...
首页> 外文期刊>Fuel >Coal pyrolysis characteristics by TG-MS and its late gas generation potential
【24h】

Coal pyrolysis characteristics by TG-MS and its late gas generation potential

机译:TG-MS分析煤的热解特性及其后期生气潜力

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

As natural gas production from deep strata becomes increasingly successful in recent years, the evaluation on gas generation potential from OM (organic matter) in the deep formations is attracting increasing attention recently, especially the late gas generation potential. In this paper, a TG-MS (thermogravimetric analysis-mass spectrometry) device was applied to investigate the process and characteristics of gas generation of HCs (hydrocarbons) and non-HCs (non-hydrocarbons) during the pyrolysis processes of coal from Songliao Basin, and its late gas generation potential. The TG-MS experimental results show that: (1) during coal pyrolysis with heating rate of 10 degrees C/min, methane generation started at similar to 300 degrees C, reached its peak generation at 480 degrees C, and ended at similar to 850 degrees C, which was much higher than the ending generation temperatures of other HCs; (2) when investigating the methane generation characteristics through the gas generation curve by ion fragments, more accurate results are obtained with mass to charge ratio m/z = 15 than currently used m/z = 16; (3) this coal has a high late gas generation potential, with 17% additional methane generated at late generation stage after 600 degrees C (equivalent to a vitrinite reflectance: Ro >= 2.5%), and the methane generation ended at a maturity level of 5.3% (Ro). After calibration with coal pyrolysis results, a kinetic model has been established and applied successfully to estimate gas generation timing and illustrate gas generation mechanisms of the Shahezi Formation in the Xujiaweizi Fault Depression. Based on the results derived from the proposed kinetic model, the gas generation timing for the Shahezi Formation was between similar to 115 and 50 Ma, and methane appeared to be generated steadily without any major generation peak indentified during this period and the gas generation lasted for similar to 65 Ma. (C) 2015 Elsevier Ltd. All rights reserved.
机译:随着近年来来自深层的天然气生产越来越成功,近来对深层地层中的OM(有机物)产气潜力的评估引起了越来越多的关注,尤其是后期产气潜力。本文采用TG-MS(热重分析-质谱)装置研究松辽盆地煤热解过程中HCs(烃)和非HCs(非烃)的产气过程和特征。 ,其后期的产气潜力。 TG-MS实验结果表明:(1)以10℃/ min的升温速率进行煤热解过程中,甲烷的生成开始于300℃左右,甲烷的峰值生成达到480℃,结束于850℃。摄氏度,远高于其他HC的最终生成温度; (2)当通过离子碎片通过气体生成曲线研究甲烷生成特性时,质荷比m / z = 15时比当前使用的m / z = 16时可获得更准确的结果; (3)该煤具有较高的后期瓦斯生成潜力,在600摄氏度后的后期生成阶段会额外产生17%的甲烷(相当于镜质体反射率:Ro> = 2.5%),并且甲烷的生成在成熟水平结束5.3%(Ro)。通过对煤热解结果的标定,建立了动力学模型,并成功地应用了动力学模型来估算天然气生成时间,并阐明了徐家围子断陷沙河子组的天然气生成机理。根据所提出的动力学模型得出的结果,沙河子组的产气时间大约在115Ma和50Ma之间,甲烷稳定地生成,在此期间没有发现任何主要的生成峰,并且瓦斯生成持续了类似于65 Ma。 (C)2015 Elsevier Ltd.保留所有权利。

著录项

  • 来源
    《Fuel》 |2015年第15期|243-253|共11页
  • 作者单位

    China Univ Petr East China, Res Inst Unconvent Petr & Renewable Energy RIUP&R, Qingdao 266580, Shandong, Peoples R China|CSIRO Energy Flagship, N Ryde, NSW 2113, Australia;

    CSIRO Energy Flagship, N Ryde, NSW 2113, Australia|UNSW Australia, Sch Biol Earth & Environm Sci BEES, Sydney, NSW 2052, Australia;

    China Univ Petr East China, Res Inst Unconvent Petr & Renewable Energy RIUP&R, Qingdao 266580, Shandong, Peoples R China;

    China Univ Petr East China, Res Inst Unconvent Petr & Renewable Energy RIUP&R, Qingdao 266580, Shandong, Peoples R China;

    China Univ Petr East China, Res Inst Unconvent Petr & Renewable Energy RIUP&R, Qingdao 266580, Shandong, Peoples R China;

  • 收录信息 美国《科学引文索引》(SCI);美国《工程索引》(EI);
  • 原文格式 PDF
  • 正文语种 eng
  • 中图分类
  • 关键词

    TG-MS; Late gas generation potential; Coal pyrolysis; Kinetics; Xujiaweizi Fault Depression; Songliao Basin;

    机译:TG-MS;晚期生气潜力;煤热解;运动学;松辽盆地徐家围子断陷;

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