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基于阻抗特征煤体中瓦斯因素对水合动力学的影响
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  • 英文篇名:Effect of Mine Gas in Coal on Hydration Kinetics Based on Impedance Characteristic
  • 作者:张强 ; 吴强 ; 张辉 ; 张保勇 ; 刘传海
  • 英文作者:ZHANG Qiang;WU Qiang;ZHANG Hui;ZHANG Bao-Yong;LIU Chuan-Hai;Department of Safety Engineering, Heilongjiang University of Science & Technology;College of Material Science and Engineering, Harbin University of Science & Technology;National Central Laboratory of Hydrocarbon Gas Transportation Pipeline Safety;
  • 关键词:瓦斯 ; 水合物 ; 阻抗 ; 动力学参数 ; 饱和度
  • 英文关键词:mine gas;;hydrate;;impedance;;kinetics parameter;;saturation
  • 中文刊名:GCRB
  • 英文刊名:Journal of Engineering Thermophysics
  • 机构:黑龙江科技大学安全工程学院;哈尔滨理工大学材料学院;瓦斯等烃气输运管网安全基础研究国家级专业中心实验室;
  • 出版日期:2019-02-15
  • 出版单位:工程热物理学报
  • 年:2019
  • 期:v.40
  • 基金:国家自然科学基金项目(No.51404102,No.51334005,No.51274267);; 2016年安全生产重大事故防治关键技术科技项目(No.heilongjiang-0002-2016AQ)
  • 语种:中文;
  • 页:GCRB201902026
  • 页数:9
  • CN:02
  • ISSN:11-2091/O4
  • 分类号:178-186
摘要
为研究不同瓦斯赋存条件下水合机理防治煤与瓦斯突出的基础规律,利用阻抗特性监测与高压瓦斯水合实验一体化装置,针对4种瓦斯气体分别在4种赋存压力(4 MPa,5 MPa,6 MPa,7 MPa)条件下开展煤体中瓦斯水合实验,根据阻抗特征获取了瓦斯水合物形成诱导时间,计算了煤体中瓦斯水合物生长速率与饱和度。结果表明:煤体中瓦斯水合过程中上层位与中层位阻抗逐渐增大,下层位阻抗逐渐减小,瓦斯水合物主要分布于上层位与中层位煤体中;随初始压力变化瓦斯水合物形成诱导时间未呈现规律性变化,随着混合气中CH_4浓度的下降,诱导时间先减小后增大,实验范围内平均诱导时间为41 min,分布范围为18~74 min;随初始压力与瓦斯气体组分浓度的变化煤体中瓦斯水合物平均生长速率呈振荡变化趋势,平均生长速率均值为0.58 cm~3·min~(-1),最快为0.84 cm~3·min~(-1);煤体中瓦斯水合物的饱和度随初始压力与瓦斯中CH_4浓度的增大呈逐渐升高的变化趋势,水合物饱和度范围为17.03%~57.03%。
        The goal of this research was to study the basic law of hydration mechanism to prevent coal and gas outburst under different gas occurrence conditions. Impedance characteristic monitoring and high pressure gas hydrate experimental device is used to carry out gas hydration experiment in coal on condition of 4 kinds of mine gas in different occurrence pressure which are 4 MPa, 5 MPa, 6 MPa and 7 MPa respectively. The induction time of gas hydrate formation is obtained according to the impedance characteristics. Meanwhile, the growth rate and saturation of mine gas hydrate are calculated. The results show that impedance value increases in the upper layer and it decreases in the lower layer in the process of mine gas hydration in coal, which also indicates that mine gas hydrate mainly forms in the upper and middle layer of the experimental reactor. The induction time of gas hydrate formation does not change regularly with the different initial pressure. However, with the decrease of CH4 concentration in the mixture gas, the induction time declines at the beginning and then rises up. The average induction time is 41 min with the range from 18 min to 74 min. The average growth rate of the gas hydrate in the coal displays the oscillation tendency with the change of initial pressure and the gas component concentration. The average growth rate is 0.58 cm~3·min~(-1) and the fastest is up to 0.84 cm~3·min~(-1). The saturation of mine gas hydrate rises gradually with the increase of initial pressure and CH4 concentration in mine gas in which the saturation ranges from 17.03% to 57.03%.
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