Migration and transformation of manganese during the artificial recharging of a deep confined aquifer

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• 作者：Xiancang Wu ; Wenjing Zhang ; Shanghai Du ; XuFei Shi…
• 关键词：Manganese ; Migration ; Transformation ; Artificial recharge ; Groundwater
• 刊名：Arabian Journal of Geosciences
• 出版年：2016
• 出版时间：February 2016
• 年：2016
• 卷：9
• 期：2
• 全文大小：1,302 KB
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• 作者单位：Xiancang Wu (1) (2)
  Wenjing Zhang (1) (2)
  Shanghai Du (1) (2)
  XuFei Shi (1) (2)
  Xipeng Yu (1) (2)
  Ying Huan (1) (2)
  Hanmei Wang (3) (4) (5)
  Xun Jiao (3) (4) (5)
  
  1. Key Laboratory of Groundwater Resources and Environment, Ministry of Education, Jilin University, Changchun, 130021, China
  2. College of Environment and Resources, Jilin University, Changchun, 130021, China
  3. Shanghai Institute of Geological Survey, Shanghai, 200072, China
  4. Shanghai Engineering Research Center of Land Subsidence, Shanghai, 200072, China
  5. Key Laboratory of Land Subsidence Monitoring and Prevention, Shanghai, 200072, China
  
• 刊物类别：Earth and Environmental Science
• 出版者：Springer Berlin Heidelberg
• ISSN：1866-7538

文摘

Field tests and laboratory experiments were performed, using an artificial groundwater recharging site in Southeast China as an example, to investigate the migration and transformation of manganese during the artificial recharging of a deep confined aquifer. The migration and transformation of total manganese and divalent manganese (Mn(II)) were influenced by mixing, oxidation reactions, and the dissolution of minerals containing manganese, and increasing the dissolved oxygen (DO) concentration was found to promote the dissolution of minerals containing manganese. The laboratory experiments showed that the retardation factors were higher upstream than downstream of the recharging hole. The amount of dissolution that occurred decreased, and the amount of mixing that occurred increased as the distance from the recharging hole increased. The DO concentration decreased as the amount of dissolution of minerals containing manganese that occurred decreased. A high temperature, a high DO concentration, and the presence of microorganisms were found to promote the dissolution of minerals containing manganese, which caused the total manganese and Mn(II) concentrations to increase.