And Vestnesa is home to a very
large gas hydrate system.
The numerical simulations of the seafloor also showed that the pockmarks in Nyegga are likely associated with this phenomenon because they are located right in the area of
the largest gas hydrate dissociation event at the end of the Ice Age.
Not exact matches
They occurred over a very short time interval immediately following onset of Cretaceous global warming, suggesting that the warming destabilized
gas hydrates and released a
large burb of methane.
Suess now attributes this buoyancy, not a typical
hydrate characteristic, to
large bubbles of
gas that accumulate in the top layers of the seafloor ooze before freezing.
A team of researchers from the GEOMAR Helmholtz Centre for Ocean Research Kiel together with colleagues from Bergen, Oslo and Tromsø (Norway), have now discovered that
large - scale sedimentation caused by melting of glaciers in a region off Norway has played a greater role in
gas hydrate dissociation than warming ocean waters.
Despite the rising sea level and therefore increasing pressure, the simulation showed that towards the end of the ice age
large amounts of
gas hydrate became unstable and the released
gas escaped through the sediment to the seawater.
Carozza et al (2011) find that natural global warming occurred in 2 stages: First, global warming of 3 ° to 9 ° C accompanied by a
large bolus of organic carbon released to the atmosphere through the burning of terrestrial biomass (Kurtz et al, 2003) over approximately a 50 - year period; second, a catastrophic release of methane
hydrate from sediment, followed by the oxidation of a part of this methane
gas in the water column and the escape of the remaining CH4 to the atmosphere over a 50 - year period.
Proposed hypothe - ses include (i) biogenic methane from
gas hydrate dissociation (Dickens et al., 1995,1997); (ii) CO2 from extensive oxidation terrestrial organic carbon (Kurtz et al., 2003; Deconto et al., 2012); (iii) thermogenic methane derived from emplacement of a
large 25 igneous province (LIP) in the North Atlantic (Svensen et al., 2010) or combinations of such sources (Sluijs et al., 2007; Panchuk et al., 2008).
Shale
gas and coal bed methane and maybe methane
hydrates are
large resources.
Carozza et al (2011) find that natural global warming occurred in 2 stages: First, global warming of 3 ° to 9 ° C accompanied by a
large bolus of organic carbon released to the atmosphere through the burning of terrestrial biomass (Kurtz et al, 2003) over approximately a 50 - year period; second, a catastrophic release of methane
hydrate from sediment, followed by the oxidation of a part of this methane
gas in the water column and the escape of the remaining CH4 to the atmosphere over a 50 - year period.
In Siberian permafrost,
large deposits of methane
gas are trapped in ice, forming what is called a
gas hydrate.
It was developed by scientists at CAGE — Centre for Arctic
Gas Hydrate Environment and Climate, and shows that seafloor off Western Svalbard was covered by a
large ice sheet during the last glaciation.
Large amounts of methane are stored in seafloor sediments as
gas hydrate, and as these melt the
gas is released into the water column.
Furthermore, there are thought to be
large amounts of non-conventional oil (e.g., heavy oil, tars sands, shales) and
gas (e.g., methane
hydrates).
The lakes may also be storing
large volumes of the potent greenhouse
gas methane, frozen in a form called methane
hydrates.
Hornbach, Matthew J., Saffer, D.M., Holbrook, W. S., Van Avendonk, H.J.A., Gorman, A., «3D seismic imaging of the Blake Ridge methane
hydrate province: evidence for
large concentrated zones of
gas hydrate and morphologically - driven advection,» Journal of Geophysical Research (Solid Earth), 2008.
Holbrook, W.S., Lizarralde, D., Pecher, I.A., Gorman, A.R., Hackwith, K.L., Hornbach, M.J., Saffer, D.M., «Escape of methane
gas through sediment waves in a
large methane
hydrate province.»
Tim Collett, USGS senior scientist, said: «The discovery of what we believe to be several of the
largest and most concentrated
gas hydrate accumulations yet found in the world will yield the geologic and engineering data needed to better understand the geologic controls on the occurrence of
gas hydrate in nature and to assess the technologies needed to safely produce
gas hydrates.»
The work being done by the USGS is intended to not only discover where
large concentrations of methane
gas hydrates are located, but also to determine the best method for safely extracting the methane trapped in the
hydrate.
And note their Section 4 — contemplating what happens if deep warm water currents change in a way that changes the current temperature in areas where methane
hydrates are in equilibrium, suggesting the possibility of a rapid
large scale release of methane
gas.
On catastrophic methane degassing: Shakova and Semiletov have proposed a mechanism — the destabilisation of the permafrost cap overlying
large methane
hydrate deposits that contain a high proportion of free
gas.
Government support will prioritize research into five types of renewables and energy forms: biomass fuels and biomass power, wind power, solar power, hydrogen energy and fuel cells, and natural
gas hydrates, of which there is a
large reserve in the South China Sea and which China recently succeeded in tapping.