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Spectroscopical study of natural nanostructured carbonaceous material shungite

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dc.contributor.author Konchits, A.A.
dc.contributor.author Shanina, B.D.
dc.contributor.author Valakh, M.Ya.
dc.contributor.author Yanchuk, I.B.
dc.contributor.author Yukhymchuk, V.O.
dc.contributor.author Yefanov, A.V.
dc.contributor.author Krasnovyd, S.V.
dc.contributor.author Skoryk, M.A.
dc.date.accessioned 2017-06-12T08:17:05Z
dc.date.available 2017-06-12T08:17:05Z
dc.date.issued 2014
dc.identifier.citation Spectroscopical study of natural nanostructured carbonaceous material shungite / A.A. Konchits, B.D. Shanina, M.Ya. Valakh, I.B. Yanchuk, V.O. Yukhymchuk, A.V. Yefanov, S.V. Krasnovyd, M.A. Skoryk // Functional Materials. — 2014. — Т. 21, № 3. — С. 260-265. — Бібліогр.: 19 назв. — англ. uk_UA
dc.identifier.issn 1027-5495
dc.identifier.other DOI: dx.doi.org/10.15407/fm21.03.260
dc.identifier.uri http://dspace.nbuv.gov.ua/handle/123456789/120499
dc.description.abstract The correlation between morphology, local structure and magnetic properties of the different origin shungite material with nanocarbon content 25-40 wt. % was studied by SEM, EPR, and Raman scattering methods. It was established that structure of the shungite samples is formed by micron size agglomerations of carbon and silicon dioxide clusters with impregnations of pyrite (FeS₂), iron oxide and aluminium oxide particles. It was found from the Raman data that nanocarbon fraction is formed from sp²-hybridized well ordered carbon clusters, size of which increases from 9 nm up to 12 nm after annealing of the samples. It was found for the first time that origin of L3 and L4 EPR lines is due to oxy-deficiency centers in the silicon dioxide clusters. uk_UA
dc.language.iso en uk_UA
dc.publisher НТК «Інститут монокристалів» НАН України uk_UA
dc.relation.ispartof Functional Materials
dc.subject Characterization and properties uk_UA
dc.title Spectroscopical study of natural nanostructured carbonaceous material shungite uk_UA
dc.type Article uk_UA
dc.status published earlier uk_UA


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