Pogodaeva T.V.

Graduated from Irkutsk Polytechnic Institute (1986), specialization "physical and chemical methods for the study of systems and processes".
PhD in Geological and Mineralogical Sciences.
Senior Researcher of the Laboratory of Hydrochemistry and Atmospheric Chemistry, Limnological Institute SB RAS.
Area of scientific interests: geology, geochemistry, bottom sediments, interstitial water, chemical composition, Baikal Lake.
Author of 43 publications, 2 patents.

New methods and technologies

Section editor – PhD in geology and mineralogy Prischepa O.M.

Article # 8_2017	submitted on 12/19/2016 displayed on website on 03/13/2017
21 p.	Krylov A.A., Khlystov O.M., Hachikubo A., Minami H., Pogodaeva T.V., Zemskaya T.I., Krzhizhanovskaya M.G., Muzafarova L.E., Atanyazov R.Zh.
pdf	Mechanism of authigenic rhodochrosite formation in the near-bottom sediments of the Saint-Petersburg-2 gas-hydrate-bearing structure (central basin of the Baikal Lake)
	Gas-hydrate-bearing fluid discharge areas are generally marked with authigenic carbonates. The latter can be formed in result of methane oxidation/generation, destruction of organic matter or the mixing of these processes. In most cases, the history of carbonates generation can be steadily reconstructed based on the isotopic data. This article discussed the mechanism of rhodochrosite crystallization, rhodochrosite which was discovered for the first time in the near-bottom sediments of the Baikal Lake gas-hydrate-bearing structures (the St. Petersburg-2 structure). The rhodochrosite formation is related to the cause of its formation were the microbial degradation of organic matter in the zone of methane generation. Keywords: authigenic carbonates, rhodochrosite, the methane, gas-hydrate-bearing structure, Lake Baikal.
article citation	Krylov A.A., Khlystov O.M., Hachikubo A., Minami H., Pogodaeva T.V., Zemskaya T.I., Krzhizhanovskaya M.G., Muzafarova L.E., Atanyazov R.Zh. Mekhanizm formirovaniya autigennogo rodokhrozita v pripoverkhnostnykh osadkakh gazogidratonosnoy struktury Sankt-Peterburg-2 v tsentral'noy kotlovine ozera Baykal [Mechanism of authigenic rhodochrosite formation in the near-bottom sediments of the Saint-Petersburg-2 gas-hydrate-bearing structure (central basin of the Baikal Lake)]. Neftegazovaya Geologiya. Teoriya I Praktika, 2017, vol. 12, no. 1, available at: http://www.ngtp.ru/rub/12/8_2017.pdf
DOI	https://doi.org/10.17353/2070-5379/8_2017

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