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Research and Development Activities on Methane Hydrate for The Future Energy Resources

机译:未来能源甲烷水合物的研发活动

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Methane hydrate is a solid material composed of a methane molecule and water molecules. Water molecules form a cage in which a methane molecules was kept at low temperature and high pressure. It is dissociated by increasing temperature and/or releasing pressure. In mid 1960, the first methane hydrate accumulation (deposit) was found in the sediment beneath the permafrost. And also the accumulation have been found in the ocean sediment below see floor over about 500m in depth. In the ocean sediment around Japan, it is estimated that the amount of gas equivalent to today's natural gas consumption for 100 years could be extracted from hydrate reservoirs.When we tried to get gas from the methane hydrate, it is necessary to control the dissociating rate of the hydrate, and the phase control process must be developed through fundamental works on phase equilibrium and kinetics of methane hydrate. The process control system of formation and dissociation of hydrate by considering molecular kinetics is very important for the development at a desirable gas production rate. In this paper, previous researches are outlined on discovery, structure and characteristics, potential for the energy resources and future subjects on the methane hydrate.
机译:甲烷水合物是由甲烷分子和水分子组成的固体物质。水分子形成笼子,其中甲烷分子被保持在低温和高压下。它通过增加温度和/或释放压力而解离。 1960年中期,在永久冻土下的沉积物中发现了第一个甲烷水合物堆积(沉积)。而且在水下约500m深度的海底沉积物中也发现了沉积物。据估计,在日本周围的海洋沉积物中,可以从水合物储层中提取相当于当今100年天然气消耗量的天然气。当我们试图从甲烷水合物中获取天然气时,有必要控制解离速率的水合物,必须通过有关甲烷水合物的相平衡和动力学的基础研究来开发相控制过程。通过考虑分子动力学来形成和分解水合物的过程控制系统,对于以所需的气体生产率进行开发非常重要。在本文中,概述了有关甲烷水合物的发现,结构和特征,能源潜力和未来主题的先前研究。

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