刘卫国

个人信息Personal Information

教授

博士生导师

硕士生导师

性别:男

毕业院校:大连理工大学

学位:博士

所在单位:能源与动力学院

学科:能源与环境工程

办公地点:大连理工大学西部校区能源与动力大楼

电子邮箱:liuwg@dlut.edu.cn

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Investigation on the induction time of methane hydrate formation in porous media under quiescent conditions

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论文类型:期刊论文

发表时间:2016-09-01

发表刊物:JOURNAL OF PETROLEUM SCIENCE AND ENGINEERING

收录刊物:SCIE、EI、Scopus

卷号:145

页面范围:565-572

ISSN号:0920-4105

关键字:Methane hydrate; Hydrate reformation; Induction time; Memory effect

摘要:The induction time for the formation of hydrates is an important parameter in hydrate-based technology and natural gas hydrate exploitation. The influences of effective factors on induction time are not explained clearly in the current. To obtain data on the induction time for hydrate formation and re-formation processes, experimental studies were carried out for methane hydrates formed in porous media. The vessel used is divided into six compartments of the same size. The temperatures of different regions in the vessel can be measured during experiments. Six T-type thermocouples and a pressure transducer (Nagano Keiki, Japan) were connected to the vessel to measure the temperature (T) and pressure (P), respectively. Forty-eight experimental cycles were performed at 6 MPa and at temperatures from 273.65 K to 276.65 K. The influences of the memory effect, initial water saturation, and hydrate dissociation temperature and dissociation time on the CH4 hydrate formation/reformation induction time are studied. The experimental results showed that there is a memory effect when the experimental temperature is greater than 275.15 K at 6 MPa and that the memory effect reduces the hydrate formation induction time. Long dissociation times and high dissociation temperatures eliminate the memory effect. Low experimental temperature led to a short induction time, and the influence of experimental temperature on the induction time was reduced when the experimental temperature was less than 275.65 K. The initial saturation also affected the induction time. The induction time for the hydrate formation decreased as the initial water saturation increased from 30% to 70%. The measured induction times were correlated to an induction time model developed based on the nucleation theory. The results obtained in this work indicate that hydrate formation in porous media is heterogeneous nucleation. (c) 2016 Elsevier B.V. All rights reserved.