SCI和EI收录∣中国化工学会会刊

›› 2015, Vol. 23 ›› Issue (2): 456-460.DOI: 10.1016/j.cjche.2014.11.019

• 研究简报 • 上一篇    

Effect of Mg2+ content in ion-exchanged Shengli lignite on its equilibrium adsorption water content and its mechanism

Xiangchun Liu, Li Feng, Xinhua Wang, Ying Zhang, Haiyan Tang   

  1. Key Laboratory of Coal Processing and Efficient Utilization of Ministry of Education, School of Chemical Engineering and Technology, China University of Mining & Technology, Jiangsu 221116, China
  • 收稿日期:2013-06-10 修回日期:2013-10-12 出版日期:2015-02-28 发布日期:2015-03-01
  • 通讯作者: Li Feng
  • 基金资助:
    Supported by the National Basic Research Program of China (2012CB214900), the National Natural Science Foundation of China (51274197), the 111 Project (B12030) and the Fundamental Research Funds for the Central Universities (2014XT05).

Effect of Mg2+ content in ion-exchanged Shengli lignite on its equilibrium adsorption water content and its mechanism

Xiangchun Liu, Li Feng, Xinhua Wang, Ying Zhang, Haiyan Tang   

  1. Key Laboratory of Coal Processing and Efficient Utilization of Ministry of Education, School of Chemical Engineering and Technology, China University of Mining & Technology, Jiangsu 221116, China
  • Received:2013-06-10 Revised:2013-10-12 Online:2015-02-28 Published:2015-03-01
  • Supported by:
    Supported by the National Basic Research Program of China (2012CB214900), the National Natural Science Foundation of China (51274197), the 111 Project (B12030) and the Fundamental Research Funds for the Central Universities (2014XT05).

摘要: Mg ion-exchanged samples were prepared with acid-washed Shengli lignite. The chemical composition of the ash of the rawsamplewas determined by X-ray fluorescence. The equilibriumadsorptionwater contents of samples were determined in a range of relative humidity. The ion-exchange process was characterized by FT-IR, ash content, and pH value. A possible mechanism is proposed for equilibrium adsorption water of ion-exchanged samples at different humidities. The extent of ion-exchange reaction between Mg2+ and lignite is controlled by the concentration of Mg2+ in MgSO4 solution. The effect of Mg2+ on equilibrium adsorption water content varies with relative humidity and content ofMg2+. The factor that controls equilibriumadsorptionwater content at low relative humidity is water interactions with sorption sites, which are Mg2+-carboxyl group complex. At middle relative humidity capillary force between Mg2+-water clustersMg+(H2O)n and capillary is more important. At high relative humidity, free water-free water interactions are more significant.

关键词: Ion-exchange, FT-IR, Equilibrium adsorption water content, Surface

Abstract: Mg ion-exchanged samples were prepared with acid-washed Shengli lignite. The chemical composition of the ash of the rawsamplewas determined by X-ray fluorescence. The equilibriumadsorptionwater contents of samples were determined in a range of relative humidity. The ion-exchange process was characterized by FT-IR, ash content, and pH value. A possible mechanism is proposed for equilibrium adsorption water of ion-exchanged samples at different humidities. The extent of ion-exchange reaction between Mg2+ and lignite is controlled by the concentration of Mg2+ in MgSO4 solution. The effect of Mg2+ on equilibrium adsorption water content varies with relative humidity and content ofMg2+. The factor that controls equilibriumadsorptionwater content at low relative humidity is water interactions with sorption sites, which are Mg2+-carboxyl group complex. At middle relative humidity capillary force between Mg2+-water clustersMg+(H2O)n and capillary is more important. At high relative humidity, free water-free water interactions are more significant.

Key words: Ion-exchange, FT-IR, Equilibrium adsorption water content, Surface