A step has been made in the direction of understanding the fundamental chem
ical processes taking place inside electric are furnaces producing manganes
e alloys. The reduction of higher manganese oxides to MnO by carbon monoxid
e has been studied in the temperature range 700 degrees C to 1100 degrees C
. A topochemical pattern with a single shrinking core inside the ore partic
les has been observed in most cases. It has been found that the reduction o
f some manganese silicates (braunite minerals) is influenced by reaction in
terface kinetics, whereas the reduction rate of manganese oxides (bixbyite
and hausmannite) is mostly determined by product shell pore diffusion. Sint
ering kinetics and the extent of natural porosity determine the product she
ll pore diffusivity. As the melting point of the reaction product is approa
ched, rapid sintering leads to a decrease in diffusivity.