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Copper isotope fractionation and transformation at the acid mine drainage-sediment interface in mining areas
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De-hong LIU1, Kai-wen CAO1, 2, Wen LIAO3, Dong-mei HOU2, Song-xiong ZHONG1, *
China Environmental Science | 2026, 46(3) : 1533 - 1542
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China Environmental Science | 2026, 46(3): 1533-1542
• Environmental Ecology •
Copper isotope fractionation and transformation at the acid mine drainage-sediment interface in mining areas
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De-hong LIU1, Kai-wen CAO1, 2, Wen LIAO3, Dong-mei HOU2, Song-xiong ZHONG1, *
Affiliations
  • 1.Institute of Eco-Environmental and Soil Science, Guangdong Academy of Sciences, Guangzhou 510650, China
  • 2.Key Laboratory of Jiangxi Province for Persistent Pollutants Prevention Control and Resource Reuse, Nanchang Hangkong University, Nanchang 330063, China
  • 3.School of Public Health, Southern Medical University, Guangzhou 510515, China
Published: 2026-03-20
Outline
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The heavy metal copper (Cu) in acid mine drainage (AMD) is an essential element for organisms but potentially toxic. To control its environmental impact, it is necessary to investigate the factors that influence Cu migration in AMD-sediment interfaces. This study investigated the isotopic composition and fractionation characteristics of Cu in AMD systems from three different mining areas in central China. By coupling these isotopic signatures with detailed physicochemical analyses, we elucidated the key factors and mechanisms controlling Cu adsorption and migration. The results revealed that the Cu isotope fractionation between solutions and sediments in the Dingjiashan gold-copper-sulfur mining area, the Guanchao lead-zinc mining area, and the Qiaolichong polymetallic mining area ranged from (0.3±0.01)‰ to (1.5±0.07)‰, (0.61±0.01)‰, and (1.03±0.02)‰, respectively. This indicates that Cu isotope fractionation in AMD systems varies across mining areas and at different locations within the same mining area. The trends in the primary Cu species in sediments are consistent with those in AMD systems, and exhibit a clear pattern: as sediment Fe-oxide content and the proportion of Fe-/Mn-oxide-bound Cu increase, the isotopic fractionation magnitude decreases; conversely, elevated sulfur/organic matters and a larger fraction of organic- sulfide-bound Cu amplify the fractionation scale, confirming that mineral adsorption and organic-sulfur complexation are the key factors governing Cu mobility and transformation in AMD systems. These results suggest that the characteristics of Cu stable isotope fractionation may serve as a potential tool to explore the key factors controlling Cu migration in AMD systems across different mining areas.

acid mine drainage  /  sediment  /  copper  /  isotope fractionation  /  migration and transformation
刘德洪, 曹开文, 廖文, 侯冬梅, 钟松雄. 矿区酸性矿山废水-沉积物界面铜同位素分馏与转化. 中国环境科学, 2026 , 46 (3) : 1533 -1542 .
De-hong LIU, Kai-wen CAO, Wen LIAO, Dong-mei HOU, Song-xiong ZHONG. Copper isotope fractionation and transformation at the acid mine drainage-sediment interface in mining areas[J]. China Environmental Science, 2026 , 46 (3) : 1533 -1542 .
Year 2026 volume 46 Issue 3
87
14
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Article Info
  • Receive Date:2025-08-16
  • Online Date:2026-10-08
  • Published:2026-03-20
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  • Received:2025-08-16
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Affiliations
    1.Institute of Eco-Environmental and Soil Science, Guangdong Academy of Sciences, Guangzhou 510650, China
    2.Key Laboratory of Jiangxi Province for Persistent Pollutants Prevention Control and Resource Reuse, Nanchang Hangkong University, Nanchang 330063, China
    3.School of Public Health, Southern Medical University, Guangzhou 510515, China
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表12种不同金属材料的力学参数
科
Family
属数
Number of
genus
种数
Number of
species
占总种数比例
Percentage of
total species (%)
属
Genus
种数
Number of
species
占总种数比例
Percentage of total
species (%)
鹅膏菌科Amanitaceae 2 11 5.26 鹅膏菌属 Amanita 10 4.78
小菇科 Mycenaceae 2 12 5.74 丝盖伞属 Inocybe 5 2.39
多孔菌科 Polyporaceae 8 14 6.70 蜡蘑属 Laccaria 5 2.39
红菇科 Russulaceae 3 23 11.00 小皮伞属 Marasmius 6 2.87
小菇属 Mycena 11 5.26
光柄菇属 Pluteus 5 2.39
红菇属 Russula 17 8.13
栓菌属 Trametes 5 2.39
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