Pyrite single-crystal cubes were cut, polished. and x-rayed to produce orientations of (100), (110), (111), and (112). These crystallographically developed surfaces then were prepared to expose an area of 1 cm(2), and the remainder of the crystal was coated with an acid-resistant silicone cement. Crystals with representative orientations then were leached in ferric sulfate solutions adjusted to a pH of 2.3 with H(2)SO(4) containing up to 6 x 10(3) ppm of Fe(3+) at 30 and 55 degrees C. Leaching was also conducted in acid-bacterial lixiviants containing Thiobacillus ferrooxidans at 30 degrees C and a thermophilic microorganism at 55 degrees C. Surface corrosion and pitting associated with pyrite leaching were examined by scanning electron microscopy. Pyrite leaching in ferric sulfate solutions was observed to be different when compared to acid-bacterial leaching. Ferric sulfate leaching required nearly 2 x 10(3) ppm of Fe(3+) at 30 degrees C while acid-bacterial leaching at 30 degrees C occurred without additions of Fe(3+), and values of Fe(3+) never exceeded 10(2) ppm. Because of precipitate formation, an accurate assessment of the role of crystallographic orientation on the leaching of pyrite is difficult.
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Keller et al. (1982) studied this question.
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