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首页> 外文期刊>The astronomical journal >The 2016 Reactivations of the Main-belt Comets 238P/Read and 288P/(300163) 2006 VW 139
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The 2016 Reactivations of the Main-belt Comets 238P/Read and 288P/(300163) 2006 VW 139

机译:2016年重新启用皮带彗星238P / Read和288P /(300163)2006 VW 139

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We report observations of the reactivations of the main-belt comets (MBCs) 238P/Read and 288P/(300163) 2006 VW 139 that also track the evolution of each object’s activity over several months in 2016 and 2017. We additionally identify and analyze archival SDSS data showing 288P to have been active in 2000, meaning that both 238P and 288P have now each been confirmed to be active near perihelion on three separate occasions. From data obtained of 288P from 2012–2015 when it appeared inactive, we find best-fit R-band H, G phase function parameters of H R ?=?16.80?±?0.12 mag and G R ?=?0.18?±?0.11, corresponding to effective component radii of r c ?=?0.80?±?0.04 km, assuming a binary system with equally sized components. Fitting linear functions to ejected dust masses inferred for 238P and 288P soon after their observed reactivations in 2016, we find an initial average net dust production rate of = ˙ M 0.7 0.3 d kg?s ?1 and a best-fit start date of 2016 March 11 (when the object was at a true anomaly of ν?=??63°) for 238P, and an initial average net dust production rate of = ? ˙ M 5.6 0.7 d kg?s ?1 and a best-fit start date of 2016 August 5 (when the object was at ν?=??27°) for 288P. Applying similar analyses to archival data, we find similar start points for previous active episodes for both objects, suggesting that minimal mantle growth or ice recession occurred between the active episodes in question. Some changes in dust production rates between active episodes are detected, however. More detailed dust modeling is suggested to further clarify the process of activity evolution in MBCs.
机译:我们报告了对主带状彗星(MBC)238P / Read和288P /(300163)2006 VW 139的重新激活的观察结果,这些活动还跟踪了2016年和2017年几个月中每个对象活动的演变。我们另外识别和分析了档案SDSS数据显示288P在2000年已经处于活动状态,这意味着现在已分别在三个不同的场合确认了238P和288P在近日点附近都处于活动状态。从2012-2015年288P处于非活动状态时获得的数据中,我们发现HR?=?16.80?±?0.12 mag和GR?=?0.18?±?0.11的最佳拟合R波段H,G相位函数参数,假设二元系统具有相同大小的分量,则它对应于有效分量半径rc =?0.80?±?0.04 km。将线性函数拟合到2016年观察到的238P和288P推算出的尘埃质量后,我们发现初始平均净粉尘产生率为=˙M 0.7 0.3 d kg?s?1,最合适的开始日期为2016年3月11日(当物体处于ν?=Δ63°的真实异常时)为238P,初始平均净粉尘产生率为=。 ˙M 5.6 0.7 d kg?s?1,最合适的开始日期为2016年8月5日(当物体位于ν?=?27°时)为288P。将类似的分析应用于档案数据,我们发现两个对象先前的活跃事件都具有相似的起点,这表明在所讨论的活跃事件之间发生了最小的地幔生长或冰期衰退。但是,检测到活动事件之间的粉尘产生速率有一些变化。建议使用更详细的粉尘模型,以进一步阐明MBC中活动演变的过程。

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