TY - JOUR
T1 - Combustion char morphology related to combustion temperature and coal petrography
AU - Rosenberg, Per
AU - Petersen, Henrik I.
AU - Thomsen, Erik
N1 - Funding Information:
The authors are grateful to the Danish Energy Agency, Elsam I/S and Elkraft A.m.b.a. for financial support. L. H. Sorensen (Research Centre Rise) is thanked for preparing laboratory-scale chars, and K. Laursen (Geological Survey of Denmark and Greenland, GEUS) for sampling full-scale chars at the Fynsvaerket p.f. power plant, Denmark. Fynsvrerket is thanked for giving access to the full-scale experiments. D. Jutson (GEUS) is thanked for reading and improving the manuscript.
PY - 1996/7
Y1 - 1996/7
N2 - The morphology of chars sampled from various laboratory-scale reactors operating at temperatures from 800 to > 1400°C, together with chars collected directly in the flame zone in a full-scale pulverized fuel combustion experiment, was examined. A coal and coal blend dominated by vitrinite-rich microlithotypes together with four coals dominated by inertinite-rich microlithotypes were used to produce the combustion chars. Char samples produced at temperatures above ∼1300°C have a morphotype composition very similar to the composition of the full-scale char samples, whereas the morphotype compositions of those produced at ∼1150°C or lower are significantly different. Correlation between coal petrography and char morphology and determination of char reactivity should thus be attempted only using chars produced at temperatures comparable with those for the intended use of the coal. A clear distinction between the high-temperature char samples (burnout 50-60 wt% daf) emerges which is related mainly to the parent coal petrography and probably secondarily to the rank. Vitrite, clarite and vitrinertite V may be correlated with the porous tenuisphere and crassisphere morphotypes, whereas inertite, durite, vitrinertite I, duroclarite and clarodurite may be correlated with the crassinetwork - mixed-network - mixed morphotype group.
AB - The morphology of chars sampled from various laboratory-scale reactors operating at temperatures from 800 to > 1400°C, together with chars collected directly in the flame zone in a full-scale pulverized fuel combustion experiment, was examined. A coal and coal blend dominated by vitrinite-rich microlithotypes together with four coals dominated by inertinite-rich microlithotypes were used to produce the combustion chars. Char samples produced at temperatures above ∼1300°C have a morphotype composition very similar to the composition of the full-scale char samples, whereas the morphotype compositions of those produced at ∼1150°C or lower are significantly different. Correlation between coal petrography and char morphology and determination of char reactivity should thus be attempted only using chars produced at temperatures comparable with those for the intended use of the coal. A clear distinction between the high-temperature char samples (burnout 50-60 wt% daf) emerges which is related mainly to the parent coal petrography and probably secondarily to the rank. Vitrite, clarite and vitrinertite V may be correlated with the porous tenuisphere and crassisphere morphotypes, whereas inertite, durite, vitrinertite I, duroclarite and clarodurite may be correlated with the crassinetwork - mixed-network - mixed morphotype group.
KW - Coal petrography
KW - Combustion char
KW - Morphology
UR - http://www.scopus.com/inward/record.url?scp=0001105884&partnerID=8YFLogxK
U2 - 10.1016/0016-2361(96)00074-9
DO - 10.1016/0016-2361(96)00074-9
M3 - Article
AN - SCOPUS:0001105884
SN - 0016-2361
VL - 75
SP - 1071
EP - 1082
JO - Fuel
JF - Fuel
IS - 9
ER -