In the utilization of boron-containing iron concentrate
(BIC),
its complex mineralogical composition and finely disseminated mineral
particles restrict its large-scale exploitation. Soda-ash roasting
proves to be a practical approach for boron activation and extraction,
wherein reactions among magnetite, silicates, and soda ash are involved,
which affect the consumption of soda ash and the subsequent recovery
of iron. This study investigates and compares the phase transformations,
microstructure evolution, and magnetism changes of soda-ash roasted
BIC under different roasting atmospheres. Results indicate that neutral
(100 vol % N2) and weakly reductive atmospheres (50 vol
% N2 + 5 vol % CO + 45 vol % CO2) regulated
the iron species into the Fe3O4 and Mg
x
Fe3–x
O4 phases with strong magnetism, respectively. In contrast, the iron
species presented as interwoven Fe2O3 and MgFe2O4 under an oxidative atmosphere (79 vol % N2 + 21 vol % O2). When the roasting atmosphere was
intensely reductive (100 vol % CO), the roasted ore consisted of sponge
iron and Mg
y
Fe1–y
O.