In-orbit calibration of the lunar magnetometer onboard SELENE (KAGUYA)

被引:43
|
作者
Takahashi, Futoshi [1 ]
Shimizu, Hisayoshi [2 ]
Matsushima, Masaki [1 ]
Shibuya, Hidetoshi [3 ]
Matsuoka, Ayako [4 ]
Nakazawa, Satoru [5 ]
Iijima, Yuichi [4 ]
Otake, Hisashi [5 ]
Tsunakawa, Hideo [1 ]
机构
[1] Tokyo Inst Technol, Dept Earth & Planetary Sci, Tokyo 1528551, Japan
[2] Univ Tokyo, Earthquake Res Inst, Tokyo 1130032, Japan
[3] Kumamoto Univ, Dept Earth & Environm Sci, Kumamoto 8608555, Japan
[4] Japan Aerosp Explorat Agcy, Inst Space & Astronaut Sci, Sagamihara, Kanagawa 2298510, Japan
[5] Japan Aerosp Explorat Agcy, Lunar & Planetary Explorat Program Grp, Tsukuba, Ibaraki 3058505, Japan
来源
EARTH PLANETS AND SPACE | 2009年 / 61卷 / 11期
关键词
SELENE (KAGUYA); lunar magnetic field; magnetometer; in-orbit calibration; CRUSTAL MAGNETIC-ANOMALIES;
D O I
10.1186/BF03352979
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The high-sensitivity fluxgate Lunar MAGnetometer (LMAG) is mounted on SELENE (KAGUYA) to investigate the near-surface electromagnetic environment and the evolution of the Moon through magnetic field observation. To avoid possible electromagnetic interferences, a triaxial fluxgate sensor (MGF-S) is installed at the far end of a 12-m-long mast. It is critical for the accurate observation to monitor MGF-S alignment in orbit, and thus We have calibrated the sensor alignment by measuring the known magnetic fields generated by the sensor alignment monitor coil (SAM-C) Wound onto the mast canister. In-orbit calibration of the MGF-S alignment Was performed twice each revolution during the initial check-out phase of the satellite. It is concluded that there is no systematic difference in the sensor alignment between the day-side and night-side. Applying a new technique based oil the Davis-Smith method to the observed magnetic field data when KAGUYA was exposed to the solar wind, a zero offset of each axis was quickly and stably determined every month. As a result, LMAG has been calibrated with an accuracy that is sufficient for detection of the lunar magnetic anomaly at an altitude of 100 km and for high-resolution electron reflectometry.
引用
收藏
页码:1269 / 1274
页数:6
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