305
Views
14
CrossRef citations to date
0
Altmetric
Original Articles

Impact of complex reacting atmosphere on ash fusion characteristics and minerals conversion in coal combustion process

, , , , &
Pages 1178-1193 | Received 12 May 2017, Accepted 13 Feb 2018, Published online: 04 Apr 2018
 

ABSTRACT

The surrounding atmosphere of coal particles changes continually during the combustion process in pulverized coal boilers. A part of noncombustible mineral composition in char will be melted under high temperature and then leads to the plugging of pores in char. The O2 molecule used for combustion is hard to diffuse into the inside of char. However, the investigation on ash fusion properties of coal in real combustion atmosphere is still ambiguous. In the present study, the ash fusion temperatures (AFTs) of high Fe coal and low Fe coal were tested under complex atmospheres, which simulated the real condition during coal particles combustion. The ash samples were prepared at 1373 K in the typical conditions and then analyzed by X-ray diffraction to explain the conversion of minerals. In addition, the chemical equilibrium compositions calculations were carried out to obtain the transformation of atmosphere-sensitive Fe species with the atmosphere change. Results indicated that the AFTs reached the lowest point in a weak reducing atmosphere (N2:CO:CO2 = 80%:5%:15%). The Fe2O3 species existed in the ash that prepared in oxidizing atmosphere were reduced due to small quality of CO in weak reducing atmosphere and then formed the Fe2+ compounds with lower melting temperature. If the concentration of CO increases, the Fe2+ compounds would be reduced continually, which would convert into elemental Fe with relatively high melting temperature. Compared with the low iron coal, the AFTs of the high iron coal reduced more obviously, when oxidizing atmosphere turned into weak reducing atmosphere.

Highlights

  • The atmosphere leading to the lowest AFTs of coal was quantified.

  • Different CO concentration affected the valence state of iron in coal ash.

  • The formed Fe2+-based compounds were the main reason which induced the lower AFTs under weak reducing atmosphere.

Acknowledgments

This study was supported by the National Natural Science Foundation of China (Nos. 51606163, 51376147), and the Foundation of State Key Laboratory of Coal Combustion (FSKLCCA1602).

Additional information

Funding

This study was supported by the National Natural Science Foundation of China: [Grant Numbers 51606163, 51376147] and the Foundation of State Key Laboratory of Coal Combustion: [Grant Number FSKLCCA1602].

Log in via your institution

Log in to Taylor & Francis Online

PDF download + Online access

  • 48 hours access to article PDF & online version
  • Article PDF can be downloaded
  • Article PDF can be printed
USD 61.00 Add to cart

Issue Purchase

  • 30 days online access to complete issue
  • Article PDFs can be downloaded
  • Article PDFs can be printed
USD 1,493.00 Add to cart

* Local tax will be added as applicable

Related Research

People also read lists articles that other readers of this article have read.

Recommended articles lists articles that we recommend and is powered by our AI driven recommendation engine.

Cited by lists all citing articles based on Crossref citations.
Articles with the Crossref icon will open in a new tab.