Flow of Products of Thermal Decomposition of Oil Shale Through Porous Skeleton; AIP Conference Proceedings; Vol. 1783 : Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016

Bibliografische gegevens
Parent link:AIP Conference Proceedings
Vol. 1783 : Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016.— 2016.— [020093, 4 p.]
Hoofdauteur: Knyazeva A. G. Anna Georgievna
Coauteur: Национальный исследовательский Томский политехнический университет (ТПУ) Институт физики высоких технологий (ИФВТ) Кафедра материаловедения в машиностроении (ММС)
Andere auteurs: Maslov А. L.
Samenvatting:Title screen
Oil shale is sedimentary rock formed by the accumulation of pelagic sediments, minerals and their further transformation. Experimental investigation of shale decomposition is very complex and expensive. The model of underground oil shale retorting is formulated in this paper. Model takes into account the reactions in solid phase and in fluid, mass and heat exchange, gaseous product flow in pores. Example of the numerical solution of the developed system of equations for the particular problem is shown.
Режим доступа: по договору с организацией-держателем ресурса
Taal:Engels
Gepubliceerd in: 2016
Onderwerpen:
Online toegang:http://dx.doi.org/10.1063/1.4966386
Formaat: Elektronisch Hoofdstuk
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=652678
Omschrijving
Samenvatting:Title screen
Oil shale is sedimentary rock formed by the accumulation of pelagic sediments, minerals and their further transformation. Experimental investigation of shale decomposition is very complex and expensive. The model of underground oil shale retorting is formulated in this paper. Model takes into account the reactions in solid phase and in fluid, mass and heat exchange, gaseous product flow in pores. Example of the numerical solution of the developed system of equations for the particular problem is shown.
Режим доступа: по договору с организацией-держателем ресурса
DOI:10.1063/1.4966386