Mann Ingrid
Department of Physics and Technology, UiT the Artic University of Norway, Postboks 6050 Langnes, 9037 Tromsø, Norway
Philos Trans A Math Phys Eng Sci. 2017 Jul 13;375(2097). doi: 10.1098/rsta.2016.0254.
Comets, comet-like objects and their fragments are the most plausible source for the dust in both the inner heliosphere and planetary debris discs around other stars. The smallest size of dust particles in debris discs is not known and recent observational results suggest that the size distribution of the dust extends down to sizes of a few nanometres or a few tens of nanometres. In the Solar System, electric field measurements from spacecraft observe events that are explained with high-velocity impacts of nanometre-sized dust. In some planetary debris discs an observed mid- to near-infrared emission supposedly results from hot dust located in the vicinity of the star. And the observed emission is characteristic of dust of sizes a few tens of nanometres. Rosetta observations, on the other hand, provide little information on the presence of nanodust near comet 67P/Churyumov-Gerasimenko. This article describes why this is not in contradiction to the observations of nanodust in the heliosphere and in planetary debris discs. The direct ejection of nanodust from the nucleus of the comet would not contribute significantly to the observed nanodust fluxes. We discuss a scenario that nanodust forms in the interplanetary dust cloud through the high-velocity collision process in the interplanetary medium for which the production rates are highest near the Sun. Likewise, fragmentation by collisions occurs near the star in planetary debris discs. The collisional fragmentation process in the inner Solar System occurs at similar velocities to those of the collisional evolution in the interstellar medium. A question for future studies is whether there is a common magic size of the smallest collision fragments and what determines this size.This article is part of the themed issue 'Cometary science after Rosetta'.
彗星、类彗星天体及其碎片是内太阳系和其他恒星周围行星碎片盘中尘埃最合理的来源。目前尚不清楚碎片盘中尘埃颗粒的最小尺寸,最近的观测结果表明,尘埃的尺寸分布延伸至几纳米或几十纳米大小。在太阳系中,航天器的电场测量观测到的事件可通过纳米级尘埃的高速撞击来解释。在一些行星碎片盘中,观测到的中红外到近红外辐射据推测是由位于恒星附近的热尘埃产生的。而观测到的辐射是几十纳米大小尘埃的特征。另一方面,罗塞塔号的观测几乎没有提供关于67P/丘留莫夫-格拉西缅科彗星附近是否存在纳米尘埃的信息。本文阐述了为何这与在内太阳系和行星碎片盘中对纳米尘埃的观测并不矛盾。彗星核直接喷射出纳米尘埃对观测到的纳米尘埃通量贡献不大。我们讨论了一种情形,即纳米尘埃是在行星际尘埃云中通过行星际介质中的高速碰撞过程形成的,在靠近太阳的区域产生率最高。同样,在行星碎片盘中靠近恒星的地方也会发生碰撞破碎。内太阳系中的碰撞破碎过程发生的速度与星际介质中的碰撞演化速度相似。未来研究的一个问题是,最小碰撞碎片是否存在一个共同的神奇尺寸,以及是什么决定了这个尺寸。本文是主题为“罗塞塔号之后的彗星科学”特刊的一部分。