An experimental study of sulphate transformation during pyrolysis of an Australian lignite

The transformation of sulphate minerals during pyrolysis of an Australian lignite has been studied using pure sulphates (CaSO 4, FeSO 4 and Fe 2(SO 4) 3), a high mineral (HM) lignite sample and a low mineral (LM) lignite sample collected from different locations of the same deposit, and samples of a...

Full description

Saved in:
Bibliographic Details
Published inFuel processing technology Vol. 91; no. 3; pp. 313 - 321
Main Authors Yani, Setyawati, Zhang, Dongke
Format Journal Article
LanguageEnglish
Published Amsterdam Elsevier B.V 01.03.2010
Elsevier
Subjects
Online AccessGet full text

Cover

Loading…
More Information
Summary:The transformation of sulphate minerals during pyrolysis of an Australian lignite has been studied using pure sulphates (CaSO 4, FeSO 4 and Fe 2(SO 4) 3), a high mineral (HM) lignite sample and a low mineral (LM) lignite sample collected from different locations of the same deposit, and samples of acid-washed LM doped with sulphates (CaSO 4+ LM and FeSO 4+ LM), respectively. Thermogravimetric analysis and fixed-bed reactor techniques were used for the pyrolysis experimentation and the lignite samples and their chars were analysed using FTIR and XRD. The TGA experiments showed that CaSO 4 decomposes between 1400 and 1700 K in nitrogen and a 50/50 N 2/CO 2 mixture, while in air CaSO 4 decomposes between 1500 and 1700 K. Using a TGA–MS it was found that only a small fraction of CaSO 4 in CaSO 4+ LM decomposed at 653 K, releasing SO 2. CaSO 4 was still observed in the char recovered at 1073 K as confirmed by the FTIR and XRD analysis. FeSO 4·7H 2O released the bound water below 543 K and the remaining FeSO 4 decomposed between 813 and 953 K. FeSO 4 in FeSO 4+ LM decomposed at 500 K to release SO 2. The inherent sulphates in HM were dominated by iron sulphates which started to decompose and release SO 2 at around 500 K and all sulphate had been decomposed at 1073 K. It was observed that during the fixed-bed pyrolysis at 1073 K in nitrogen, approximately 36% of the total sulphur in the CaSO 4+ LM decomposed, 88% of the total sulphur in the FeSO 4+ LM decomposed and around 76% of the total sulphur in HM decomposed. It was also confirmed that FeSO 4+ LM produced more volatile sulphur than CaSO 4+ LM during pyrolysis.
Bibliography:ObjectType-Article-1
SourceType-Scholarly Journals-1
ObjectType-Feature-2
content type line 23
ISSN:0378-3820
1873-7188
DOI:10.1016/j.fuproc.2009.11.002