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Pore Space Change of Various Lithotypes of the Kerogen Domanic Rocks at Different Heating Rates

D.R. Gafurova1, D.V. Korost1, E.V. Kozlova2, A.G. Kalmykov1, G.A. Kalmykov1

Original article

DOI https://doi.org/10.18599/grs.19.3.17

255-263
rus.
eng.

open access

Under a Creative Commons license

The results of pore space changes as a result of heating Domanik Formation rock samples at different heating rates are shown. Microtomography method revealed that after heating in significant changes may arise, lens-like large pores can be formed, the number of pores and their coherence increase. It was found that changes in the pore space depend on the texture of rocks, the amount of organic matter and its degree of maturity, with all the factors must be considered together. Heating rate also influences the change in the pore space. The results should been considered in the retrieving of the natural reservoirs formation.

Domanik Formation, pore space, samples heating, kerogen cracking

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1Lomonosov Moscow State University, Moscow, Russia
2Skolkovo Institute of Science and Technology, Moscow, Russia

For citation:

Gafurova D.R., Korost D.V., Kozlova E.V., Kalmykov A.G., Kalmykov G.A. Pore Space Change of Various Lithotypes of the Kerogen Domanic Rocks at Different Heating Rates. Georesursy = Georesources. 2017. V. 19. No. 3. Part 2. Pp. 255-263. DOI: https://doi.org/10.18599/grs.19.3.17