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Energy resources methane

Natural gas (methane) can be obtained from gas hydrates. Gas hydrates are also called clathrates or methane hydrates. Gas hydrates are potentially one of the most important energy resources for the future. Methane gas hydrates are increasingly considered a potential energy resource. Methane gas hydrates are crystalline solids formed by combination of methane and water at low temperatures and high pressures. Gas hydrates have an iee-hke crystalline lattiee of water molecules with methane molecules trapped inside. Enormous reserves of hydrates can be foimd imder eontinental shelves and on land under permafrost. The amount of organic... [Pg.16]

Methane from renewable biological sources will never be a major energy resource, yet it can be a valuable addition to the energy supply mix. Nevertheless, whether methane comes from fossil fuel reservoirs or from bioconversions, it is certain to provide useful energy for many years to come. [Pg.794]

Gas hydrates are non-stoichiometric crystals formed by the enclosure of molecules like methane, carbon dioxide and hydrogen sulfide inside cages formed by hydrogen-bonded water molecules. There are more than 100 compounds (guests) that can combine with water (host) and form hydrates. Formation of gas hydrates is a problem in oil and gas operations because it causes plugging of the pipelines and other facilities. On the other hand natural methane hydrate exists in vast quantities in the earth s crust and is regarded as a future energy resource. [Pg.314]

The key to establishing gas hydrates as a significant energy resource is whether the methane gas will ever be economically and safely producible. The current state of knowledge is still too limited to allow reliable estimates on the start of an economic gas hydrate production. The BGR (2003) estimates gas hydrate resources at 500 Tm3. [Pg.99]

Methane hydrates have attracted much attention as future energy resources because of the enormous amounts of those deposits. Because methane has fewer carbon atoms than all other fossil fuels and the amount of exhaust CO2 is relatively small when it bums, hydrates are considered to be cleaner energy resources. Various researchers have reported that they have accumulated extensively in permafrost regions and in sediments beneath the deep ocean floor. ... [Pg.585]

Naturally occurring clathrate hydrates are found in marine sediments and in permafrost. Because they contain a large amount of methane, they are thought to have potential as an unconventional energy resource. At the same time, however, clathrate hydrates are a serious problem for the gas and oil industries, because they form easily under suitable conditions at the sites of natural gas production, transportation, and processing. The inhibition and control of hydrates in pipelines adds tremendously to gas production costs. ... [Pg.609]

A GAS HYDRATE, also known as a gas clathrate, is a gas-bearing, icelike material. It occurs in abundance in marine sediments and stores immense amounts of methane, with major implications for future energy resources and global climate change. Furthermore, gas hydrate controls some of the physical properties of sedimentary deposits and thereby influences seafloor stability. [Pg.130]

The impact on the global warming potential depends upon the use of energy resources of each process. The main greenhouse factors involved are gaseous emissions of CO2 and methane. Flnid-bed and fixed-bed gasification and waste incineration yield increased gas emissions in comparison to landfill because they release them immediately and not in more than 100 years, as assumed for the landfill. [Pg.543]


See other pages where Energy resources methane is mentioned: [Pg.358]    [Pg.358]    [Pg.262]    [Pg.166]    [Pg.339]    [Pg.347]    [Pg.95]    [Pg.621]    [Pg.57]    [Pg.98]    [Pg.296]    [Pg.262]    [Pg.537]    [Pg.282]    [Pg.162]    [Pg.408]    [Pg.611]    [Pg.48]    [Pg.96]    [Pg.97]    [Pg.18]    [Pg.39]    [Pg.449]    [Pg.486]    [Pg.237]    [Pg.59]    [Pg.321]    [Pg.239]    [Pg.396]    [Pg.86]    [Pg.278]    [Pg.563]    [Pg.481]    [Pg.497]    [Pg.281]    [Pg.139]    [Pg.142]    [Pg.736]    [Pg.1009]    [Pg.2474]    [Pg.422]    [Pg.552]    [Pg.106]   
See also in sourсe #XX -- [ Pg.321 , Pg.475 , Pg.585 , Pg.609 ]




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