Ongoing methane discharge at well site 22/4b (North Sea)and discovery of a spiral vortex bubble plume motion.

Schneider von Deimling, Jens, Linke, Peter , Schmidt, Mark and Rehder, Gregor (2015) Ongoing methane discharge at well site 22/4b (North Sea)and discovery of a spiral vortex bubble plume motion. Open Access Marine and Petroleum Geology, 68 . pp. 718-730. DOI 10.1016/j.marpetgeo.2015.07.026.

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Supplementary data:



• Mega ebullition of biogenic methane from an abandoned offshore gas well, North Sea.
• Evidence for midwater bubble plume intrusion, fallback, and short-circuiting of the plume.
• Effective trapping of seabed released methane underneath the thermocline.
• First observation of a spiral vortex methane plume and marginal turbulences.
• Megaplumes appear less efficient in terms of vertical methane transport than previously thought.


First direct evidence for ongoing gas seepage activity on the abandoned well site 22/4b (Northern North Sea, 57°55′ N, 01°38′ E) and discovery of neighboring seepage activity is provided from observations since 2005. A manned submersible dive in 2006 discovered several extraordinary intense seepage sites within a 60 m wide and 20 m deep crater cut into the flat 96 m deep seafloor. Capture and (isotope) chemical analyses of the gas bubbles near the seafloor revealed in situ concentrations of methane between 88 and 90%Vol. with δ13C–CH4 values around −74‰ VPDB, indicating a biogenic origin. Bulk methane concentrations throughout the water column were assessed by 120 Niskin water samples showing up to 400.000 nM CH4 in the crater at depth. In contrast, concentrations above the thermocline were orders of magnitude lower, with a median value of 20 nM. A dye tracer injection into the gas seeps revealed upwelling bubble and water motion with gas plume rise velocities up to ∼1 ms−1 (determined near the seabed). However, the dissolved dye did not pass the thermocline, but returned down to the seabed. Measurements of direct bubble-mediated atmospheric flux revealed low values of 0.7 ± 0.3 kty−1, much less than current state-of-the-art bubble dissolution models would predict for such a strong and upwelling in situ gas bubble flux at shallow water depths (i.e. ∼100 m). Acoustic multibeam water column imaging data indicate a pronounced 200 m lateral intrusion at the thermocline together with high methane concentration at this layer. A partly downward-orientated bubble plume motion is also visible in the acoustic data with potential short-circuiting in accordance to the dye experiment. This observation could partly explain the observed trapping of most of the released gas below the well-established thermocline in the North Sea. Moreover, 3D analyses of the multibeam water column data reveal that the upwelling plume transforms into a spiral expanding vortex while rising through the water column. Such a spiral vortex motion has never been reported before for marine gas seepage and might represent an important process with strong implication on plume dynamics, dissolution behavior, gas escape to the atmosphere, and is considered very important for respective modeling approaches.

Document Type: Article
Funder compliance: info:eu-repo/grantAgreement/EC/FP7/265847
Additional Information: WOS:000367631900003
Keywords: Mega gas blowout 22/4b, North Sea, Methane seepage, Multibeam, Spiral vortex, Turbulence, Trapping, Thermocline, Flare imaging, RV Alkor, AL259, AL290, RV Meteor, RV Celtic Explorer, ROV KIEL 6000, JAGO, CE12010
Research affiliation: OceanRep > The Future Ocean - Cluster of Excellence > FO-R05
OceanRep > The Future Ocean - Cluster of Excellence > FO-R06
OceanRep > GEOMAR > FB2 Marine Biogeochemistry > FB2-MG Marine Geosystems
OceanRep > The Future Ocean - Cluster of Excellence
OceanRep > GEOMAR > FB4 Dynamics of the Ocean Floor > FB4-GDY Marine Geodynamics
Refereed: Yes
Open Access Journal?: No
DOI etc.: 10.1016/j.marpetgeo.2015.07.026
ISSN: 0264-8172
Projects: GEOTECHNOLOGIEN, Eurofleets, ECO2, SUGAR II, Future Ocean
Date Deposited: 19 Dec 2013 12:15
Last Modified: 23 Nov 2020 13:25

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