Flow of products of thermal decomposition of oil shale through porous skeleton

A. G. Knyazeva, A. L. Maslov

Research output: Chapter in Book/Report/Conference proceedingConference contribution

Abstract

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.

Original languageEnglish
Title of host publicationAdvanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016: Proceedings of the International Conference on Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016
PublisherAmerican Institute of Physics Inc.
Volume1783
ISBN (Electronic)9780735414457
DOIs
Publication statusPublished - 10 Nov 2016
EventInternational Conference on Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016 - Tomsk, Russian Federation
Duration: 19 Sep 201623 Sep 2016

Conference

ConferenceInternational Conference on Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016
CountryRussian Federation
CityTomsk
Period19.9.1623.9.16

    Fingerprint

ASJC Scopus subject areas

  • Physics and Astronomy(all)

Cite this

Knyazeva, A. G., & Maslov, A. L. (2016). Flow of products of thermal decomposition of oil shale through porous skeleton. In Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016: Proceedings of the International Conference on Advanced Materials with Hierarchical Structure for New Technologies and Reliable Structures 2016 (Vol. 1783). [020093] American Institute of Physics Inc.. https://doi.org/10.1063/1.4966386