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天王星磁层中的高能带电粒子。

Energetic charged particles in the uranian magnetosphere.

作者信息

Stone E C, Cooper J F, Cummings A C, McDonald F B, Trainor J H, Lal N, McGuire R, Chenette D L

出版信息

Science. 1986 Jul 4;233(4759):93-7. doi: 10.1126/science.233.4759.93.

Abstract

During the encounter with Uranus, the cosmic ray system on Voyager 2 measured significant fluxes of energetic electrons and protons in the regions of the planets magnetosphere where these particles could be stably trapped. The radial distribution of electrons with energies of megaelectron volts is strongly modulated by the sweeping effects ofthe three major inner satellites Miranda, Ariel, and Umbriel. The phase space density gradient of these electrons indicates that they are diffusing radially inward from a source in the outer magnetosphere or magnetotail. Differences in the energy spectra of protons having energies of approximately 1 to 8 megaelectron volts from two different directions indicate a strong dependence on pitch angle. From the locations of the absorption signatures observed in the electron flux, a centered dipole model for the magnetic field of Uranus with a tilt of 60.1 degrees has been derived, and a rotation period of the planet of 17.4 hours has also been calculated. This model provides independent confirmaton of more precise determinations made by other Voyager experiments.

摘要

在与天王星相遇期间,“旅行者2号”上的宇宙射线系统在行星磁层中粒子能够稳定捕获的区域测量到了高能电子和质子的显著通量。具有兆电子伏特能量的电子的径向分布受到三大内侧卫星米兰达、艾瑞尔和天卫二的扫掠效应的强烈调制。这些电子的相空间密度梯度表明它们正从外磁层或磁尾的一个源径向向内扩散。来自两个不同方向的能量约为1至8兆电子伏特的质子能谱差异表明对俯仰角有很强的依赖性。根据在电子通量中观测到的吸收特征位置,推导出了天王星磁场的中心偶极模型,其倾斜度为60.1度,还计算出了该行星17.4小时的自转周期。该模型为其他“旅行者”号实验做出的更精确测定提供了独立验证。

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