INFLUENCE OF OXIDABILITY OF CARBONIFEROUS COALS FROM THE DOBRUDJA FOREDEEP ON VITRINITE REFLECTANCE

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dc.contributor.author Ivanova A.V.
dc.contributor.author Zaitseva L.B.
dc.date.accessioned 2025-02-16T08:50:37Z
dc.date.available 2025-02-16T08:50:37Z
dc.date.issued 2006
dc.identifier https://www.elibrary.ru/item.asp?id=27850073
dc.identifier.citation Lithology and Mineral Resources, 2006, 41, 5, 435-439
dc.identifier.issn 0024-4902
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/48030
dc.description.abstract Importance of the study of the influence of coal oxidability on vitrinite reflectance (VR) as a criterion of the quality of coals and indicator of paleogeothermal regime is shown. Overview of relevant concepts demonstrates that this issue remains debatable. Carboniferous coals of the Dobrudja foredeep, which belong to the class of helitolites in terms of their microcomponent composition, were studied. They were subjected to oxidation during storage outdoors. Consequently, the VR value of high volatile bituminous (long-flame and gas ranks, according to the Russian classification) coals decreased, but this parameter remained virtually unaltered for medium volatile bituminous (fat) coals. Bulgarian researchers obtained similar results for Carboniferous coals of the Dobrudja basin represented by helitolites and mixtohumolites. In our opinion, the VR decrease in the course of coal oxidation is caused by decrease in the condensation and density of aromatic structures and increase in the share of nonaromatic carbon atoms. © Pleiades Publishing, Inc. 2006.
dc.subject Carboniferous
dc.title INFLUENCE OF OXIDABILITY OF CARBONIFEROUS COALS FROM THE DOBRUDJA FOREDEEP ON VITRINITE REFLECTANCE
dc.type Статья
dc.identifier.doi 10.1134/S002449020605004X
dc.subject.age Paleozoic::Carboniferous
dc.subject.age Палеозой::Каменноугольная


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