Acid mine drainage from the (Samma)taejung coal mine was examined using water-quality analysis, degassing and neutralization trials, and geochemical modeling. The mine water was highly acidic (pH 3.34) and contained elevated levels of dissolved Fe, Al...
Acid mine drainage from the (Samma)taejung coal mine was examined using water-quality analysis, degassing and neutralization trials, and geochemical modeling. The mine water was highly acidic (pH 3.34) and contained elevated levels of dissolved Fe, Al, Mn, Mg, SiO2, CO2, and SO4 2–. Stoichiometric calculations estimated approximately 393 kg/day of precipitation, with secondary minerals derived from CO2, SO4 2–, Ca, and Mg exceeding contaminant mass. Neutralization modeling showed that calcite precipitates around pH 6.5, while Mn(OH)2, brucite, and gypsum form sequentially above pH 9. Dissolved CO2 was removed within 20 min of degassing, which controlled calcite precipitation. At pH > 9, gypsum and brucite formation were identified as the main cause of sludge generation. These findings suggest that combining CO2 degassing with maintaining the neutralization reactor below pH 9 can reduce lime consumption and minimize sludge production.