Abstract
Bulk of the main part of the Chelyabinsk meteorite (ordinary chondrite, LL5) for the presence of nanometer pores therein is investigated by means of the positron annihilation lifetime spectroscopy (PALS). In addition, its phase composition is studied with a help of the transmission Mossbauer spectroscopy (TMS). These results are refined by means of the powder X-ray diffraction (XRD). The obtained data demonstrate an absence of the nanometer pores in the meteorite. TMS data show that the meteorite consists of mineral phases (olivine and pyroxene), which are rather typical for the ordinary chondrites. Iron is present in sulfide and nickel forms. Possible applications of nuclear-physics methods for analysis of an origin of meteorites and evolution of the Solar system are discussed.
Similar content being viewed by others
References
E. M. Galimov, V. P. Kolotov, M. A. Nazarov, et al., Geochem. Int. 51, 522 (2013). https://doi.org/10.1134/S0016702913070100
The Meteoritical Society. https://meteoritical.org
D. Giebel, J. Kansy, Mater. Sci. Forum. 666, 138 (2011).
J. G. Stevens, Mössbauer Mineral Handbook (Mössbauer Effect Data Center, 2005).
The International Centre for Diffraction Data. http://www.icdd.com
Acknowledgment
Experimental part of this research was performed using facilities of the center KAMIKS (http://kamiks.itep.ru/) of the NRC “Kurchatov Insutute”—ITEP.
Author information
Authors and Affiliations
Corresponding author
Ethics declarations
The authors declare that they have no conflicts of interest.
Additional information
Russian Text © The Author(s), 2018, published in Yadernaya Fizika i Inzhiniring, 2018, Vol. 9, No. 5, pp. 481–487.
Rights and permissions
About this article
Cite this article
Bokov, A.V., Stepanov, S.V., Byakov, V.M. et al. Investigation of the Meteorite “Chelyabinsk” by Means of the Positron Annihilation Lifetime and Transmission Mössbauer Spectroscopies. Phys. Atom. Nuclei 82, 1552–1557 (2019). https://doi.org/10.1134/S1063778819120020
Received:
Revised:
Accepted:
Published:
Issue Date:
DOI: https://doi.org/10.1134/S1063778819120020