CaSO4-C-H2O体系研究:模拟实验与热力学探讨
DOI:
作者:
作者单位:

作者简介:

通讯作者:

中图分类号:

基金项目:

国家自然科学基金项目(面上项目,重点项目,重大项目)


Study of CaSO4-C-H2O System: Simulation Experiments and Thermodynamic Assessment
Author:
Affiliation:

Fund Project:

  • 摘要
  • |
  • 图/表
  • |
  • 访问统计
  • |
  • 参考文献
  • |
  • 相似文献
  • |
  • 引证文献
  • |
  • 资源附件
  • |
  • 文章评论
    摘要:

    传统认为TSR成因的固态沥青(焦沥青)属于热化学反应的终端产物,不会对TSR的反应进程起到重要作用。本文以活性炭作为固态沥青(焦沥青)的模型化合物,开展了CaSO4-C-H2O体系的热模拟实验研究,探讨了CaSO4-C-H2O体系发生TSR的热力学特征。实验结果表明,CaSO4-C-H2O体系在300 ℃时即可启动TSR,主要生成CaCO3、H2S和CO2等产物。这一TSR门限温度要远低于以往室内利用气态或液态烃类进行的TSR模拟实验温度范围,与热力学计算结果一致。利用HSC Chemistry 5.0软件进行TSR过程模拟,发现25 -200 ℃时CaSO4-C-H2O体系发生的TSR完全受动力学控制,在温度保持不变情况下,压力增大不利于CaSO4-C-H2O体系发生TSR。较少的含水量对TSR有一定促进作用,而含水量过多则可能抑制TSR的进行,含水量对TSR的影响可能与CaSO4在水中的饱和浓度有关。在一定的温度下,当体系pH≤2时,随着pH逐渐降低,CaSO4的量呈线性递减,但在沉积盆地地层水pH范围内(pH>4),pH对TSR的作用可以忽略不计。CaSO4-C-H2O体系发生的TSR反应是一个放热过程,并且随着温度升高,反应热逐渐增大。在25-200℃范围内,TSR反应热为12.9-133 J/(mol)CaSO4。热力学计算以及模拟实验结果均暗示,固态沥青(焦沥青)可能比烃类更容易参与TSR。

    Abstract:

    Traditionally TSR-solid bitumens (pyrobitumen) have been recognized as direct, stable products of the thermochemical process. Compared with hydrogen sulfide (H2S), the presence of these solid bitumens has not been considered an important factor in TSR In this paper, activated carbon (C) was selected as a model compound for solid bitumen (pyrobitumen), and thermochemical reduction of calcium sulfate (CaSO4) by activated carbon (C) was carried out under hydrothermal conditions at elevated temperatures. Thermodynamic characteristics of the system of CaSO4-C-H2O were investigated. According to the experimental results, CaCO3, H2S and CO2 were determined as the main TSR products. The threshold temperature for initiating TSR in the present study was only 300 ℃, which was much lower than those of most previous TSR simulations using hydrocarbons and in accordance with the further thermodynamic calculations. Process simulation of TSR was conducted using the software of HSC Chemistry 5.0. It was found that at reservoir temperatures of 25℃-200℃, TSR in the system of CaSO4-C-H2O was totally controlled by kinetic factors. Under a constant temperature, the increasing pressure was unfavorable to the initiation of TSR. The intensity of TSR was closely associated with the amount of water. The small amount of water may contribute to better oxidizing conditions. The influence of water content on TSR may be related to the saturation concentration of CaSO4. When pH≤2, sulfate reduction rates are dependent upon the decrease of pH at a certain temperature. However, in the pH range of sedimentary basin formation water (pH>4), effect of pH on TSR is negligible. TSR in the system of CaSO4-C-H2O was an exothermic process. The released heat increased with the increasing temperatures, which was estimated as about12.9 J-133 J/(mol)CaSO4 at 25 ℃-200 ℃. Thermodynamic studies and the experimental results implied that solid bitumens (pyrobitumen) more easily involved in TSR than gaseous or liquid hydrocarbons.

    参考文献
    相似文献
    引证文献
引用本文

丁康乐,罗跃,单敬福,关富佳,王莎莎.2013. CaSO4-C-H2O体系研究:模拟实验与热力学探讨[J].地质学报,87(3):424-432.
ding kang le, luo yue, Shan Jing fu, guan fu jia, wang sha sha.2013. Study of CaSO4-C-H2O System: Simulation Experiments and Thermodynamic Assessment[J]. Acta Geologica Sinica,87(3):424-432.

复制
分享
文章指标
  • 点击次数:
  • 下载次数:
  • HTML阅读次数:
  • 引用次数:
历史
  • 收稿日期:2012-03-08
  • 最后修改日期:2012-07-31
  • 录用日期:2012-08-20
  • 在线发布日期: 2013-03-01
  • 出版日期: