The alkali reserve of interstitial water at the sites of methane emission in the Sea of Okhotsk.

Tishchenko, P. Y., Pavlova, G. Y., Suess, Erwin, Nedashkovskii, A. P., Domeier, Bettina and Greinert, Jens (2001) The alkali reserve of interstitial water at the sites of methane emission in the Sea of Okhotsk. Geochemistry International, 39 (6). pp. 597-603.

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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 equationwas constructed connecting changes in alkalinity with variations of Ca2+, SO42- and NH4+ in interstitial solutions.

Document Type: Article
Keywords: Sea of Okhotsk, methane emission, alkali reserve
Research affiliation: OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
Refereed: Yes
Open Access Journal?: No
Publisher: Springer
Date Deposited: 19 Apr 2016 07:39
Last Modified: 19 Jan 2018 11:25
URI: https://oceanrep.geomar.de/id/eprint/32097

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