Abstract

Using a custom-designed self-heating apparatus and procedure, activation energy ( E a) was determined for four sulfide-bearing materials: two nickel concentrates, a copper concentrate and a sphalerite/pyrite mixture. The E a ranged from 22–29 kJ mol −1, implying a common reaction. Comparing to literature, the E a values correspond to partial oxidation of hydrogen sulfide, supporting the contention that H 2S may be an intermediate product in the self-heating of sulfide minerals.

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