Structure Characteristics Analysis of Long Flame Coal

Article Preview

Abstract:

Applying X-ray diffraction, an analysis of crystallite structure on the coal samples from Hami, including raw coal and coals heated respectively at 200°C, 250°C and 300°C, was carried out. The results show: The intensity of the 002 diffraction peak increases, the γ diffraction peak of the coals decreases, the 100 diffraction peak appears and its intensity increases, the size of the crystallite, the stacking height of the aromatic layer and the condensation degree of the aromatic rings increase, and the proportion of the non-crystallite decreases in coal samples, with the temperature increasing at below 300°C.

You might also be interested in these eBooks

Info:

Periodical:

Advanced Materials Research (Volumes 724-725)

Pages:

1046-1049

Citation:

Online since:

August 2013

Export:

Price:

Permissions CCC:

Permissions PLS:

Сopyright:

© 2013 Trans Tech Publications Ltd. All Rights Reserved

Share:

Citation:

[1] S. Ergun and V.H. Tiensuu. Interpretation of the intensities of X-rays scattered by coals. Fuel Vol.38 (1959), p.64

Google Scholar

[2] Ergun S. Graphite like layers in coals and high vacuum distillation products. Fuel Vol.37 (1958), p.365

Google Scholar

[3] D.L. Wertz. X-ray analysis of the Argonne premium coals. 1. Use of absorption/diffraction methods. Energy & Fuels Vol.4 (1990), p.442

DOI: 10.1021/ef00023a006

Google Scholar

[4] D.L. Wertz, C.B. Smithhart and S.L. Wertz. X-ray mass absorption coefficients: measurements and uses in the quantitative of charactive diffraction analysis of pyrite in coals. 38th applications of X-ray analysis, Denver, CO: Plenum (1989).

DOI: 10.1154/s037603080001990x

Google Scholar

[5] D.L. Wertz and M. Bissell. One-dimensional description of the average polycyclic aromatic unit in Pocahontas no. 3 coal: an X-ray scattering study. Fuel Vol.74 (1995), p.1431

DOI: 10.1016/0016-2361(95)00107-g

Google Scholar

[6] D.L. Wertz and M. Bissel. Analysis of the average poly-cyclic aromatic unit in meta-anthracite coal using conventional X-ray powder diffraction and intensity separation methods. 42nd applications of X-ray analysis, Denver, CO: Plenum (1993).

DOI: 10.1007/978-1-4615-2528-8_60

Google Scholar

[7] D.L. Wertz and M. Bissell. Relating the nonideal diffraction from the graphene layer stacking peak to the aliphatic carbon abundance in bituminous coals. Energy & Fuels Vol.8 (1994),p.613–7.

DOI: 10.1021/ef00045a016

Google Scholar

[8] D.L. Wertz. X-ray scattering analysis of the average polycyclic aromatic unit in Argonne premium coal 401. Fuel Vol.77 (1998), p.43

DOI: 10.1016/s0016-2361(97)00150-6

Google Scholar

[9] FRL Schoening. X-ray structure of some South African coals before and after heat treatment at 500 and 1000℃. Fuel Vol.62 (1983),p.1315

DOI: 10.1016/s0016-2361(83)80016-7

Google Scholar

[10] FRL Schoening. X-ray structure parameters of coal. Fuel Vol.61 (1982),p.695

Google Scholar

[11] L. Lu, V. Sahajwalla, C. Kong and D. Harris. Quantitative X-ray diffraction analysis and its application to various coals. Carbon Vol.39 (2001), p.1821

DOI: 10.1016/s0008-6223(00)00318-3

Google Scholar

[12] T.F. Yen, J.G. Erdman and S.S. Pollack. Investigation of the structure of petroleum asphaltenes by X-ray diffraction. Anal. Chem. Vol.33 (1961), p.1587

DOI: 10.1021/ac60179a039

Google Scholar