在彗星拦截器的背景下:彗星彗发和小天体表面的一些尘埃粒子的意想不到的偏振特性

A. Levasseur-Regourd, E. Hadamcik, J. Lasue, J. Milli, J. Renard
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引用次数: 0

摘要

ESA-JAXA彗星拦截器任务预计将飞越一颗动态的新彗星(或星际彗星),并更好地揭示其尘埃颗粒和核表面的特性。因此,我们暂时比较了一些彗星释放的尘埃的偏振特性,以及一些小天体表面上的尘埃。彗星尘埃粒子的线偏振相位曲线(在等效波长范围内观察到)显示出类似的趋势。然而,一些独特的动态新彗星或碎片彗星(如C/1995 O1 Hale-Bopp, C/1999 S4 LINEAR)可能比哈雷彗星或木星族彗星(如1P/哈雷,67P/Churyumov-Gerasimenko)呈现更高的正分支。这些差异是尘埃颗粒性质(大小、形态、复杂光学指数)差异的线索。由彗核频繁撞击太阳系内部所喷射出的尘埃粒子,确实可能部分来自相当致密的表层,正如罗塞塔号在67P彗星的小叶上所探测到的那样[1]。虽然对彗星核表面的偏振观测几乎是不可能的,但对1P/Encke相当静止的核的观测已经获得[2]。可以指出,1P/Encke与非典型小天体(如Phaeton,特别是Bennu[3])以及彗星彗发尘埃的偏振特性之间存在相似性。数值模拟和实验室模拟可能是更好地理解这种相似性的独特工具。还可以补充说,来自彗星的尘埃颗粒,特别是木星家族的尘埃颗粒,可能会以CP-IDPs的形式在地球的平流层中被收集,并且在恒星系统的碎片盘中发现的尘埃显示出与高极化彗星相似的极化水平[4]. [1]Kofman等,地球物理学报,497,2616-2622,2020,[2]Boehnhardt等,A&A, 489, 1337-1343, 2008。[3]李晓明,李晓明,李晓明,等。[4] Levasseur-Regourd等人,PSS, 186, 104896, 2020, 
本文章由计算机程序翻译,如有差异,请以英文原文为准。
In the context of Comet Interceptor: Unexpected polarimetric properties of some dust particles in cometary comae and on small bodies surfaces

The ESA-JAXA Comet Interceptor mission is expected to flyby a dynamically new comet (or an interstellar one) and better reveal the properties of its dust particles and nucleus surface. We therefore tentatively compare polarimetric properties of dust released by some comets, as well as present on surfaces of some small bodies.

Phase curves of the linear polarization of cometary dust particles (observed in equivalent wavelength ranges) show analogous trends. Some unique dynamically new comets or fragmenting comets (e.g. C/1995 O1 Hale-Bopp, C/1999 S4 LINEAR) may nevertheless present a higher positive branch than Halley-type or Jupiter-family comets (e.g. 1P/Halley, 67P/Churyumov-Gerasimenko). Such differences are clues to differences in the properties (sizes, morphologies, complex optical indices) of the dust particles. Dust particles, ejected by nuclei frequently plunging in the inner Solar System, might indeed partly come from quite dense a surface layer, as detected on the small lobe of comet 67P by Rosetta [1].

Although polarimetric observations of surfaces of cometary nuclei are almost impossible, observations of the rather quiescent nucleus of 1P/Encke have been obtained [2].  Similarities between polarimetric properties of 1P/Encke and atypical small bodies (e.g. Phaeton and particularly Bennu [3]), and of dust in cometary comae may be pointed out. Numerical and laboratory simulations could represent a unique tool to better understand such similarities. It may also be added that dust particles originating from comets, with emphasis on those of Jupiter-family, may survive atmospheric entry, as CP-IDPs collected in the Earth’s stratosphere, and that dust found in debris disks of stellar systems shows levels of polarization similar to those of highly-polarized comets [4].

 

[1] Kofman et al., MNRAS, 497, 2616-2622, 2020, [2] Boehnhardt et al., A&A, 489, 1337-1343, 2008. [3] Cellino et al., MNRAS, 481, L49-L53, 2018. [4] Levasseur-Regourd et al., PSS, 186, 104896, 2020,

 

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