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Interplanetary Dust, Meteoroids, Meteors and Meteorites

机译:尘埃粉尘,流星,流星和陨石

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Interplanetary dust particles and meteoroids mostly originate from comets and asteroids. Understanding their distribution in the Solar system, their dynamical behavior and their properties, sheds light on the current state and the dynamical behavior of the Solar system. Dust particles can endanger Earth-orbiting satellites and deep-space probes, and a good understanding of the spatial density and velocity distribution of dust and meteoroids in the Solar system is important for designing proper spacecraft shielding. The study of interplanetary dust and meteoroids provides clues to the formation of the Solar system. Particles having formed 4.5 billion years ago can survive planetary accretion and those that survived until now did not evolve significantly since then. Meteoroids and interplanetary dust can be observed by measuring the intensity and polarization of the zodiacal light, by observing meteors entering the Earth's atmosphere, by collecting them in the upper atmosphere, polar ices and snow, and by detecting them with in-situ detectors on space probes.
机译:截然粉尘颗粒和菱形主要来自彗星和小行星。了解他们在太阳系中的分配,它们的动态行为及其性质,揭示了当前状态和太阳系的动力学行为。灰尘颗粒可以危及地球轨道卫星和深空探头,并且良好地了解太阳系中的灰尘和沟槽的空间密度和速度分布对于设计适当的航天器屏蔽是重要的。截然灰尘和菱形的研究提供了太阳系形成的线索。形成了45亿年前的颗粒可以存活行星炎症和那些幸存下来的人,直到现在以来不会显着发展。通过在高层大气,极地冰雪和雪中收集进入地球大气的流星,通过观察到八抗灯光的强度和极化,可以观察到陨石和行星灰尘,通过在高层大气,极地冰雪和雪中收集它们,并通过在空间上的原位探测器检测它们探针。

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