首页> 外文期刊>Energy >Mathematical models of the heat-water dissociation. of natural gas hydrates considering a moving Stefan boundary
【24h】

Mathematical models of the heat-water dissociation. of natural gas hydrates considering a moving Stefan boundary

机译:热水分离的数学模型。 Stefan边界移动的天然气水合物数量

获取原文
获取原文并翻译 | 示例
           

摘要

This paper presents mathematical models for radial, quasi-steady state heat transfer in a semi-infinite hydrate reservoir with a moving boundary that is related to the dissociation of natural gas hydrates. The exact solutions of the temperature in the dissociation zone and hydrate zone, using the Paterson exponential integral function, are obtained, and the dissociation frontal brim location of the hydrates is determined by combining the Deaton method with the Clausius Claperyron equation. A sample calculation shows that the reservoir temperature falls sharply to the dissociation temperature and then drops gradually with increasing distance to the reservoir temperature. With respect to time, the temperature increases slowly to the dissociation temperature, after which, the dissociation temperature falls sharply to the temperature close to that of the injected hot-water. By increasing the temperature of injected hot-water, more hydrates participate in dissociation; with an increase in time, the radius quickly increases, but the radius of hydrate dissociation increases slowly. (C) 2015 Elsevier Ltd. All rights reserved.
机译:本文提出了一个半无限水合物储层中径向,准稳态传热的数学模型,该水合物储层的运动边界与天然气水合物的解离有关。利用帕特森指数积分函数,获得了离解区和水合物区温度的精确解,并通过将Deaton方法与Clausius Claperyron方程相结合来确定水合物的离解前缘位置。样本计算表明,储层温度急剧下降至解离温度,然后随着距储层温度距离的增加而逐渐下降。关于时间,温度缓慢升高至离解温度,此后,离解温度急剧下降至接近注入热水的温度。通过增加注入热水的温度,更多的水合物参与离解。随着时间的增加,半径迅速增加,但是水合物离解的半径缓慢增加。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号