Počet záznamů: 1  

Simulation of Space Weathering on Asteroid Spectra through Hydrogen Ion Irradiation of Meteorites

  1. 1.
    SYSNO ASEP0571244
    Druh ASEPJ - Článek v odborném periodiku
    Zařazení RIVJ - Článek v odborném periodiku
    Poddruh JČlánek ve WOS
    NázevSimulation of Space Weathering on Asteroid Spectra through Hydrogen Ion Irradiation of Meteorites
    Tvůrce(i) Palamakumbure, L. (FI)
    Mizohata, K. (FI)
    Flanderová, Kateřina (GLU-S) ORCID, SAI
    Korda, D. (FI)
    Penttilä, A. (FI)
    Kohout, Tomáš (GLU-S) RID, SAI, ORCID
    Číslo článku72
    Zdroj.dok.The Planetary Science Journal. - : American Astronomical Society
    Roč. 4, č. 4 (2023)
    Poč.str.10 s.
    Jazyk dok.eng - angličtina
    Země vyd.US - Spojené státy americké
    Klíč. slovaSpace weathering ; meteorite ; chondrite ; reflectance spectra ; solar wind ; Bjurböle ; Avahandava ; Luotolax
    Obor OECDAstronomy (including astrophysics,space science)
    Způsob publikováníOpen access
    Institucionální podporaGLU-S - RVO:67985831
    UT WOS000976724200001
    EID SCOPUS85179793323
    DOI10.3847/PSJ/acc848
    AnotaceSpace weathering can be defined as the combination of physical and chemical changes that occur in material exposed to an interplanetary environment on the surface of airless bodies. This process results in alterations in material spectroscopic features. Eventually, it can lead to misinterpretation of remotely sensed data in the visible–near-infrared wavelength range. This study simulates the solar wind effect on asteroid spectra through low-energy 1 keV H+ irradiation of meteorite pressed-powder samples under three fluences, 2 × 1017, 5 × 1017, and 1 × 1018 H+ cm−2, and evaluates changes associated with reflectance spectra. The meteorites subjected to the study are Bjurböle (L/LL4), Avanhandava (H4), and Luotolax (howardite). The most prominent changes in all three meteorites are (1) a decrease of 550 nm reflectance, (2) reddening in the 1 μm region, and (3) a monotonous decrease in absorption band strengths in Bjurböle. No significant changes were observed in the 2 μm region. The results imply that at short timescales (102–103 yr), radiation damage as amorphization and vesicle formation caused by low-energy solar wind is the dominant space weathering factor in all three meteorite compositions, causing spectral changes predominantly in the 1 μm region.
    PracovištěGeologický ústav
    KontaktJana Popelková, popelkova@gli.cas.cz, Sabina Janíčková, Tel.: 233 087 272
    Rok sběru2024
    Elektronická adresahttps://iopscience.iop.org/article/10.3847/PSJ/acc848
Počet záznamů: 1  

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