Methane in waters and bottom sediments of the North (Severnaya) Dvina mouth area in 2004-2006

• Main Authors: Gar'kusha, D N, Fedorov, YuA, Khromov, M I
• Format: Other/Unknown Material
• Language: English
• Published: PANGAEA 2010
• Subjects: Aisberg-2-2004-1; Aisberg-2-2004-13; Aisberg-2-2004A-1; Aisberg-2-2004A-10; Aisberg-2-2004A-11; Aisberg-2-2004A-13; Aisberg-2-2004A-2; Aisberg-2-2004A-3; Aisberg-2-2004A-4; Aisberg-2-2004A-5; Aisberg-2-2004A-6; Aisberg-2-2004A-7; Aisberg-2-2004A-8; Aisberg-2-2004A-9; Aisberg-2-2004B-1; Aisberg-2-2004B-10; Aisberg-2-2004B-11; Aisberg-2-2004B-12; Aisberg-2-2004B-13; Aisberg-2-2004B-3; Aisberg-2-2004B-5; Aisberg-2-2004B-7; Aisberg-2-2004B-9; Aisberg-2-2005-1; Aisberg-2-2005-10; Aisberg-2-2005-13; Aisberg-2-2005-3; Aisberg-2-2005-4; Aisberg-2-2005-5; Aisberg-2-2005-6; Aisberg-2-2005-7; Aisberg-2-2005-8; Aisberg-2-2005-9; Aisberg-2-2006-1; Aisberg-2-2006-10; Aisberg-2-2006-13; Aisberg-2-2006-9; Aisberg-2-NDM-1; Aisberg-2-NDM-10; Aisberg-2-NDM-13; Aisberg-2-NDM-14-1; Aisberg-2-NDM-14-10; Aisberg-2-NDM-14-11; Aisberg-2-NDM-14-12; Aisberg-2-NDM-14-13; Aisberg-2-NDM-14-2; Aisberg-2-NDM-14-3; Aisberg-2-NDM-14-4; Aisberg-2-NDM-14-5; Aisberg-2-NDM-14-6; Severnaya Dvina; dvina
• Online Access: https://doi.pangaea.de/10.1594/PANGAEA.763838; https://doi.org/10.1594/PANGAEA.763838

The mouth area of the North (Severnaya) Dvina River is characterized by a high concentrations of methane in water (from 1.0 to 165.4 µl/l) and bottom sediments (from 14 to 65000 µl/kg), being quite comparable to productive mouth areas of rivers from the temperate zone. Maximum methane concentrations in water and sediments were registered in the delta in segments of channels and branches with low rates of tidal and runoff currents, where domestic and industrial wastewaters are supplied. In the riverine and marine water mixing zone with its upper boundary, locating far into the delta and moving depending on a phase of the tidal cycle, decrease of methane concentration with salinity increase was observed. The prevailing role in formation of the methane concentration level in water of the mouth area pertains to bottom sediments, which is indicated by close correlation between gas concentrations in these two media. Existence of periodicity in variations of methane concentration in river water downstream caused by tidal effects was found.