Distribution and dynamics of decimetre-sized dust agglomerates in the coma of 67P/Churyumov-Gerasimenko

被引:4
|
作者
Lemos, Pablo [1 ,2 ]
Agarwal, Jessica [1 ,2 ]
Schroter, Matthias [3 ]
机构
[1] Tech Univ Carolo Wilhelmina Braunschweig, Inst Geophys & Extraterr Phys, Mendelssohnstr 3, D-38106 Braunschweig, Germany
[2] Max Planck Inst Solar Syst Res, Justus von Liebig Weg 3, D-37077 Gottingen, Germany
[3] Max Planck Inst Dynam & Self Org, Fassberg 17, D-37077 Gottingen, Germany
基金
欧洲研究理事会;
关键词
methods: data analysis; methods: numerical; comets: individual: 67P/Churyumov-Gerasimenko; ATMOSPHERELESS BODIES; RADIATIVE-TRANSFER; PHASE FUNCTION; 2.2; AU; OSIRIS; EVOLUTION; SURFACES; GIADA; GAS;
D O I
10.1093/mnras/stad032
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We present a method to analyse images of the coma of 67P/Churyumov-Gerasimenko obtained using OSIRIS, the main imaging system on-board Rosetta, where dust aggregates can be seen as bright tracks because of their relative velocity with respect to the spacecraft. We applied this method to 105 images taken in 2015 July, 2015 December, and 2016 January, identifying more than 20 000 individual objects. We performed a photometric analysis of them, finding their phase function. This phase function follows the same trend as the one found for the nucleus, consistent with the detected particles having a size larger than similar to 1 mm. Additionally, the phase function becomes shallower for increasing heliocentric distances, indicating a decrease in the mean agglomerate size. In order to characterize the agglomerates observed in the image, we developed a simplified model for their ejection and dynamics in the coma, and generated synthetic images based on it. We solved the inverse problem by finding the simulation parameters that give the best fit between synthetic and real images. In doing so, we were able to obtain a mean agglomerate size similar to dm and initial speed similar or equal to 1ms(-1). Both show a decrease with increasing heliocentric distance, sign of the reduction in activity. Also, the sizes obtained by the comparison are not compatible with ejection caused by water activity, so other sources have to be invoked, mainly CO2.
引用
收藏
页码:5775 / 5786
页数:12
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