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Natural gas hydrates - A promising source of energy

机译:天然气水合物-一种有希望的能源

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Gas hydrates are clathrate physical compounds, in which the molecules of gas are occluded in crystalline cells, consisting of water molecules retained by the energy of hydrogen bonds. All gases can form hydrates under different pressures and temperatures. The crystalline structure of solid gas hydrate crystals has a strong dependence on gas composition, pressure, and temperature. Presently, three crystalline structures are known (Sloan, 1990, 2007) to form at moderate pressure, and nearly ten structures in the pressure range above 100 MPa. For example, methane hydrate can be stable at a pressure of 20 nPa to 2 GPa, and at temperatures changing from 70 to 350 K (Makogon, 1997). Formation of gas hydrate occurs when water and natural gas are present at a low temperature and a high pressure. Such conditions often exist in oil and gas wells, and pipeline equipment. Hydrate plugs can damage gas transport system equipment. The petroleum industry spends about one billion US dollars a year to prevent hydrate formation in wells, pipelines and equipment. Natural deposits of gas hydrates also exist on Earth in colder regions, such as permafrost, or sea bottom areas. Natural gas hydrates are an unconventional energy resource. Potential reserves of gas in hydrated posits distributed offshore and on land are over 1.5 x 10~(16) m~3 (Makogon, 1982). About 97% of natural gas hydrates have been located offshore, and only 3% on land. At present time, there are several successful federal research programs in a number of countries for research and development of gas hydrate deposits. Over 230 gas hydrate deposits were discovered, over a hundred wells drilled, and kilometers of cores studied. Gas hydrate resource is distributed conveniently for development by most every country. Effective tools for the recovery of gas from hydrate deposits, and new technology for development of gas hydrate deposits are being developed. There is a commercial production of natural gas from hydrates in Siberia. Researchers continue to study the properties of natural gas hydrates at reservoir conditions, and develop new technologies for exploration and production of gas from hydrate deposits in different geological formations.
机译:气体水合物是笼形的物理化合物,其中的气体分子被吸留在结晶池中,由氢键能量保留的水分子组成。所有气体可以在不同的压力和温度下形成水合物。固体气体水合物晶体的晶体结构强烈依赖于气体组成,压力和温度。目前,已知在中等压力下会形成三种晶体结构(Sloan,1990,2007),在高于100 MPa的压力范围内会形成近十种晶体结构。例如,甲烷水合物在20 nPa至2 GPa的压力以及70至350 K的温度变化下可以保持稳定(Makogon,1997)。当水和天然气在低温和高压下存在时,就会形成天然气水合物。此类条件通常存在于油气井和管道设备中。水合物塞可能损坏气体传输系统设备。石油工业每年花费约10亿美元来防止井,管道和设备中的水合物形成。天然气水合物的天然沉积物也存在于地球上较冷的地区,例如永久冻土或海底地区。天然气水合物是一种非常规能源。分布在近海和陆地上的水合气藏中的天然气潜在储量超过1.5 x 10〜(16)m〜3(Makogon,1982)。约有97%的天然气水合物位于海上,而陆地上只有3%。目前,在许多国家中有几个成功的联邦研究计划,用于研发天然气水合物矿床。发现了230多个天然气水合物矿床,钻了100多口井,并研究了数千米的岩心。天然气水合物资源被大多数国家方便地分配用于开发。正在开发用于从水合物沉积物中回收气体的有效工具,以及用于开发天然气水合物沉积物的新技术。西伯利亚有天然气水合物的商业生产。研究人员继续研究储层条件下天然气水合物的性质,并开发新技术,以利用不同地质构造中的水合物沉积物勘探和生产天然气。

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