4.5 Article

Application of TG-FTIR to study SO2 evolved during the thermal decomposition of coal-derived pyrite

期刊

THERMOCHIMICA ACTA
卷 555, 期 -, 页码 1-6

出版社

ELSEVIER
DOI: 10.1016/j.tca.2012.12.025

关键词

Coal-derived pyrite; Thermal decomposition; Gas evolution; TG-FTIR

资金

  1. National Natural Science Foundation of China [51034006]
  2. China Postdoctoral Science Foundation [2011M500034, 2012T50160]

向作者/读者索取更多资源

The thermal decomposition of the coal-derived pyrite was studied using thermogravimetry combining with Fourier-transform infrared spectroscopy (TG-FTIR) techniques to gain knowledge on the SO2 gas evolution process and formation mechanism during the thermal decomposition of the coal-derived pyrite. The results showed that the thermal decomposition of the coal-derived pyrite which started at about 400 degrees C was complete at 600 degrees C; the gas evolved can be established by combining the DTG peak, the Gram-Schmidt curve and in situ FUR spectroscopic evolved gas analysis. It can be observed from the spectra that the pyrolysis products for the sample mainly vary in quantity, but not in species. It was proposed that the oxidation of the coal-derived pyrite started at about 400 degrees C and that pyrrhotite and hematite were formed as primary products. The SO2 released by the thermal decomposition of the coal-derived pyrite mainly occurred in the first pyrolysis stage between 410 and 470 degrees C with the maximum rate at 444 degrees C. Furthermore, the SO2 gas evolution and formation mechanism during the thermal decomposition of the coal-derived pyrite has been proposed. (C) 2013 Elsevier By. All rights reserved.

作者

我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。

评论

主要评分

4.5
评分不足

次要评分

新颖性
-
重要性
-
科学严谨性
-
评价这篇论文

推荐

暂无数据
暂无数据