Multispectral polarimetry as a tool to investigate texture and chemistry of lunar regolith particles |
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Authors: | Yuriy Shkuratov Nikolay Opanasenko Yevgen Grynko Viktor Korokhin Gorden Videen Urs Mall |
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Affiliation: | a Astronomical Institute of V.N. Karazin Kharkov National University, 35 Sumskaya St., Kharkov 61022, Ukraine b Institute of Low Temperature Science, Hokkaido University, Kita-ku North 19 West 8, Sapporo 060-0819, Japan c Max-Planck Institute for Solar System Research, Max-Planck St. 2, 37191 Katlenburg-Lindau, Germany d Department of Geological Sciences, Brown University, Providence, RI 02912, USA e Space Science Institute, 4750 Walnut St., Suite 205, Boulder, CO 80301, USA f Astronomical Institute, University of Amsterdam, Kruislaan 403, 1098 SJ Amsterdam, The Netherlands |
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Abstract: | ![]() We report results of telescope polarimetric imaging of the Moon with a CCD LineScan Camera at large phase angles, near 88°. This allows measurements of the polarization degree with an absolute accuracy better than 0.3% and detection of features with polarization contrast as small as 0.1%. The measurements are carried out in two spectral bands centered near 0.65 and 0.42 μm. We suggest characterizing the lunar regolith with the parameter a(Pmax)A, where Pmax,A, and a are the degree of maximum polarization, albedo, and the parameter describing the linear regression of the correlation Pmax-A. The parameter bears significant information on the particle characteristic size and packing density of the lunar regolith. We also suggest characterizing the lunar regolith with color-ratio images obtained with a polarization filter at large phase angles. We here consider the color-ratios C||(0.65/0.42 μm) and C⊥(0.65/0.42 μm). Using light scattering model calculations we show that the color-ratio images obtained with a polarization filter at large phase angles suggest a new tool to study the lunar surface. In particular, it turns out that the color-ratios C||(0.65/0.42 μm) and C⊥(0.65/0.42 μm) are sensitive to somewhat different thicknesses of the surfaces of regolith particles. We consider the applicability of the Hubble Space Telescope, the Very Large Telescope (ESO), and a spacecraft on a lunar polar orbit for polarimetric observations of the lunar surface. |
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Keywords: | Polarimetry Moon, surface Regolith |
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