Gas hydrate refers to a solid compound made up of water molecules and gas molecules, usually methane. It forms when gas molecules get trapped within water molecules at very cold temperatures and high pressures, creating a crystalline structure. These hydrates are often found in deep seas and permafrost regions.
Full definition
One cubic meter
of gas hydrate on the ocean floor contains 165 cubic meters of gas at room temperature and pressure.
Ice sheets are heavy and cold, providing pressure and temperatures that contain methane in form of ice - like substance
called gas hydrate.
This year's spending plan is focused on carbon capture and storage technologies and
gas hydrate research.
Warming destabilises permafrost and marine sediments of methane
gas hydrates in some regions according to some model simulations (Denman et al., 2007 Section 7.4.1.2), as has been proposed as an explanation for the rapid warming that occurred during the Palaeocene / Eocene thermal maximum (Dickens, 2001; Archer and Buffett, 2005).
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.
«The most likely process where this happens - and there is geological evidence that it has happened in the past - is when the
methane gas hydrate layer in the sediment destabilises on a slope.
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.
Gordon Research Conference on
Natural Gas Hydrate Systems will be held in Galveston, Texas from February 28 to March 4, 2016.
The University of New Hampshire will study the dynamic response of
gas hydrate systems and their potential impact on sea - floor stability, ocean ecology, and global climate by reconstructing the paleo - positions of certain parameters related to the release of methane at three sites on the Cascadia margin.
These data include new aircraft observations from the northern permafrost region (e.g., the NASA Arctic - Boreal Vulnerability Experiment) and measurement of sea - air gas exchange (e.g., the U.S. Geological Survey (USGS)
Gas Hydrates Project).
It was stored
as gas hydrate in the sediment, constantly fed by gas from below, creating over-pressured conditions.
Cretaceous climate warming led to a significant methane release from the seafloor, indicating potential for similar destabilization of
gas hydrates under modern global warming.
Such a scenario, though very uncertain, has the potential to influence the stability of
gas hydrates on the slope.
There are
large gas hydrate deposits, and many crater - like structures, so - called «pockmarks», on the seabed.
Reference: Serov, P., et.al., Postglacial response of Arctic
Ocean gas hydrates to climatic amelioration.
In 2002 an international team of scientists began drilling into the frozen
Mallik Gas Hydrate Field in Canada's Northwest Territories to explore this second possibility.
When drilling in oil - and gas - bearing formations submerged in deep water, the reservoir gas may flow into the well bore and
form gas hydrates owing to the low temperatures and high pressures found during deep water drilling.
Our results stress the importance of external climatic forcing of the dynamics of the seafloor, and the role of the rapid warming following the Younger Dryas in pacing the
marine gas hydrate reservoir.
The Indian National
Gas Hydrate Program was an important part of the Bay of Bengal explorations, as India can use a natural gas supply to replace LNG imports.
Brewer, P.G., C. Paull, E.T. Peltzer, W. Ussler, G. Rehder, and G. Friederich, Measurements of the fate of
gas hydrates during transit through the ocean water column, Geophysical Research Letters, 29 (22), 2002.
The research to be conducted by Georgia Tech will advance the understanding of the behavior of
gas hydrates hosted in fine - grained sediments such as clay or silt, and will evaluate extraction methods relevant to the potential to produce gas from such sediments.
The research proposed by Oklahoma State will help to further develop an understanding of the structural and geologic controls on hydrate occurrence and distribution in Walker Ridge 313 and Green Canyon 955 using new techniques to interpret
gas hydrate occurrences in existing seismic data, along with well data collected during prior Energy Department research efforts at those sites.
[25] The Mallik
gas hydrate field was first discovered by Imperial Oil in 1971 - 1972.
Gas hydrates naturally form along the coasts of continents and in Arctic permafrost, places where water and gas mix at relatively high pressure and low temperature.
Permafrost was known to
contain gas hydrates — icelike mixtures of water and organic gases first identified in deep - sea sediments which form only at very high pressures and low temperatures.
«We should see
gas hydrate becoming a meaningful and environmentally friendly resource in the next century,» Sassen says.
Biastoch, et al (eleven of them, including Latif, and Wallman at the University of Kiel, have thought about the fate of the methane hydrates, and in an article entitled «Rising Arctic Ocean temperatures
cause gas hydrate destabilization and ocean acidification» conclude that the major effect will be a decrease of pH, near the Arctic Ocean coasts.
«The Energy Policy Act of 2005 similarly speaks directly to the production of fossil fuels... («The purpose of this section is to promote natural gas production from the natural
gas hydrate resources on the outer Continental Shelf and Federal lands in Alaska»); id.
Researchers at Southern Methodist University will conduct numerical modeling, field data collection, and extensive laboratory analyses to characterize the state of the upper boundary of pressures and temperatures
where gas hydrates are in a stable form on the Alaskan Beaufort continental slope.
This is
why gas hydrates are found not only in the Arctic, but all over the world on the sea shelf and underwater slopes.
Based on pressure and temperature modelling, we show that the last deglaciation could have triggered dissociation of
gas hydrates present in the region of the northern part of the Norwegian Channel, causing degassing of 0.26 MtCH4 / km2 at the seafloor.
Phrases with «gas hydrate»