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Oxidation of high sulphur coal. Part 1. Desulphurisation and evidence of the formation of oxidised organic sulphur species

✍ Scribed by D. Borah; M.K. Baruah; I. Haque


Book ID
104135614
Publisher
Elsevier Science
Year
2001
Tongue
English
Weight
192 KB
Volume
80
Category
Article
ISSN
0016-2361

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✦ Synopsis


A systematic study has been made on the desulphurisation of organic sulphur in both feed and mercury-treated coal for their unoxidised samples as well as their oxidised samples prepared at 50, 100 and 150ЊC in air under normal atmospheric pressure. A continuous increase of organic sulphur loss has been observed; the magnitude of which is substantial in mercury-treated samples. Formation of oxidised organic sulphur functionalities (SyO and -SO 2 ) are identified by infrared spectroscopy. The band in the region 1080-1020 cm Οͺ1 assignable to SyO stretch for all oxidised sulphur species (sulphoxide, sulphone, sulphonic acid, sulfenic acid and sulphinic acid) while the band in the region 1350-1320 cm Οͺ1 attributable to assymmetric and 1170-1120 cm Οͺ1 to symmetric for -SO 2 stretch for sulphones, sulphonic acid and sulphinic acid, increase in intensity up to 100ЊC which decline at 150ЊC. The absorbance of these bands are qualitatively correlated with those of aliphatic and aromatic C-H content. The aliphatic C-H content follows similar pattern as observed for the absorbance for SyO and -SO 2 strech; however, the trend is exactly similar with the mercury-treated sample. The difference of absorbance between SyO and -SO 2 gives an indication of the extent of sulphoxide and sulfenic acid formation. Mercury has a catalytic effect in both accelerating the oxidised species formation and their desulphurisation. This study further reveals that up to 50ЊC desulphurisation is primarily due to the release of free radicals of sulphur species while SyO species along with these radicals predominantly removed beyond 50ЊC. Knowledge gained from this study would be helpful for various coal conversion processes.


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