Astronomy and Astrophysics; Space and Planetary Science
Abstract :
[en] We have synthesized and analyzed by mid-infrared reflectance spectroscopy silicate glasses that are representative for the glasses on the surface of Mercury. The glass compositions are based on high-pressure laboratory experiments and the resulting compositions of the glass phase. The spectra are of interest for investigating the surface of Mercury using the MERTIS (Mercury Radiometer and Thermal Infrared Spectrometer) instrument on board of the ESA/JAXA BepiColombo mission. Both powdered fractions and polished blocks have been analyzed. Powdered size fractions of 0–25 μm, 25-63 μm, 63-125 μm, and 125–250 μm were measured in reflectance in the thermal infrared (2–20 μm). Spectra for powdered bulk glasses (1.6 wt% - 19.0 wt% MgO) show a single, dominating Reststrahlenband (RB, 9.3–9.8 μm), a Christiansen Feature (CF; 7.6 μm - 8.1 μm), and a size dependent Transparency Feature (TF; 11.6–11.9 μm). Micro-FTIR analyses of polished blocks of glasses (3.4–26.5 wt% MgO) have characteristic bands at 7.8–8.2 μm (CF), and 9.3–9.9 μm (RB). Only few olivine crystalline features were observed. Spectral features correlate with compositional characteristics, e.g. SiO2 content or SCFM (SiO2/(SiO2 + CaO + FeO + MgO) index. The strongest correlation between band features CF and the strong RB are with Mg/Si. No simple mixture of glass spectra from this study is able to reproduce the entire ground based spectrum of the surface of Mercury. However, Mg-rich glasses reproduce identified features at 8.5 μm, 9.9 μm and 12.4 μm.
Disciplines :
Earth sciences & physical geography
Author, co-author :
Morlok, Andreas; Institut für Planetologie, Westfälische Wilhelms-Universität Universität Münster, Germany
Renggli, Christian; Institut für Mineralogie, Westfälische Wilhelms-Universität Universität Münster, Münster, Germany
Charlier, Bernard ; Université de Liège - ULiège > Département de géologie > Pétrologie, géochimie endogènes et pétrophysique
Reitze, Maximilian P.; Institut für Planetologie, Westfälische Wilhelms-Universität Universität Münster, Germany
Klemme, Stephan; Institut für Mineralogie, Westfälische Wilhelms-Universität Universität Münster, Münster, Germany
Namur, Olivier; Department of Earth and Environmental Sciences, KU Leuven, Leuven, Belgium
Royal Society SNF - Schweizerischer Nationalfonds zur Förderung der wissenschaftlichen Forschung F.R.S.-FNRS - Fonds de la Recherche Scientifique DLR - Deutsches Zentrum für Luft- und Raumfahrt STFC - Science and Technology Facilities Council
Funding text :
C.R. was supported by a SNF postdoctoral fellowship.K.H.J. was supported by the UK Science and Technology Facilities Council (ST/M001253/1) and the Royal Society (RS/UF140190).This work was supported by DLR grant 50 QW 1302/1701 in the framework of the BepiColombo mission (A.M.,I.W.,A.N.S.,M.P.R., K.E.B., J.H.)B.C. is a Research Associate of the Belgian Fund for Scientific Research-FNRS and acknowledges support by the FNRS Incentive Grant 31,230,854.
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