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DOI10.1016/j.epsl.2019.115884
Space weathering by simulated micrometeorite bombardment on natural olivine and pyroxene: A coordinated IR and TEM study
Weber I.; Stojic A.N.; Morlok A.; Reitze M.P.; Markus K.; Hiesinger H.; Pavlov S.G.; Wirth R.; Schreiber A.; Sohn M.; Hübers H.-W.; Helbert J.
发表日期2020
ISSN0012821X
卷号530
英文摘要We studied space-weathering effects caused by micrometeorite bombardment simulated by pulsed intense infrared laser, generating ∼15 mJ per pulse in high vacuum. For our investigation, we selected a natural olivine (San Carlos olivine (Fo91)) and a natural pyroxene (Bamble orthopyroxene (En87)) as important rock forming minerals of the Earth upper mantle as well as key planetary minerals. Irradiated areas of powdered pressed samples were examined by optical reflection spectroscopy in a broad optical and infrared wavelength range (visible-, near-, and mid-infrared) and transmission electron microscopy to identify changes due to micrometeorite impacts. The present study aims to investigate especially the effects of micrometeorite bombardment on reflectance spectra in the mid-IR in preparation for future space missions, as well as for the MERTIS experiment onboard the BepiColombo mission. For both irradiated samples, we found a reduction in albedo and in the reflectance of characteristic Reststrahlen bands and an increase of the transparency feature. VIS and NIR spectra of both minerals show the typical darkening and reddening as described for other space-weathered samples. TEM studies revealed that space-weathered layers in olivine and pyroxene differ in their respective thickness, ∼450 nm in olivine, 100-250 nm in pyroxene, as well as in developed “nanostratigraphy” of laser-ablated material, like nanophase iron (npFe). In conclusion, our spectral and structural findings were compared to samples in which space weathering was caused by different processes. A comparison with these data demonstrates that there is no difference in optical reflectance spectroscopy, but a significant difference in the microstructure of minerals due to the weathering source in space, as there are solar wind and solar flares cause other structural and chemical changes as the bombardment with micrometeorites. © 2019 Elsevier B.V.
关键词MERTISmicrometeorite bombardmentnatural silicatesnpFespace weathering
英文关键词Experimental mineralogy; High resolution transmission electron microscopy; Infrared devices; Olivine; Pulsed lasers; Reflection; Silicates; Spacecraft instruments; Infrared wavelengths; MERTIS; micrometeorite bombardment; npFe; Optical reflection spectroscopies; Reflectance spectrum; Rock-forming minerals; Space weathering; Weathering; infrared spectroscopy; micrometeorite; olivine; pyroxene; silicate; transmission electron microscopy; upper mantle; weathering
语种英语
来源期刊Earth and Planetary Science Letters
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/202963
作者单位Westfälische Wilhelms Universität Münster, Institut für Planetologie, Wilhelm – Klemm Str. 10, Münster, 48149, Germany; German Aerospace Center (DLR), Institute of Optical Sensor Systems, Rutherfordstr. 2, Berlin, 12489, Germany; Helmholtz-Zentrum Potsdam, Deutsches Geoforschungszentrum (GFZ), Telegrafenberg, Potsdam, 14473, Germany; Hochschule Emden/Leer, Constantiaplatz 4, Emden, 26723, Germany; German Aerospace Center (DLR), Institute of Planetary Research, Rutherfordstr. 2, Berlin, 12489, Germany
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Weber I.,Stojic A.N.,Morlok A.,et al. Space weathering by simulated micrometeorite bombardment on natural olivine and pyroxene: A coordinated IR and TEM study[J],2020,530.
APA Weber I..,Stojic A.N..,Morlok A..,Reitze M.P..,Markus K..,...&Helbert J..(2020).Space weathering by simulated micrometeorite bombardment on natural olivine and pyroxene: A coordinated IR and TEM study.Earth and Planetary Science Letters,530.
MLA Weber I.,et al."Space weathering by simulated micrometeorite bombardment on natural olivine and pyroxene: A coordinated IR and TEM study".Earth and Planetary Science Letters 530(2020).
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