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Landfill leachate has a high chloride (Cl − ) content. Because it is highly mobile, and cannot be sorbed or transformed bio-chemically, it is important to have detailed information about how it migrates in landfill sites. In this study, we set up four lab-scale simulated landfills, including an anaerobic landfill (AL), an anaerobic landfill with leachate recirculation (RAL), an anaerobic/semi-anaerobic landfill with leachate recirculation (RASL), and an anaerobic/semi-aerobic landfill (ASL), to explore how, when regulated, moisture and air affected the migration of chlorine. We found that water and air had a strong influence on the release of Cl − . Leachate obviously promoted Cl −  dissolution in refuse when recirculated. When air was introduced into landfill, thereby changing it from anaerobic to semi-aerobic, the leachate Cl −  concentration increased sharply from around 4–9 g L −1  (RASL) and 18 g L −1  (ASL), respectively. In principle, Cl −  is released continuously when leachate is recirculated in landfills (RAL and RASL), but it can also be found a terminal when the leachate recirculation stops (AL and ASL). Cumulative amounts of 64, 66, 27, and 53 g of Cl −  were released from the AL, RAL, RASL, and ASL, respectively. Lower COD/Cl and-N/Cl ratios in ASL and RASL after day 175 indicated that lower Cl −  pollution risk than that in AL and RAL.

Effect of air and water on the release of chlorine from semi-aerobic landfill