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 |
|