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The Proposal of Methane Hydrate Development System using Carbon Dioxide Hydrate

机译:利用二氧化碳水合物开发甲烷水合物系统的建议

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As for the development of methane hydrate that exists under bottom of the sea, the safety measures are most important. The methane hydrate development system using artificial block and prop system was proposed to prevent the landslide and the sudden fall. Artificial block system is a method of improving strength of the sediment by injecting carbon dioxide into the sediment.It was assumed to form carbon dioxide hydrate in the bottom of the sea stratum to achieve this purpose, and so we examined the properties of formation / dissociation, and the influence of the particle. The results obtained are as follows;(1)The formation condition approaches the estimated equilibrium value by mixing the particle, and the level of the shift depends on the correlation of the heat conductivity of the particle and waten It can be suggested that carbon dioxide hydrate be formed easily at the case without the stratum particle when the carbon dioxide bubble rises as a result within the space of the particle in the sediment. It is considered that the dissociation condition of carbon dioxide hydrate almost agrees to the estimated equilibrium value in any case, and is not influenced by the presence of the stratum particle.(2) It has been understood that the supercooling phenomenon be comes smaller with increasing the particle diameter, and that the particle diameter has close relation to the formation condition of carbon dioxidehydrate. This shows that the formation condition changes according to the particle diameter of the sediment.(3) The initial formation rate varies from the range of 0.2 to 0.6 ml / (min g), and the dissociation rate varies from 1 to 1.5 ml I (min g) in case of carbon dioxide hydrate. The rates increase with the presence of the particle, and also increase with the particle diameter.We will continue to achieve the methane hydrate development system by the experiment that uses similar particles to the strata of the sea sediment in the future.
机译:对于海底甲烷水合物的开发,安全措施是最重要的。为了防止山体滑坡和突降,提出了利用人工区块和支撑系统开发甲烷水合物系统。人工区块系统是通过向沉积物中注入二氧化碳来提高沉积物强度的方法,为了达到这一目的,人们假设在海床底部形成二氧化碳水合物,因此我们研究了地层/离解的性质。以及粒子的影响。得到的结果如下:(1)通过混合颗粒使形成条件达到估计的平衡值,并且位移的水平取决于颗粒与水的导热性的相关性。当二氧化碳气泡在沉淀物中的颗粒空间内上升时,在没有地层颗粒的情况下容易形成颗粒。认为在任何情况下,二氧化碳水合物的解离条件几乎都与估计的平衡值一致,并且不受层状颗粒的存在的影响。(2)可以理解,随着温度的升高,过冷现象会变小。粒径,该粒径与二氧化碳水合物的形成条件密切相关。这表明形成条件随沉积物的粒径而变化。(3)初始形成速率在0.2至0.6 ml /(min g)的范围内变化,离解速率在1至1.5 ml I(最小g)如果是二氧化碳水合物。速率随着颗粒的存在而增加,并且也随着粒径的增加而增加。将来,我们将通过使用与海底沉积物地层相似的颗粒的实验,继续实现甲烷水合物开发系统。

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