orbital-similarity D-criteria and backwards integration of the orbit of comet 300P and the JEO stream. We confirm the reports of an unexpected swarm of meteoroids originating in the JEO stream. JEO meteoroids have low material strengths characteristic for fragile cometary bodies, and they exhibit signs of a porous structure. The emission spectra reveal slightly increased iron content compared to all other measured cometary streams, but they are generally consistent with a primitive chondritic composition. Further dynamical analysis suggests that the JEO stream is likely to originate from comet 300P/Catalina and that it was formed within the last 1000 years. Over longer timescales, the meteoroids in the stream move to chaotic orbits due to the turbulent orbital evolution of the comet. Our results also suggest that the impact of the small asteroid 2019 MO on June 22 was not connected to the JEO activity.