Microbial sulfate reduction in acidic (pH 3) strip-mine lakes

Abstract ³⁵SO₄ reduction was detected in slurries of sediments obtained from Reservoir 29 (pH 3.8) and Lake B (pH 6.2), two acid strip-mine lakes in Indiana. The rates varied seasonally and were higher in summer and fall than in the spring. The optimal pH for sulfate reduction in Reservoir 29 sediments was 5, but samples had increased activity at pH 7 within 24 h after adjusting the pH to this value. In Lake B, the optimal pH for sulfate reduction was the in situ pH (6.2). Sulfate reduction in both lakes was stimulated 2–3-fold by increasing p _H2. High concentrations (5 mM) of organic acids inhibited sulfate reduction at pH 3.8, but stimulation was observed at concentrations of 0.1 mM. Acid-volatile sulfides accounted for about 70% of the products of ³⁵SO₄ reduction.