The material balance of organic matter of Domanic shale formation after thermal treatment

dc.contributor.author	Onishchenko Y.
dc.contributor.author	Vakhin A.
dc.contributor.author	Gareev B.
dc.contributor.author	Batalin G.
dc.contributor.author	Morozov V.
dc.contributor.author	Eskin A.
dc.date.accessioned	2020-01-15T21:46:19Z
dc.date.available	2020-01-15T21:46:19Z
dc.date.issued	2019
dc.identifier.issn	1091-6466
dc.identifier.uri	https://dspace.kpfu.ru/xmlui/handle/net/155797
dc.description.abstract	© 2019, © 2019 Taylor & Francis Group, LLC. In this paper, we discuss the amount of generated gaseous and liquid hydrocarbons as a product of artificial maturation of organic matters of Domanic black shale. The material balance of organic matter for initial rock sample and after thermal treatment at 300 and 500 °С were estimated. The amount of generated liquid hydrocarbon was minimum at 500 °С. As a result of kerogen destruction, no asphaltenes were observed during generation of liquid hydrocarbons. Based on the results of elemental analysis, Van Krevelen diagram was plotted.
dc.relation.ispartofseries	Petroleum Science and Technology
dc.subject	Composition; Domanic rock; maturity; organic matter
dc.subject	thermal analysis
dc.subject	Volga-Ural basin
dc.title	The material balance of organic matter of Domanic shale formation after thermal treatment
dc.type	Article
dc.relation.ispartofseries-issue	7
dc.relation.ispartofseries-volume	37
dc.collection	Публикации сотрудников КФУ
dc.relation.startpage	756
dc.source.id	SCOPUS10916466-2019-37-7-SID85060331445

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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.