RESULTS FROM ACTIVE SPACECRAFT POTENTIAL CONTROL ON THE GEOTAIL SPACECRAFT

被引:40
作者
SCHMIDT, R
ARENDS, H
PEDERSEN, A
RUDENAUER, F
FEHRINGER, M
NARHEIM, BT
SVENES, R
KVERNSVEEN, K
TSURUDA, K
MUKAI, T
HAYAKAWA, H
NAKAMURA, M
机构
[1] AUSTRIAN RES CTR SEIBERSDORF, A-2444 SEIBERSDORF, AUSTRIA
[2] INST SPACE & ASTRONAUT SCI, SAGAMIHARA, KANAGAWA 229, JAPAN
[3] UNIV TOKYO, DEPT EARTH & PLANETARY SCI, TOKYO, JAPAN
关键词
D O I
10.1029/95JA01552
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
A low and actively controlled electrostatic potential on the outer surfaces of a scientific spacecraft is very important for accurate measurements of cold plasma electrons and ions and the DC to low-frequency electric field. The Japanese/NASA Geotail spacecraft carries as part of its scientific payload a novel ion emitter for active control of the electrostatic potential on the surface of the spacecraft. The aim of the ion emitter is to reduce the positive surface potential which is normally encountered in the outer magnetosphere when the spacecraft is sunlit. Ion emission clamps the surface potential to near the ambient plasma potential. Without emission control, Geotail has encountered plasma conditions in the lobes of the magnetotail which resulted in surface potentials of up to about +70 V, The ion emitter proves to be able to discharge the outer surfaces of the spacecraft and is capable of keeping the surface potential stable at about +2 V. This potential is measured with respect to one of the electric field probes which are current biased and thus kept at a potential slightly above the ambient plasma potential. The instrument uses the liquid metal field ion emission principle to emit indium ions. The ion beam energy is about 6 keV and the typical total emission current amounts to about 15 mu A. Neither variations in the ambient plasma conditions nor operation of two electron emitters on Geotail produce significant variations of the controlled surface potential as long as the resulting electron emission currents remain much smaller than the ion emission current. Typical results of the active potential control are shown, demonstrating the surface potential reduction and its stability over time.
引用
收藏
页码:17253 / 17259
页数:7
相关论文
共 25 条
[1]  
DECREAU PME, 1978, SPACE SCI REV, V22, P633
[2]   PLASMA CLOUDS IN MAGNETOSPHERE [J].
DEFOREST, SE ;
MCILWAIN, CE .
JOURNAL OF GEOPHYSICAL RESEARCH, 1971, 76 (16) :3587-+
[4]  
FEUERBACHER B, 1972, J APPL PHYS, V45, P1563
[5]   THE CHARGING OF SPACECRAFT SURFACES [J].
GARRETT, HB .
REVIEWS OF GEOPHYSICS, 1981, 19 (04) :577-616
[6]   PROPERTIES OF SATELLITE PHOTOELECTRON SHEATH DERIVED FROM PHOTOEMISSION LABORATORY MEASUREMENTS [J].
GRARD, RJL .
JOURNAL OF GEOPHYSICAL RESEARCH, 1973, 78 (16) :2885-2906
[7]   THE POTENTIAL OF AN ELECTROSTATICALLY CLEAN GEOSTATIONARY SATELLITE AND ITS USE IN PLASMA DIAGNOSTICS [J].
KNOTT, K ;
DECREAU, PME ;
KORTH, A ;
PEDERSEN, A ;
WRENN, GL .
PLANETARY AND SPACE SCIENCE, 1984, 32 (02) :227-237
[9]  
LINDQVIST PA, 1983, ESA SP198, P25
[10]  
MCPHERSON DA, 1976, PROGR ASTRONAUTICS A, V47, P15