Data processing and preliminary results of the Chang'e-3 VIS/NIR Imaging Spectrometer in-situ analysis

被引:0
|
作者
Bin Liu [1 ]
Chun-Lai Li [1 ]
Guang-Liang Zhang [1 ]
Rui Xu [2 ]
Jian-Jun Liu [1 ]
Xin Ren [1 ]
Xu Tan [1 ]
Xiao-Xia Zhang [1 ]
Wei Zuo [1 ]
Wei-Bin Wen [1 ]
机构
[1] Key Laboratory of Lunar and Deep Space Exploration, National Astronomical Observatories,Chinese Academy of Sciences
[2] Key Laboratory of Space Active Opto-Electronics Technology, Shanghai Institute of Technical,Physics, Chinese Academy of Sciences
基金
中国国家自然科学基金;
关键词
Chang’e-3 — VNIS — in-situ analysis — data processing;
D O I
暂无
中图分类号
P184.5 [月球表面物理及观测方法];
学科分类号
070401 ;
摘要
The Chang’e-3 Visible and Near-infrared Imaging Spectrometer(VNIS) is one of the four payloads on the Yutu rover. After traversing the landing site during the first two lunar days, four different areas are detected, and Level 2A and 2B radiance data have been released to the scientific community. The released data have been processed by dark current subtraction, correction for the effect of temperature,radiometric calibration and geometric calibration. We emphasize approaches for reflectance analysis and mineral identification for in-situ analysis with VNIS. Then the preliminary spectral and mineralogical results from the landing site are derived. After comparing spectral data from VNIS with data collected by the M3 instrument and samples of mare that were returned from the Apollo program, all the reflectance data have been found to have similar absorption features near 1000 nm except lunar sample71061. In addition, there is also a weak absorption feature between 1750~2400 nm on VNIS, but the slopes of VNIS and M3 reflectance at longer wavelengths are lower than data taken from samples of lunar mare. Spectral parameters such as Band Centers and Integrated Band Depth Ratios are used to analyze mineralogical features. The results show that detection points E and N205 are mixtures of high-Ca pyroxene and olivine,and the composition of olivineat point N205 is higher than that at point E, but the compositions of detection points S3 and N203 are mainly olivine-rich. Since there are no obvious absorption features near 1250 nm, plagioclase is not directly identified at the landing site.
引用
收藏
页码:1578 / 1594
页数:17
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