Observation of charged nanograins at comet 67P/Churyumov-Gerasimenko

被引:27
作者
Burch, J. L. [1 ]
Gombosi, T. I. [2 ]
Clark, G. [3 ]
Mokashi, P. [1 ]
Goldstein, R. [1 ]
机构
[1] Southwest Res Inst, San Antonio, TX 78238 USA
[2] Univ Michigan, AOSS Dept, Ann Arbor, MI 48109 USA
[3] Johns Hopkins Univ, Appl Phys Lab, Laurel, MD USA
基金
美国国家航空航天局;
关键词
ELECTRON SENSOR; DUST; PLASMA; IONS; IES;
D O I
10.1002/2015GL065177
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Soon after the Rosetta Orbiter rendezvoused with comet 67P/Churyumov-Gerasimenko at a solar distance of similar to 3.5 AU and began to fly in triangular-shaped trajectories around it, the Ion and Electron Sensor detected negative particles at energies from about 100 eV/q to over 18 keV/q. The lower energy particles came from roughly the direction of the comet; the higher-energy particles came from approximately the solar direction. These particles are interpreted as clusters of molecules, most likely water, which we refer to as nanograins because their inferred diameters are less than 100 nm. Acceleration of the grains away from the comet is through gas drag by the expanding cometary atmosphere, while acceleration back to the vicinity of the comet is caused partly by solar radiation pressure but mainly by the solar wind electric field. These observations represent the first measurements of energetic charged submicron-sized dust or ice grains (nanograins) in a cometary environment.
引用
收藏
页码:6575 / 6581
页数:7
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