THE ALKALI RESERVE OF INTERSTITIAL WATER AT THE SITES OF METHANE EMISSION IN THE SEA OF OKHOTSK

dc.contributor.author	Tishchenko P.Ya.
dc.contributor.author	Pavlova G.Yu.
dc.contributor.author	Nedashkovskii A.P.
dc.contributor.author	Suess E.
dc.contributor.author	Domeier B.
dc.contributor.author	Greinert I.
dc.date.accessioned	2021-02-25T05:13:21Z
dc.date.available	2021-02-25T05:13:21Z
dc.date.issued	2001
dc.description.abstract	The chemical composition (alkalinity, pH, NH4+, PO43-, Si, H2S, Cl-, Ca2+, and SO42-) of interstitial water was studied in the sediments of the Sea of Okhotsk at sites of methane emission. Variations in alkalinity were observed in the sediments from a typical seawater value (2.3 mM/kg) to 63 mM/kg. It is demonstrated that they are caused by the processes of sulfate reduction and methane generation. Based on the balance relationships, an equation was constructed connecting changes in alkalinity with variations of Ca2+, SO42+, and NH4+ in interstitial solutions.
dc.identifier	https://elibrary.ru/item.asp?id=13385833
dc.identifier.citation	Geochemistry International, 2001, 39, 6, 597-603
dc.identifier.issn	0016-7029
dc.identifier.uri	https://repository.geologyscience.ru/handle/123456789/25709
dc.title	THE ALKALI RESERVE OF INTERSTITIAL WATER AT THE SITES OF METHANE EMISSION IN THE SEA OF OKHOTSK
dc.type	Статья

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