Acid sulfate soils are formed through the bacterial reduction of iron and sulfate in wet, oxygen-limited soils, producing pyrite. Undisturbed acid sulfate soils appear dark and wet with no structure, but when drained or disturbed they turn yellow, brown, and red as pyrite is oxidized, releasing sulfuric acid and lowering the pH. This can cause poor growth of plants and fish, and even fish kills. Proper management of acid sulfate soils is important for agriculture and aquaculture, including drying, tilling, liming, and maintaining water levels.