Estimated Optical Constants of Calcite at visible to mid-infrared wavelengths (0.3-6 μm)

Physics

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[3672] Mineralogy And Petrology / Planetary Mineralogy And Petrology, [3934] Mineral Physics / Optical, Infrared, And Raman Spectroscopy, [5410] Planetary Sciences: Solid Surface Planets / Composition, [5464] Planetary Sciences: Solid Surface Planets / Remote Sensing

Scientific paper

Carbonate minerals are germane to questions involving volatile and climate history on Mars [e.g., 1,2]. Spectral observations provide evidence for the presence of carbonates in the Martian environment [1, 3-7]. Carbonate minerals are identified in Asian [8] and Saharan dust [9-11]. The imaginary index of refraction in the visible to mid-infrared wavelengths (vmir) of has been determined from a few of the many studies of carbonates spanning over 100 years [12-16]. The growing evidence for carbonates on Mars, the presence of carbonates in terrestrial aerosols, and the disagreement among the optical constants for these materials in the vmir has motivated a broader effort to determine the optical constants of carbonates [17-18]. The results of the application of the techniques described in [19] to estimate the optical constants of calcite will be presented. [1] Pollack et al. 1987 Icarus, 71, 203 [2] Fanale et at. 1992 in Mars, U. Arizona Press, 1135 [3] Lellouch et al. 2000 [4] Calvin et al. 1994 JGR. 99, 14659 [5] Bandfield et al. 2003, Science 301, 1084 [6] Ehlmann et al. 2008 Science, 322, 1828 [7] Palomba et al. 2009 Icarus 203, 58 [8] Jeong 2008 JGR., 113, D02208 [9] Glaccum and Prospero 1980 Mar. Geol., 37, 295 [10] Avila et al. 1997 JGR 102, 21,977 [11] Reid et al. 2003 JGR, 108, D19 [12] Nysander, 1909 Phys. Rev. 28, 291 [13] Merrit 1895 Phys. Rev. 2, 424 [14] Hellewege et al. 1970 Z. Phys., 232, 61 [15] Marra, et al. 2006 J. Quant. Spect. & Rad. Trans. 100, 250 [16] Ivalev and Papova 1972 Sov. Phys. J. 5, 91 [17] Roush, 2009 Lunar Planet. Sci. Conf 40, abstract 1080 [18] Roush 2010 Euro. Planet. Sci. Cong. abstract 341 [19] Roush et al. 2007 JGR, 112, E10003

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