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EPR study of hydrocarbon generation potential of organic-rich domanik rocks

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dc.contributor.author Khasanova N.
dc.contributor.author Gabdrakhmanov D.
dc.contributor.author Kayukova G.
dc.contributor.author Mikhaylova A.
dc.contributor.author Morozov V.
dc.date.accessioned 2018-04-05T07:10:18Z
dc.date.available 2018-04-05T07:10:18Z
dc.date.issued 2017
dc.identifier.uri http://dspace.kpfu.ru/xmlui/handle/net/130353
dc.description.abstract © Kazan Federal University (KFU). The objects of investigation were samples of domanik formation rocks of Berezovskaya area of Romashkinskoye oil field. Content of Mn 2+ , SO 3 − , SO 2 − ions, vanadyl-ions and free radicals has been estimated with the X-band (9.43 GHz) electron paramagnetic resonance (EPR) spectroscopy. Composition of rock and extracted from it bitumen has been studied with methods of thermal analysis, X-ray-structural analysis and gas chromatography. Significant differences in mineralogical composition and content of organic matter were revealed in samples taken from adjacent intervals. Pyrolytic experiments have been conducted to simulate kerogen maturation and petroleum generation. The increasing number of free radicals was registered in all samples after pyrolysis in a hydrogen atmosphere at 350°C. A new organic free radical C350 was registered after pyrolysis. It is suggested that domanik source rocks have not fully realized their hydrocarbon generation potential.
dc.subject Domanik rocks
dc.subject EPR spectroscopy
dc.subject Generation potential
dc.subject Kerogen
dc.subject Pyrolysis
dc.title EPR study of hydrocarbon generation potential of organic-rich domanik rocks
dc.type Article
dc.relation.ispartofseries-issue 1
dc.relation.ispartofseries-volume 19
dc.collection Публикации сотрудников КФУ
dc.source.id SCOPUS-2017-19-1-SID85020934532


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  • Публикации сотрудников КФУ Scopus [24551]
    Коллекция содержит публикации сотрудников Казанского федерального (до 2010 года Казанского государственного) университета, проиндексированные в БД Scopus, начиная с 1970г.

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