Grain size distribution of Isalnita power plant lignite ash and elemental composition of size classes

Citation
G. Niac et al., Grain size distribution of Isalnita power plant lignite ash and elemental composition of size classes, FUEL, 80(5), 2001, pp. 731-737
Citations number
21
Categorie Soggetti
Chemistry,"Chemical Engineering
Journal title
FUEL
ISSN journal
00162361 → ACNP
Volume
80
Issue
5
Year of publication
2001
Pages
731 - 737
Database
ISI
SICI code
0016-2361(200104)80:5<731:GSDOIP>2.0.ZU;2-A
Abstract
Grain size analysis of 48 samples of Isalni(a power plant lignite ash revea led a mixture of three populations, each of them showing best fit to Weibul l distribution with smallest size (x(0)) 40, 350 and 740 mum, mean size (x( m)) 163, 506 and 1068 mum, exponent (alpha) 1.42, 2.31 and 0.84, and partic ipation to the whole mass with (p) 49, 23 and 28%, respectively. The fine p opulation originates, according to the "two phase model of coal", from the mineral, the coarse, from the maceral pseudo-phase, while the middle fracti on is presumably formed from extraneous minerals. Other three samples taken from the same power plant twenty years later could be resolved alike in th ree populations, with x(0) and x(m) shifted to smaller sizes. Concentration s of Na and Ca are evenly distributed among size classes, concentrations of K, Mg, Al, Fe, Ti and P are decreasing with particle size, while the conce ntration of S and C increases from the smallest to the largest size class 5 and 10 times, respectively, due to the mainly organic origin of these elem ents. (C) 2001 Elsevier Science Ltd. All rights reserved.