The flame behaviour of the most important carbonates in European impor
t coals has been investigated. The flame tests were performed in a lab
oratory facility in which the environment of a coal burner was simulat
ed. For the tests the coal minerals were separated from the coal by fl
oat-sink separation. Electron microscopy was used to determine the siz
e and morphology of the particles sampled from the flame. The viscosit
y of the particles was derived from tests of their adherence to refrac
tory deposit plates placed in the flame. Calcite (CaCO3) particles of
60 mu m, a typical size in pulverized coal, broke up into fragments ap
proximately ten times smaller. The rime taken for complete fragmentati
on corresponded to the time calculated for the decomposition of the ca
lcite, None of the 'siderite' samples tested showed fragmentation. Det
ailed analyses with TGA MS (thermogravimetry coupled with mass spectro
metry) were performed to determine the actual fraction of FeCO3 in the
'siderite' samples. Flame products of siderite proper had high viscos
ity. Siderite particles with embedded silicates had flame products of
low viscosity, Ankerite (CaFe(CO3)(2)) did not fragment and the flame
product was fluid.