Mercury:: Thermal modeling and mid-infrared (5-12 μm) observations

被引:92
作者
Emery, JP [1 ]
Sprague, AL
Witteborn, FC
Colwell, JE
Kozlowski, RWH
Wooden, DH
机构
[1] Univ Arizona, Lunar & Planetary Lab, Tucson, AZ 85721 USA
[2] Univ Colorado, Atmospher & Space Phys Lab, Boulder, CO 80309 USA
[3] Susquehanna Univ, Selingsgrove, PA 17870 USA
[4] NASA, Ames Res Ctr, Mt View, CA 94035 USA
关键词
thermal modeling; Mercury surface composition; Mercury; planetary surfaces;
D O I
10.1006/icar.1998.6012
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
We present and use a new rough-surface thermal model to aid in the analysis of new mid-infrared spectral measurements of Mercury from 5-12.5 mu m. The model calculates spatially resolved thermal emission from slowly rotating, airless bodies. The Mercury data contain the first spectral measurements of Mercury between 5-7.5 mu m, a region not accessible from ground-based telescopes, and are also the first observations of Mercury to be made while flying on the Kuiper Airborne Observatory (KAO). They were obtained with the High-efficiency Infrared Faint Object Grating Spectrometer (HIFOGS). Our rough surface thermal model which best fit the KAO data has a Hapke <(theta)over bar> of 20 degrees. A strong 5-mu m emission feature was present during both observing periods. We suggest the 5-mu m excess may be a result of near surface thermal gradients in regolith materials with a 30 to 100-mu m grainsize, but cannot entirely rule out an observational artifact resulting from our instrumentation or the telescope on the KAO, Other features in the spectra are consistent with a feldspathic and feld-spathoidal surface composition. (C) 1998 Academic Press.
引用
收藏
页码:104 / 123
页数:20
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