Oxidation rates have been estimated on various iron sulphide minerals such as pyrite, marcasite, melnikovite and pyrrhotite by observing oxygen quantity consumed by them.
At first, it has been ascertained that the rates are greatly infiuenced by water, temperature, and grain size of the specimen. Oxidation rates arerapid in order of pyrrhotite, melnikovite, marcasite and pyrite, and there existrather variation in them even among each mineral.
In order to compare with oxidation rates of various minerals, the factor (kθ
0) has been proposed by the writers. Here, (kθ
0) means the oxidation rate of apparent unit surface area of the specimen at θ0°C (cc/hr/m2)., (kθ
0) can be calculated from the equation, dx/dt=0.017 (kθ
0) e0.693 θ-θ
0/10, where xis the oxygen quantity consumed by the specimen (cc), t is time (hr), dx/dt is the oxygen consumption rate under the conditions of this experiment, and θ
0, θ
0 are temperature (°C) respectively.
Furthermore, consideration has been given to the oxygen poor air which often exists in the metal mine.
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