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@ARTICLE{Tanner:817668,
author = {Tanner, J. and Bläsing, Marc and Müller, Michael and
Bhattacharya, S.},
title = {{R}eactions and {T}ransformations of {M}ineral and
{N}on-{M}ineral {I}norganic {S}pecies {D}uring the
{E}ntrained {F}low {P}yrolysis and {CO}$_{2}$ {G}asification
of {L}ow {R}ank {C}oals},
journal = {Energy $\&$ fuels},
volume = {30},
number = {5},
issn = {0887-0624},
address = {Columbus, Ohio},
publisher = {American Chemical Society},
reportid = {FZJ-2016-04336},
pages = {3798-3808},
year = {2016},
abstract = {The reactions and transformations of mineral and nonmineral
inorganic species in Victorian (MOR) and Rhenish (HKT) coals
were investigated in a two-stage process under high
temperature, entrained flow pyrolysis, and gasification
conditions. The parent coals were pyrolyzed at a temperature
between 1100 and 1400 °C in 100 vol $\%$ nitrogen. The
resulting char samples were collected and gasified at their
corresponding pyrolysis temperatures in 10–80 vol $\%$ CO2
in N2. Low temperature (500 °C) ash subsamples from the
parent coals, chars, and gasification residues were analyzed
for elemental and mineral phase composition. The phase
composition analysis was in agreement with the proportions
of various inorganic constituents in the elemental analysis.
In general, the extent of reaction and phase transformation
increased with increasing temperature and carbon conversion,
which is related to increasing temperature and CO2
concentration. The char elemental and phase compositions
were similar to those of the corresponding parent coal and
consisted predominantly of SiO2, CaSO4, and CaCO3 with minor
amounts of MgO and Fe2O3 in the MOR samples. Char
gasification resulted in consistently increasing reaction
and transformation trends, which indicates that
thermodynamic equilibrium was not reached. Low temperature
gasification of MOR and HKT char samples resulted
predominantly in thermal decomposition of CaSO4, retention
of CaCO3 due to recarbonation, and formation of MgO. The ash
composition at high temperature differed based on the
amounts of and reactions between various parent coal
inorganic constituents. In particular, the fate of Ca and Mg
differed markedly between the two coals. For MOR,
decomposition of MgO resulted in depletion of Mg at high
temperatures, whereas Mg was retained in HKT gasification
residues as MgAl2O4 and Ca2MgSi2O7 due to higher Si and Al
content. CaO from CaSO4 and CaCO3 decomposition was retained
in MOR samples as Ca2Fe2O5 and Ca2SiO4, and in HKT as
Ca2MgSi2O7.},
cin = {IEK-2},
ddc = {620},
cid = {I:(DE-Juel1)IEK-2-20101013},
pnm = {111 - Efficient and Flexible Power Plants (POF3-111)},
pid = {G:(DE-HGF)POF3-111},
typ = {PUB:(DE-HGF)16},
UT = {WOS:000376417600027},
doi = {10.1021/acs.energyfuels.5b03012},
url = {https://juser.fz-juelich.de/record/817668},
}