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Volume 2019, Article ID 5203606, 1 page

Corrigendum to “Dry CO2–CO Fluid as an Important Potential Deep Earth Solvent”

1Thermodynamics of Minerals, Institute of Experimental Mineralogy RAS, Chernogolovka, Russia
2Institute of Physics of the Earth RAS, Moscow, Russia
3Geosciences, Mississippi State University, Mississippi State, MS, USA
4Diamond Mineralogy, Institute of Geology Ural Branch RAS, Syktyvkar, Russia

Correspondence should be addressed to A. G. Simakin;

Received 14 January 2019; Accepted 15 January 2019; Published 3 April 2019

Copyright © 2019 A. G. Simakin et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

In the article titled “Dry CO2–CO Fluid as an Important Potential Deep Earth Solvent” [1], the authors mistakenly presented molar fractions for CO2 instead of CO in the subsection “Fluid in Albite Glass” of the Experimental Results section. Therefore, the second sentence in the sixth paragraph of the subsection, “These calculations showed XN2 = 0.043, 0.048, 0.051 in the fluids where XCO2 = 0.154, 0.164, 0.062 respectively”, should be corrected to “These calculations showed , 0.048, and 0.051 in the fluids where , 0.164, and 0.062, respectively”.


  1. A. G. Simakin, T. P. Salova, R. I. Gabitov, and S. I. Isaenko, “Dry CO2–CO fluid as an important potential deep Earth solvent,” Geofluids, vol. 16, no. 5, pp. 1043–1057, 2016. View at Publisher · View at Google Scholar · View at Scopus