MNO2/MN2+ SYSTEM AS THE POTENTIAL-GOVERNING SYSTEM IN EH MEASUREMENTS ON STRONGLY OXIDIZED PELAGIC BOTTOM SEDIMENTS

dc.contributor.author	Pisarevskiy A.M.
dc.contributor.author	Tishchenko P.Y.
dc.contributor.author	Gramm-Osipov L.M.
dc.contributor.author	Nikolayev Y.I.
dc.date.accessioned	2020-10-11T11:11:58Z
dc.date.available	2020-10-11T11:11:58Z
dc.date.issued	1989
dc.identifier	https://elibrary.ru/item.asp?id=31166210
dc.identifier.citation	Transactions (Doklady) of the USSR Academy of Sciences. Earth Science Sections, 1989, , 3, 212-214
dc.identifier.issn	0891-5571
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/17972
dc.description.abstract	Study of the redox state of pelagic bottom sediments (red clays) is important to an understanding of the evolution of iron-manganese nodules in the ocean. There is now a large body of direct potentiometric measurements of these sediments, made with platinum indicator electrodes. But there has been no discussion of the nature of the potential-governing system or of the reason for the difficulty of measurements (slow attainment of steady-state potential, and poor reproducibility of results). In the present paper the authors describe investigations made during the 8th cruise of the R/V Akademik Aleksandr Vinogradov in the Central Pacific Ocean during 1986.
dc.title	MNO2/MN2+ SYSTEM AS THE POTENTIAL-GOVERNING SYSTEM IN EH MEASUREMENTS ON STRONGLY OXIDIZED PELAGIC BOTTOM SEDIMENTS
dc.type	Статья

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