Spatial variations of methane distribution in marine environment and its fluxes at the water–atmosphere interface in the western Sea of Okhotsk

• Published in: Water resources Vol. 44; no. 4; pp. 662 - 672
• Main Authors: Mishukova, G. I., Shakirov, R. B.
• Format: Journal Article
• Language: English
• Published: Moscow Pleiades Publishing 01.07.2017; Springer Nature B.V
• Subjects: Anomalies; Aquatic Pollution; Atmosphere; Bottom sediments; Composition; Continental shelves; Cruises; Distribution; Earth and Environmental Science; Earth Sciences; Faults; Fluxes; Gases; Geochemistry; Geological faults; Hydrocarbons; Hydrogeology; Hydrology/Water Resources; Interaction between Continental Waters and the Environment; Marine environment; Mathematical analysis; Methane; Natural gas; Oil; Seawater; Sediment; Sediments; Spatial analysis; Spatial distribution; Spatial variations; Surface water; Waste Water Technology; Water; Water Management; Water Pollution Control; Sea of Okhotsk; methane; methane flux; oil and gas fields; distribution; hydrocarbon gases; tectonic structures
• ISSN: 0097-8078; 1608-344X
• DOI: 10.1134/S0097807817040133

Data of integrated gas-geochemical studies in the 45 cruise of the R/V Akademik M.A. Lavrent’ev in July 2008 were used to study the spatial distribution of methane in the surface seawater layer, the distribution and qualitative composition of hydrocarbon gases in bottom sediments of the northwestern continental shelf, northeastern slope of Sakhalin Island, and Deryugin depression in the Sea of Okhotsk. The specific features of the methane anomalies that form in this case are considered. Tectonic faults and the distribution of oil-and-gas-bearing structures are the main factors governing the formation of hydrocarbon gas fluxes in the study area. The surface water in the entire examined area was found to be oversaturated with methane. A developed model was used to calculated methane fluxes at the water–atmosphere interface and to identify areas with maximal fluxes (up to 324 mol/(km 2 day).