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二氧化碳-水体系中水合物形成的相图及高压边界

Phase diagram and high-pressure boundary of hydrate formation in the carbon dioxide-water system.

作者信息

Manakov Andrej Yu, Dyadin Yuriy A, Ogienko Andrey G, Kurnosov Alexander V, Aladko Eugeny Ya, Larionov Eduard G, Zhurko Fridrih V, Voronin Vladimir I, Berger Ivan F, Goryainov Sergei V, Lihacheva Anna Yu, Ancharov Aleksei I

机构信息

Nikolaev Institute of Inorganic Chemistry SB RAS, Akademii, Lavrentiev Avenue, 3, Novosibirsk, 630090, Russian Federation.

出版信息

J Phys Chem B. 2009 May 21;113(20):7257-62. doi: 10.1021/jp9008493.

Abstract

Experimental investigation of the phase diagram of the system carbon dioxide-water at pressures up to 2.7 GPa has been carried out in order to explain earlier controversial results on the decomposition curves of the hydrates formed in this system. According to X-ray diffraction data, solid and/or liquid phases of water and CO2 coexist in the system at room temperature within the pressure range from 0.8 to 2.6 GPa; no clathrate hydrates are observed. The results of neutron diffraction experiments involving the samples with different CO2/H2O molar ratios, and the data on the phase diagram of the system carbon dioxide-water show that CO2 hydrate of cubic structure I is the only clathrate phase present in this system under studied P-T conditions. We suppose that in the cubic structure I hydrate of CO2 multiple occupation of the large hydrate cavities with CO2 molecules takes place. At pressure of about 0.8 GPa this hydrate decomposes into components indicating the presence of the upper pressure boundary of the existence of clathrate hydrates in the system.

摘要

为了解释该系统中形成的水合物分解曲线早期存在争议的结果,已对压力高达2.7 GPa的二氧化碳-水体系的相图进行了实验研究。根据X射线衍射数据,在室温下,水和二氧化碳的固相和/或液相在0.8至2.6 GPa的压力范围内共存;未观察到笼形水合物。涉及不同CO₂/H₂O摩尔比样品的中子衍射实验结果以及二氧化碳-水体系的相图数据表明,在研究的P-T条件下,立方结构I的CO₂水合物是该体系中唯一存在的笼形相。我们认为,在立方结构I的CO₂水合物中,大的水合物笼被CO₂分子多重占据。在约0.8 GPa的压力下,这种水合物分解成组分,表明该体系中笼形水合物存在的压力上限。

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