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Dust at the Martian moons and in the circummartian space

机译:火星月球和环绕环境中的尘埃

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The paper provides the current understanding of the dust particle dynamics near the surface and in the circummatrian space of the Martian moons based on existing models developed for airless and non-magnetized bodies. In particular we discuss the response of the regolith of the Martian moons to exposure to radiation, the dynamics of charged dust on their surfaces, their plasma environments, the models and indirect observations of their putative dust tori. It is concluded that there is a good theoretical understanding of the behavior of the dynamics of dust particles near the moons Phobos and Deimos. Current models predict dust rings near orbits of the Martian moons based on detailed estimates for the sources and sinks of the dust particles as well as their lifetimes. However, there is no compelling observational evidence for the predicted dust torus around Phobos or Deimos orbits, and there are no observations yet of dust dynamics near their surfaces. Naturally, in order to detect the motion of dust near the surfaces of these moons, and their dust tori we need measurements using a complementary set of sensitive instruments, including impart dust detectors, electric field sensors, and optical cameras in future missions to Mars and its moons.
机译:本文基于为无气和非磁化物体开发的现有模型,提供了对火星卫星表面和周围环境中尘埃粒子动力学的最新理解。特别是,我们讨论了火星卫星的碎石对暴露于辐射的响应,其表面带电尘埃的动力学,等离子环境,模型及其推定尘埃花托的间接观测。可以得出结论,对卫星Phobos和Deimos附近的尘埃动力学具有良好的理论理解。当前的模型是根据对尘埃粒子的来源和沉降及其寿命的详细估算,来预测火星卫星轨道附近的尘埃环。但是,目前还没有令人信服的观测证据可证明火卫一或狄莫斯轨道周围的尘埃圆环,并且还没有观测到它们表面附近的尘埃动力学。自然地,为了检测尘埃在这些卫星表面附近的运动及其尘埃托,我们需要使用一套互补的敏感仪器进行测量,包括在未来的火星探测任务中配备尘埃探测器,电场传感器和光学相机。它的卫星。

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