Radial mathematical model for hot water dissociation frontal brim of natural gas hydrates

被引:0
|
作者
Li, Ming-Chuan [1 ]
Fan, Shuan-Shi [2 ]
机构
[1] School of Petroleum Engineering, China University of Petroleum (East China)
[2] School of Chemistry and Chemical Engineering, South China University of Technology
来源
Gao Xiao Hua Xue Gong Cheng Xue Bao/Journal of Chemical Engineering of Chinese Universities | 2013年 / 27卷 / 05期
关键词
Dissociation frontal brim; Natural gas hydrate; Radial mathematical model; Stefan moving boundary;
D O I
10.3969/j.issn.1003-9015.2013.05.006
中图分类号
学科分类号
摘要
Based on the description of dissociation process of natural gas hydrate in a semi-infinite zone, a radial pseudo-stationary mathematical model of heat transfer was built with Stefan moving boundary, and accurate solution of temperature applied in dissociation zone and natural gas hydrate zone was calculated by using Paterson method of exponential integral function. In addition, the location of dissociation frontal brim of natural gas hydrate was determined by combining Deaton method with Clausius-Clapeyron equation for decomposition heat. Radial dissociation laws of natural gas hydrate were obtained through an example of a steady hydrate reservoir whose physical parameters are known: with the increasing of radial range, temperature of hydrate reservoir drops abruptly to 8.416°C (dissociation temperature) and further to 5.33°C (reservoir temperature), and the location of dissociation frontal brim changes slowly; besides, with the increase of time, the temperature rises sharply after increasing slowly from 5.33°C to 8.416°C, and after adequate days will reach 100°C (the injected hot water temperature); furthermore, radius of hydrate dissociation grows slowly, and after 150 days supposed dissociation temperature changes 27.3°C for 80~100°C and 49.3°C for 100~150°C.
引用
收藏
页码:761 / 766
页数:5
相关论文
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