期刊
PLANETARY AND SPACE SCIENCE
卷 99, 期 -, 页码 48-54出版社
PERGAMON-ELSEVIER SCIENCE LTD
DOI: 10.1016/j.pss.2014.05.007
关键词
Nanodust; Charged dust; Rosetta; 67P/CG
Nanodust particles are ubiquitous in the solar system; we may expect that comet 67P/Churyumov-Gerasimenko, the target of the upcoming ROSETTA mission, is also a source of nanodust, that is dust particles of nanometer size. Due to their small size and mass, the dust detectors cannot observe them directly neither on the orbiter nor on the Philae lander. However, if nanodust grains get charged, the ion and electron sensors on board of the orbiter might detect them. In this study we investigate whether this is a realistic option. We show that when the comet activity is low between 3.25 and 2.7 AU, the cometary-surface and a part of the dust particles get charged due to the charging currents of the solar wind and photoionization as a result of solar radiation. The nucleus' surface potential depends on the solar wind density, and it is higher than +4 V for solar zenith angle between 0 degrees and 50 degrees for solar wind density n(d=1 AU)=4 x 10(-6) m(-3), and nano-size dust gets immediately accelerated when it collected Q = + 1e positive charge due to photoelectron emission. The energy of this charged nanodust is higher than 4 eV and it could be detected not far from the subsolar region by the ion and electron sensor (IES) of the Rosetta Plasma Package. In this paper we examine this process in detail. (C) 2014 Published by Elsevier Ltd.
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